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  • 1
    Call number: AWI P5-20-94119
    Description / Table of Contents: Der exklusive Fotoband zur Jahrhundertexpedition in die Arktis. Im September 2019 legte die Polarstern in Richtung Arktis ab - an Bord das internationale MOSAiC-Forscherteam, das die Auswirkungen des Klimawandels auf das ewige Eis erkundet. Chronologisch aufgebaut dokumentiert der bildgewaltige Band in bisher ungesehenen Fotografien von Esther Horvath Leben und Arbeiten während der einjährigen Reise unter den extremen Bedingungen am Nordpol. Begleitet von kenntnisreichen Essays und Textbeiträgen von Experten, Wissenschaftlern und Expeditionsteilnehmern ist der Band ein eindrucksvolles Zeugnis der wohl größten klimatischen Herausforderung unserer Zeit und bietet Einblicke in dieses einmalige Forschungsprojekt sowie die spektakuläre, schützenswerte Polarlandschaft.
    Type of Medium: Monograph available for loan
    Pages: 240 Seiten , 250 Illustrationen , 30.5 cm x 24.5 cm
    ISBN: 978-3-7913-8669-0
    Language: German
    Note: Vorwort Prolog Die Vermessung einer schwindenden Welt Feuertaufe Vorbereitung für den Einsatz am Limit Leinen los Aufbruch ins arktische Eis Die Erfindung der Eisdrift Die Drift Vom Aufbau des nördlichsten Forschungscamps Atmosphärenforschung Das Observatorium Aufzeichnungen aus dem Eis Das arktische Meereis Alltag Leben am Ende der Welt Das Ökosystem der Arktis Die Forschung des Teams Biogeochemie Nachtschicht Forschung bei 24 Stunden Dunkelheit Ozeanforschung und Klimawandel Schichtwechsel Ablösung am Nordpol Im Gespräch mit Esther Horvath Eine andere Welt Drift durch den arktischen Sommer Dank Impressum
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  • 2
    Call number: AWI G5-20-94097
    Type of Medium: Dissertations
    Pages: vi, 127 Seiten , Illustrationen, Diagramme, Karten
    Language: English
    Note: Dissertation, Universität Potsdam, 2020 , Table of contents Abstract Kurzfassung Table of contents Chapter 1: Introduction 1.1 The challenge of proxy uncertainties 1.2 Aims and approaches 1.3 Thesis outline and author's contributions Chapter 2: Comparing methods for analysing time scale dependent correlations in irregularly sampled time series data 2.1 Abstract 2.2 Introduction 2.3 Methods 2.3.1 Time scale dependency 2.3.2 Irregularity 2.3.3 Surrogate data 2.3.3.1 Construction of surrogate signals 2.3.3.2 Construction of irregular sampling 2.3.4 Evaluation of the estimation methods 2.4 Results 2.4.1 Correlation of red signal - white noise time series 2.4.2 Correlation of white signal - white noise time series 2.5 Discussion 2.5.1 Effect of irregularity and non-simultaneousness in sampling 2.5.2 Choosing the best method 2.5.2.1 Handling irregularity 2.5.2.2 Accounting for time scale dependency 2.5.3 Example application to observed proxy records 2.6 Conclusion 2.7 Computer code availability 2.8 Acknowledgements 2.9 Appendix 2-A. Significance test for time scale dependent correlation estimates Chapter 3: Empirical estimate of the signal content of Holocene temperature proxy records 3.1 Abstract 3.2 Introduction 3.3 Data 3.3,1 Proxy records 3.3.2 Climate model simulations 3.4 Method 3.4.1 Approach and assumptions 3.4.2 Spatial correlation structure of model vs. reanalysis data 3.4.3 Processing steps 3.4.3.1 Estimation of the spatial correlation structure 3.4.3.2 Estimation of the SNRs 3.5 Results 3.5.1 Spatial correlation structure and correlation decay length 3.5.2 SNR estimates 3.6 Discussion 3.6.1 Spatial correlation structure of model simulations 3.6.2 Finite number of proxy records 3.6.3 Proxy-specific recording of climate variables 3.6.4 Time uncertainty and non-climatic components of the proxy signal 3.6.5 Implications and future steps forward 3.7 Conclusion 3.8 Code availability 3.9 Data availability 3.10 Acknowledgements Chapter 4: Testing the consistency of Holocene and Last Glacial Maximum spatial correlations in temperature proxy records 4.1 Abstract 4.2 Introduction 4.3 Data 4.4 Method 4.4.1 Approach and assumptions 4.4.2 Holocene and LGM spatial correlation structure from climate model simulation 4.4.3 Effect of changes in climate variability on the predicted correlations 4.4.4 Effect of changes in time uncertainty on the predicted correlations 4.4.S Estimating the surrogate-based LGM spatial correlation and accounting for parameter uncertainty 4.5 Results 4.6 Discussion 4.6.1 Proxy-specific recording and finite number of records 4.6.2 Time uncertainty of proxy records 4.6.3 Contrary behaviour of U K'37 records 4.6.4 Spatial correlation structure and orbital trends 4.7 Conclusion 4.8 Acknowledgements 4.9 Appendix 4-A. Deriving the effect of a different signal variance on the correlation Chapter 5: Synthesis 5.1 Irregular sampling and time scale dependent correlations 5.2 Spatial correlation structure of proxy records 5.3 Consistency of spatial correlations for different climate states 5.4 Signal content of proxy records 5.5 Concluding remarks and Outlook Chapter A: Supplement of Chapter 3 - Empirical estimate of the signal content of Holocene temperature proxy records A.1 Supplementary Figures A.2 Supplementary Tables Chapter B: Supplement of Chapter 4 - Testing the consistency of Holocene and Last Glacial Maximum spatial correlations of temperature proxy records 8.1 Supplementary Figures 8.2 Supplementary Tables References Danksagung Eidesstattliche Erklärung
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  • 3
    Monograph available for loan
    Monograph available for loan
    Hoboken, NJ : Wiley Blackwell
    Call number: AWI G3-20-93617
    Type of Medium: Monograph available for loan
    Pages: xiii, 454 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 978-1-405-10006-9
    Language: English
    Note: Contents Preface Acknowledgements 1 Introduction 1.1 The Periglacial Concept: Definitions and Scope 1.2 The Periglacial Realm 1.3 The Development of Periglacial Geomorphology 1.4 Periglacial Geomorphology: The Quaternary Context 1.5 The Aims and Organization of this Book 2 Periglacial Environments 2.1 Introduction 2.2 Periglacial Climates 2.3 Soils in Periglacial Environments 2.4 Vegetation Cover in Periglacial Environments 2.5 Synthesis 3 Ground Freezing and Thawing 3.1 Introduction 3.2 Ground Heating and Cooling 3.3 Soil Freezing 3.4 Ice Segregation in Freezing Soils 3.5 Thaw Consolidation 3.6 Synthesis 4 Permafrost 4.1 Introduction 4.2 Permafrost Thermal Regime 4.3 Classification of Permafrost 4.4 Detection, Mapping and Modelling of Permafrost 4.5 Permafrost Distribution 4.6 Permafrost-glacier Interactions 4.7 The Geomorphic Importance of Permafrost 5 Ground Ice and Cryostratigraphy 5.1 Introduction 5.2 Genetic Classification of Ground Ice 5.3 Description of Ground Ice 5.4 Ice Contacts 5.5 Cryostratigraphy 5.6 The Transition Zone 5.7 Massive Ground Ice 5.8 Yedoma 6 Thermal Contraction Cracking: Ice Wedges and Related Landforms 6.1 Introduction 6.2 Thermal Contraction Cracking and Polygon Evolution 6.3 Ice Veins and Ice Wedges 6.4 Ice-wedge Polygons 6.5 Sand Veins and Sand Wedges 6.6 Composite Veins and Composite Wedges 6.7 Sand-wedge Polygons 6.8 Frost Cracking of Seasonally Frozen Ground 6.9 Thaw Modification of Frost Wedges 6.10 Frost-Wedge Pseudomorphs and Frost Polygons in Areas of Past Permafrost 7 Pingos, Palsas and other Frost Mounds 7.1 Introduction 7.2 Characteristics of Pingos 7.3 Hydrostatic Pingos 7.4 Hydraulic Pingos 7.5 Pingo Problems and Problem Pingos 7.6 Segregation Ice Mounds: Palsas, Lithalsas and Related Landforms 7.7 Palsas 7.8 Peat Plateaus 7.9 Lithalsas 7.10 Permafrost Plateaus 7.11 Other Permafrost Mounds 7.12 Ephemeral Frost Mounds 7.13 Relict Permafrost Mounds 8 Thermokarst 8.1 Introduction 8.2 Thermokarst Lakes and Drained Lake Basins 8.3 Thermokarst Pits, Bogs and Fens 8.4 Retrogressive Thaw Slumps 8.5 Small-scale Thermokarst Features: Beaded Streams, Sinkholes and Thermokarst Gullies 8.6 Sediment Structures associated with Thermokarst 8.7 Relict Thermokarst Phenomena 9 Seasonally Frozen Ground Phenomena 9.1 Introduction 9.2 Upfreezing of Clasts 9.3 Frost Heave of Bedrock 9.4 Patterned Ground: The Embroidery on the Landscape 9.5 Patterned Ground Processes 9.6 Sorted Patterned Ground 9.7 Nonsorted Patterned Ground 9.8 Cryoturbations 9.9 Pedogenic Effects of Freezing and Thawing 9.10 Fragipans 9.11 Synthesis 10 Rock Weathering and Associated Landforms 10.1 Introduction 10.2 Physical Weathering Processes 10.3 Chemical Weathering Processes 10.4 Biotic Weathering Processes 10.5 Weathering Processes in Periglacial Environments 10.6Cold-climate Karst 10.7 Tors 10.8 Blockfields and Related Periglacial Regolith Covers 10.9 Brecciated Bedrocks 11 Periglacial Mass Movement and Hillslope Evolution 11.1 Introduction 11.2 Solifluction Processes 11.3 Solifluction Landforms 11.4 Pleistocene Solifluction Landforms and Slope Deposits 11.5 Active-layer Failures 11.6 Permafrost Creep 11.7 Nivation 11.8 Cryoplanation 11.9 Slope Form and Slope Evolution 12 Talus Slopes and Related Landforms 12.1 Introduction 12.2 Rockfall Talus 12.3 The Geomorphic Role of Snow Avalanches 12.4 Debris-flow Activity 12.5 Rock Glaciers 12.6 Pronival (Protalus) Ramparts 12.7 Synthesis 13 Fluvial Processes and Landforms 13.1 Introduction 13.2 Periglacial Hydrology 13.3 Slopewash 13.4 Slushflows 13.5 Sediment Transport in Periglacial Rivers 13.6 Bank and Channel Erosion 13.7 River Channels 13.8 Alluvial Landforms in Periglacial Environments 13.9 Valley Form 13.10 Pleistocene Periglacial Rivers 13.11 Synthesis 14 Wind Action 14.1 Introduction 14.2 Aeolian Processes 14.3 Wind Erosion in Present Periglacial Environments 14.4 Aeolian Deposits in Present Periglacial Environments 14.5 Quaternary Aeolian Deposits 14.6 Synthesis 15 Periglacial Coasts 15.1 Introduction 15.2 The Nature of Periglacial Coasts 15.3 The Role of Ice in Shoreline Evolution 15.4 Ice-rich Permafrost Coasts 15.5 Thermokarst Coasts 15.6 Barrier Coasts 15.7 Salt Marshes and Tidal Flats 15.8 Rock Coasts 15.9 Raised and Inherited Shorelines 15.10 Lake Shorelines 15.11 Synthesis 16 Past Periglacial Environments 16.1 Introduction 16.2 Palaeoenvironmental Reconstruction Based on Periglacial Features 16.3 Past Periglacial Environments of the British Isles 16.4 Pre-Late Devensian Periglacial Features in the British Isles 16.5 The Dimlington Stade in the British Isles 16.6 The Younger Dryas (Loch Lomond) Stade in the British Isles 16.7 Past Periglacial Environments of the British Isles: Commentary 16.8 Late Weichselian Periglacial Environments in Continental Europe 16.9 Late Wisconsinan Periglacial Environments in North America 16.10 Permafrost Extent in the Northern Hemisphere During the Last Glacial Stage 16.11 Concluding Comments 17 Climate Change and Periglacial Environments 17.1 Introduction 17.2 Permafrost Degradation 17.3 Geomorphological Implications of Climate Change in the Circumpolar North 17.4Geomorphological Implications of Climate Change in High Mountain Environments 17.5 Climate Change ,Permafrost Degradation and Greenhouse Gas Emissions 17.6 Conclusion Appendix: Text Abbreviations, Units and Symbols Employed in Equations References Index
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  • 4
    Call number: AWI P1-20-94200 ; M 23.94200
    Description / Table of Contents: Die Hochgebirge haben eine große Bedeutung für das globale Klima, die Wasserversorgung und die Biosphäre. So ist die besonders starke Ausprägung des Amazonas-Regenwalds den Anden zu verdanken. Sie verhindern den Durchzug der aus dem Atlantik mit viel Luftfeuchtigkeit kommenden Wolken. Dadurch erhält das Amazonas-Gebiet im Jahresdurchschnitt über 2.000 mm Regen, was die Grundlage für die intensive Bewaldung ist. Obwohl die Gebirge global nur ca. 12% der Landfläche bedecken, beherbergen Hochgebirge rund die Hälfte aller Säugetierarten und 74% aller endemischen Vogelarten (ohne Inselarten). 21 der 34 globalen Biodiversitätshotspots befinden sich in Hochgebirgen. In den Gebirgen entstehen aufgrund von höheren Niederschlägen wichtige Wasserressourcen auch für die angrenzenden Tiefländer. Trotz der für den Menschen oft erschwerten Zugänglichkeit sind Hochgebirge und Hoch-Plateaus, besonders in tropischen Regionen, Orte dichter Besiedlung und sogar von Hochkulturen. Die Folgen des Klimawandels sind in den Hochgebirgen besonders deutlich. So war die Erwärmung in den vergangenen Jahrzehnten dort höher als in den Flachländern. Die Gletscher schrumpfen in fast allen Gebirgen, insbesondere in den letzten Jahrzehnten. Auf den jetzt eisfreien Flächen siedeln sich schon nach wenigen Jahren neue Pflanzengemeinschaften an. In den Alpen hat das Eisvolumen seit 1850 schon um mehr als zwei Drittel abgenommen. Das entspricht allein seit 1997 einem Süßwasserverlust von etwa dem 14fachen Volumen des Bodensees. Insgesamt sind die Klimaänderungen in den Gebirgsregionen gravierender als im Flachland. Mit der Zunahme der Starkregen und dem Rückgang des Permafrosts nimmt die Gefahr von Erdrutschen zu, und manche Gletscher wurden instabil. Im Mittel haben sich die Temperaturen im Gebirgspermafrost in einem Jahrzehnt von 2007 bis 2016 um etwa 0,2°C erhöht. Die Schneedeckendauer nahm in den letzten Jahrzehnten kontinuierlich ab; die Herausforderungen für den Wintertourismus werden zusehends größer.
    Type of Medium: Monograph available for loan
    Pages: 384 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9783982006734
    Language: German
    Note: Inhaltsverzeichnis Vorwort Liste der Autoren/Autorinnen und der Gutachter Hochgebirge: Definition, Bedeutung, Veränderungen und Gefahren / (José L. Lozán,Siegmar-W. Breckle, Heidi Escher-Vetter, Hartmut Graßl & Dieter Kasang) 1 Bedeutung der Hochgebirge 1.1 Der Einfluss von Hochgebirgen auf die Zirkulation der Atmosphäre / (Jürgen Böhner & Jörg Bendix) 1.2 Die Entstehung der Hochgebirge / (Martin Meschede) 1.3 Übersicht über die wichtigsten Gebirge der Erde / (José L.Lozán, Siegmar-W. Breckle, Dieter Kasang & Heidi Escher-Vetter) 1.4 Berge und Gebirge im Meer / (Bernd Christiansen) 1.5 Hochgebirge: Wassertürme für eine wachsende Weltbevölkerung / (Carmen de Jong) 1.6 Erdoberflächenprozesse im Hochgebirge – Der Einfluss des Klimawandels / (Lothar Schrott & Jan Blöthe) 1.7 Hochgebirge: Hotspots der Biodiversität / (Severin Irl & Andreas H. Schweiger) 1.8 Hochgebirge als Ressourcenräume für Tiefländer / (Matthias Winiger) 1.9 Bevölkerung und Siedlungsstrukturen im Hochgebirge / (Christoph Stadel & Axel Borsdorf) 1.10 Lokale Anpassungsstrategien für Landnutzung in Hochgebirgen / (Hermann Kreutzmann) 2 Paläoökologische Veränderungen in Hochgebirgen 2.1 Globale Klima- und Gletscherveränderungen im Pleistozän und Holozän / (Heinz Veit & Alexander Groos) 2.2 Welche Umweltinformationen können aus Jahrringen abgeleitet werden? / (Achim Bräuning & Jussi Grießinger) 2.3 Holozäne Klimaänderungen und Waldgrenzschwankungen in den Alpen / (Conradin A. Burga) 2.4 Anthropogene Einflüsse auf die Hochgebirgsumwelt im Holozän: Einblicke aus einer alpinen Bergbaulandschaft / (Kerstin Kowarik & Hans Reschreiter) 3 Veränderungen der Kryosphäre in Hochgebirgen 3.1 Gletscherbeobachtung und globale Trends / (Frank Paul & Martin Hoelzle) 3.2 Die Gletscher Hochasiens im Klimawandel / (Tobias Bolch, Atanu Bhattacharya & Owen King) 3.3 Die Karakorum-Anomalie / (Christoph Mayer, Astrid Lambrecht & Alexander Groos) 3.4 Wenn Gletscher abrutschen / (Andreas Kääb) 3.5 Tropische Gletscher: Ostafrika / (Rainer Prinz & Thomas Mölg) 3.6 Die Gletscher der Anden im Klimawandel / (Thorsten Seehaus) 3.7 Gletscher und Schnee in Hochgebirgen Nordamerikas / (Dieter Kasang & José L. Lozán) 3.8 Gletscherschmelze unter Schuttbedeckung: Verbreitung, Prozesse und Messmethoden / (Pascal Buri, Simone Schauwecker & Jakob Steiner) 3.9 Permafrost in den Alpen – Langzeitbeobachtung und Entwicklung über zwei Jahrzehnte (Jeannette Nötzli) 3.10 Globale Klimaänderung und die Gletscher auf Neuseeland / (Stefan Winkler) 3.11 Einfluss des Klimawandels auf die Schneebedeckung / (Kay Helfricht & Marc Olefs) 4 Hydrologische Veränderungen in Hochgebirgen 4.1 Hochgebirgsgewässer im Wandel / (Heike Zimmermann-Timm, Deep Narayan Shah & Ram Devi Tachamo Shah) 4.2 Einfluss des globalen Wandels auf die Bodenstabilität des alpinen Graslandes / (Christine Alewell, Lauren Zweifel & Katrin Meusburger 4.3 Sozio-Hydrologie des Trans-Himalaya – Schmelzwasserverfügbarkeit und Bewässerungslandwirtschaft / (Marcus Nüsser, Juliane Dame & Susanne Schmidt) 4.4 Hochgebirge und Wasserressourcen in Peru und Kalifornien / (Dieter Kasang) 4.5 Hydrologische Veränderungen in vergletscherten Einzugsgebieten / (Regine Hoch) 5 Biodiversität der Hochgebirge im Klimawandel 5.1 Klimawandel und Vegetationsdynamik im Hochgebirge / (Harald Pauli) 5.2 Phänologische Veränderungen in Hochgebirgen / (Christian Rixen) 5.3 Klimawandel und Gebirgswälder: Bedrohung der Multifunktionalität? / (Georg Gratzer) 5.4 Alpine Waldgrenzen im Klimawandel – Wie sind die heterogenen Reaktionsmuster zu erklären? / (Udo Schickhoff, Maria Bobrowski & Niels Schwab) 5.5 Vegetation und Klimawandel an der Ostkordillere von Ecuador am Beispiel des Páramo de Papallacta / (M. Daud Rafiqpoor & Siegmar-W. Breckle) 5.6 Auswirkungen des Klimawandels auf das Wachstum von Zwergsträuchern in Hochgebirgen / (Stef Weijers & Jörg Löffler) 5.7 Pflanzen besiedeln neue Lebensräume: Primärsukzession auf Gletschervorfeldern / (Brigitta Erschbamer & Conradin A. Burga) 5.8 Klimawandel und biologische Invasionen im Hochgebirge /(Anna Schertler, Franz Essl & Bernd Lenzner) 5.9 Die Tierwelt der Alpen im Klimawandel / (Peter Huemer, Hermann Sonntag, Friederike Barkmann & André Stadler) 5.10 Ökologische Folgen des Landnutzungswandels in den Alpen / (Erich Tasser & Ulrike Tappeiner) 6 Sozioökonomische Veränderungen in Hochgebirgen 6.1 Ökonomische Bewertung von Biodiversität und Ökosystemleistungen in den Alpen / (Andreas Bartel & Barbara Färber) 6.2 Der sozioökonomische Strukturwandel in den Alpen / (Oliver Bender & Andreas Haller) 6.3 Klimawandel und Wintersporttourismus: Wahrnehmung und Reaktion der Touristen / (Jürgen Schmude & Maximilian Witting) 6.4 Mensch-Umwelt-Interaktionen im Äthiopischen Hochland / (Simon Strobelt & Michèle von Kocemba) 7 Naturgefahren in Hochgebirgen 7.1 Klimawandel, Morphodynamik und gravitative Massenbewegungen / (Thomas Glade) 7.2 Einfluss der Permafrostdegradation auf Hangstabilität / (Friederike Günzel & Wilfried Haeberli) 7.3 Warnsignal Klima - Die Lawinengefahr im Klimawandel / (Benjamin Reuter, Christoph Mitterer & Sascha Bellaire) 7.4 Gefahren aus vergletscherten Vulkanen: Das Beispiel Nevado del Ruiz / (Simon Allen, Christian Huggel & Frank Paul) 7.5 Bedrohung durch Erdbeben im Himalaya / (Birger-G. Lühr) 7.6 Risiken durch Gletscherseen im Klimawandel / (Holger Frey & Wilfried Haeberli) 7.7 Bergstürze, Seeausbrüche und Muren im Pamir / (Siegmar-W. Breckle & Martin Mergili) 8 Maßnahmen zum Klimaschutz und zur Anpassung 8.1 Klimawandel und Naturschutz im Gebirge: Neue Herausforderungen / (Mario F. Broggi) 8.2 Klimawandel und Anpassungsstrategien im Alpentourismus / (Ulrike Pröbstl-Haider) 8.3 Klimawandel in den Lebenswelten und Handlungslogiken ländlicher Bevölkerung im Hochgebirge: Perspektiven aus dem Callejón de Huaylas, Peru / (Martina Neuburger) 8.4 Hochland-Tiefland Beziehungen in ihrer Bedeutung für eine nachhaltige Entwicklung in Gebirgsräumen / (Paul Messerli, Susanne Wymann von Dach & Thomas Kohler) 9 Sachregister
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  • 5
    Call number: AWI P7-19-93234 ; IASS 19.93234 ; PIK N 454-20-93234
    In: World ocean review, 6
    Type of Medium: Series available for loan
    Pages: 329 Seiten , Illustrationen
    ISBN: 978-3-86648-634-8
    Series Statement: World ocean review 6
    Language: German
    Note: Inhalt Vorwort Arktis und Antarktis – Naturräume in Poleposition Eine kurze Geschichte der Polarregionen Der Mensch erobert die Polargebiete Conclusio: Arktis und Antarktis – zwei grundverschiedene Polargebiete Die Polargebiete als Teil des globalen Klimasystems Warum es in den Polarregionen so kalt wird Eisschollen, Eisschilde und das Meer Conclusio: Eine Kettenreaktion mit frostigem Ende Die Auswirkungen des Klimawandels auf die Polarregionen Die Pfade der Wärme Der Rückzug des Eises Conclusio: Mehr Wärme – viel weniger Eis Die Flora und Fauna der Polarregionen Ein Leben in der Kälte Das Leben im Meer Polare Ökosysteme auf dem Rückzug Conclusio: Hochspezialisiert und extrem gefährdet Politik und Wirtschaft in den Polarregionen Die Arktis und die Antarktis als politische Arenen Ein Wirtschaftsaufschwung mit Nebenwirkungen Conclusio: Wachsendes Interesse an den Polarregionen Gesamt-Conclusio Glossar Abkürzungen Quellenverzeichnis Mitwirkende Index Partner und Danksagung Abbildungsverzeichnis Impressum
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  • 6
    Call number: AWI A4-15-0044
    Description / Table of Contents: This document presents the Policy-maker's Summary of the 2015 AMAP Assessments of Short-lived Climate Pollutants (Methane, Black carbon and Ozone).
    Type of Medium: Monograph available for loan
    Pages: 14 S. : Ill., graph. Darst.
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  • 7
    Monograph available for loan
    Monograph available for loan
    Bonn : Rheinwerk Verlag GmbH
    Call number: AWI S4-16-90097
    Type of Medium: Monograph available for loan
    Pages: 467 Seiten , 1 CD-ROM , 24.5 cm
    Edition: 3., aktualisierte und erweiterte Auflage (2. Auflage im Rheinwerk Verlag)
    ISBN: 9783836237789
    Series Statement: Rheinwerk Computing
    Language: German
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  • 8
    Series available for loan
    Series available for loan
    Akureyri : International Arctic Science Committee
    Associated volumes
    Call number: AWI P5-17-90721
    In: IASC ... bulletin, 2017
    Type of Medium: Series available for loan
    Pages: 86 S. , Ill., graph. Darst., Kt.
    ISBN: 978-9935-24155-9
    ISSN: 1654-7594
    Series Statement: IASC Bulletin 2017
    Language: English
    Note: Content: Preface. - 1 IASC Internal Development. - IASC Organization. - IASC Council . - IASC Executive Committee. - IASC Secretariat. - Allen Pope New IASC Executive Secretary. - IASC Secretariat Moves to Iceland. - IASC Future Strategy. - IASC Medal 2017. - 2 IASC Working Groups. - Cross-Cutting Initiatives. - Atmosphere Working Group (AWG). - Cryosphere Working Group (CWG). - Marine Working Group (MWG). - Social and Human Working Group (SHWG). - Terrestrial Working Group (TWG). - 3 Arctic Science Summit Week 2016. - Upcoming ASSWs. - 4 Data and Observations. - Arctic Data Committee (ADC). - Sustaining Arctic Observing Networks (SAON). - 5 Partnerships. - Asian Forum for Polar Sciences (AFoPS). - Arctic Council. - 6 Capacity Building. - IASC Fellowship Program. - Overview of Supported Early Career Scientists. - Annex. - Polar Acronyms.
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  • 9
    Monograph available for loan
    Monograph available for loan
    Baltimore, Md. : Johns Hopkins University Pr.
    Call number: AWI E1-15-89213
    Description / Table of Contents: Alfred Wegener aimed to create a revolution in science which would rank with those of Nicolaus Copernicus and Charles Darwin. After completing his doctoral studies in astronomy at the University of Berlin, Wegener found himself drawn not to observatory science but to rugged fieldwork, which allowed him to cross into a variety of disciplines. The author of the theory of continental drift - the direct ancestor of the modern theory of plate tectonics and one of the key scientific concepts of the past century - Wegener also made major contributions to geology, geophysics, astronomy, geodesy, atmospheric physics, meteorology, and glaciology. Remarkably, he completed this pathbreaking work while grappling variously with financial difficulty, war, economic depression, scientific isolation, illness, and injury. He ultimately died of overexertion on a journey to probe the Greenland ice cap and calculate its rate of drift. This landmark biography - the only complete account of the scientist's fascinating life and work - is the culmination of more than twenty years of intensive research. In Alfred Wegener, Mott T. Greene places Wegener's background and theoretical advances in earth science in the context of his brilliantly eclectic career, bringing Wegener to life by analyzing his published scientific work, delving into all of his surviving letters and journals, and tracing both his passionate commitment to science and his thrilling experiences as a polar explorer, a military officer during World War I, and a world record-setting balloonist. In the course of writing this book, Greene traveled to every place that Alfred Wegener lived and worked - to Berlin, rural Brandenburg, Marbug, Hamburg, and Heidelberg in Germany; to Innsbruck and Graz in Austria; and onto the Greenland ice cap. He also pored over archives in Copenhagen, Munich, Marburg, Graz, and Bremerhaven, where the majority of Wegener's surviving papers are found. Written with great immediacy and descriptive power, Alfred Wegener is a powerful portrait of the scientist who pioneered the modern notion of unified earth science. The book should be of interest not only to earth scientists, students of polar travel and exploration, and historians but to all readers who are fascinated by the great minds of science.
    Type of Medium: Monograph available for loan
    Pages: xiv, 675 S. , Ill., Kt.
    ISBN: 9781421417127
    Language: English
    Note: Contents: Preface. - Acknowledgements. - 1. The boy: Berlin and Brandenburg, 1880-1899. - 2. The student: Berlin - Heidelberg - Innsbruck - Berlin, 1899-1901. - 3. The astronomer: Berlin, 1901-1904. - 4. The aerologist: Lindenberg, 1905-1906. - 5. The polar meteorologist: Greenland, 1906. - 6. The Arctic explorer (1): Greenland, 1907-1908. - 7. The atmospheric physicist (1): Berlin und Marburg, 1908-1910. - 8. The atmospheric physicist (2): Marburg, 1910. - 9. At a crossroads: Marburg, 1911. - 10. The theorist of continental drift (1): Marburg, December 1911 - February 1912. - 11. The theorist of continental drift (2): Marburg, February - April 1912. - 12. The Arctic explorer (2): Greenland, 1912-1913. - 13. The soldier: Marburg and "The Field", 1913-1915. - 14. The meteorologist: "In the field", 1916-1918. - 15. The geophysicist: Hamburg, 1919-1920. - 16. From geophysicist to climatologist: Hamburg, 1920-1922. - 17. The paleoclimatologist: Hamburg, 1922-1924. - 18. The professor: Graz, 1924-1928. - 19. Theorist and Arctic explorer: Graz and Greenland, 1928-1929. - 20. The expedition leader: Graz and Greenland, 1929-1930. - Epilogue. - Notes. - Bibliographical essay. - Index.
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  • 10
    Call number: AWI G6-18-91326
    Type of Medium: Monograph available for loan
    Pages: 279 Seiten , Diagramme, Karten
    ISBN: 9783110402421
    Language: English
    Note: Contents: Preface. - Acknowledgements. - 1 Introduction. - 1.1 Origin and characters of silicon and its isotopes. - 1.2 A brief description of silicon geochemistry. - 1.3 The history of silicon isotope studies. - 2 Analytical methods of silicon isotope composition. - 2.1 Gas source isotope ratio mass spectrometric analysis of silicon isotopes. - 2.2 Multi-collector inductively coupled plasma mass spectrometric (MC-ICPMS) analysis of silicon isotopes. - 2.3 Secondary ion mass spectrometry analyses. - 2.4 Standards and reference materials for silicon isotope measurement. - 2.5 Comparison of different methods on silicon isotope analyses. - 3 Mechanisms of silicon isotope fractionation. - 3.1 The thermodynamic silicon isotope exchange fractionation. - 3.2 Kinetic fractionation of silicon isotopes. - 4 Distribution of silicon isotopes in nature. - 4.1 Silicon isotope compositions of extraterrestrial materials. - 4.2 Silicon isotope distribution in lithosphere. - 4.3 Silicon isotope compositions of soils. - 4.4 Hydrosphere. - 4.5 Biosphere. - 5 Several aspects of silicon isotope applications. - 5.1 Studies on global silicon cycle. - 5.2 Silicon isotope studies on environmental variation of ocean. - 5.3 Studies on mechanisms of absorption, transportation and precipitation of silicon in plant growth processes. - 5.4 Studies on silicon source and genesis of ore deposits. - References. - Index.
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  • 11
    Monograph available for loan
    Monograph available for loan
    Bremerhaven [u.a.] : Alfred-Wegener-Institut
    Call number: AWI S6-17-91076
    Type of Medium: Monograph available for loan
    Pages: 108 Seiten , Illustrationen, graphische Darstellungen
    Language: German
    Note: Der richtige Standort - ein Grußwort / Gotthilf Hempel. - Vorwort / Karin Lochte, Bernhard Diekmann. - Die Entwicklung der Forschungsstelle Potsdam / Hans-Wolfgang Hubberten, Klaus Dethloff, Bernhard Diekmann, Diedrich Fritzsche. - Die Entwicklung der Atmosphärenforschung / Klaus Dethloff, Markus Rex, Roland Neuber, Annette Rinke, Dörthe Handorf, Marion Maturilli, Christoph Ritter, Peter von der Gathen, Ralph Lehmann, Wolfgang Dorn, Ingo Wohltmann. - Die Entwicklung der Periglazialforschung: Rückblick und Ausblick / Guido Grosse, Hans-Wolfgang Hubberten. - Die AWIPEV-Station auf Spitzbergen / Roland Neuber, Marion Maturilli, Christoph Ritter. - Permafrost-Langzeit-Observatorien in Sibirien und auf Spitzbergen / Julia Boike, Anne Morgenstern, Guido Grosse. - Küstenforschung im Nordwesten Kanadas / Michael Fritz, Hugues Lantuit. - Das Atmosphärenobservatorium Palau - Polarforschung in den Tropen / Markus Rex, Katrin Müller. - Zum Nordpol auf einer Eisscholle - Teilnahme an der Driftstation NP-35 / Marion Maturilli, Jürgen Gräser. - Polarer Ozonverlust im Klimawandel / Markus Rex, Peter von der Gathen, Ralph Lehmann, Ingo Wohltmann. - Vom grünen Laserstrahl zur Mikrophysik des Aerosols / Christoph Ritter, Marion Maturilli, Roland Neuber. - Wie können arktische Klimaänderungen das Wetter und Klima in Mitteleuropa beeinflussen? / Dörthe Handorf, Klaus Dethloff, Annette Rinke, Ralf Jaiser, Wolfgang Dorn, Heidrun Matthes. - Permafrost im Wandel - Regionaler Fokus, globale Bedeutung / Jens Strauss, Josefine Lenz, Thomas Schneider von Deimling, Frank Günther, Lutz Schirrmeister. - Arktischer Klimawandel und terrestrische Ökosysteme / Ulrike Herzschuh, Thomas Laepple, Hanno Meyer, Kathleen Stoof-Leichsenring, Heike Zimmermann, Laura Epp, Stefan Kruse, Boris Biskaborn, Diedrich Fritzsche, Birgit Heim, Bernhard Diekmann. - Das EU-Projekt PAGE21 / Hans-Wolfgang Hubberten, Julia Boike, Hugues Lantuit, Leen Kaisa Viitanen. - ICOP 2016 / Karina Schollän, Hans-Wolfgang Hubberten. - Nationale und internationale Sekretariate. - Potsdamer Nachwuchs. - Impressum.
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  • 12
    Call number: M 17.90886 / Büro 00.10 ; AWI S5-18-90886
    Type of Medium: Monograph available for loan
    Pages: 350 Seiten
    Edition: 2., überarbeitete und erweiterte Auflage
    ISBN: 978-3-11-053868-7
    Language: German
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  • 13
    Monograph available for loan
    Monograph available for loan
    Cheltenham : Edward Elgar Publishing Ltd
    Call number: AWI P5-18-91257 ; IASS 18.91435
    Description / Table of Contents: The Arctic is a region that has seen exponential growth as a space of geopolitical interest over the past decade. This insightful book is the first to analyse the European Union’s Arctic policy endeavours of the early 21st Century from a critical geopolitical perspective. Exploring the EU’s decade-long undertaking to construct legitimacy in the Arctic between 2008 and 2017, Andreas Raspotnik investigates whether the EU can figure prominently in the Arctic region as an international actor. This book presents the EU’s interest in the Arctic as a fascinating test case for how the EU aims to assert its policies and values in a neighbouring region. This contemporary and intriguing book will be an invaluable resource for scholars and students of international relations, European studies, geography, and Arctic studies, as well as those on courses relating to international organisations and global/regional politics. It will also appeal to the broader public with an interest in the challenges and opportunities of the Arctic region.
    Type of Medium: Monograph available for loan
    Pages: x, 231 Seiten , Illustrationen
    ISBN: 978-1-78811-208-6 , 9781788112093 (eBook)
    Language: English
    Note: Contents: List of figures and tables. - List of boxes. - Acknowledgements. - List of abbreviations. - PART I INTRODUCTION . - 1. The Geopolitics of an Arctic Meltdown and the Question of EUropean Arctic Space. - PART II GEOPOLITICS. - 2. The Thought Experiment Referred to as Geopolitics. - PART III THE ARCTIC. - 3. Arctic Geopolitics and the Regional Zeitgeist of the Twenty-First Century. - PART IV THE EUROPEAN UNION. - 4. EUropean Dimensions of Arctic Presence. - 5. An Action in the Making: The EU’s Arctic Policy-Making Process. - 6. The EU’s Arctic Space-Making Practices. - PART V CONCLUSION. - 7. A European Geopolitical Subject in the Arctic?. - REFERENCES. - APPENDIX I. - APPENDIX II. - INDEX.
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  • 14
    Call number: AWI G6-18-91956
    Description / Table of Contents: Earth's climate varies continuously across space and time, but humankind has witnessed only a small snapshot of its entire history, and instrumentally documented it for a mere 200 years. Our knowledge of past climate changes is therefore almost exclusively based on indirect proxy data, i.e. on indicators which are sensitive to changes in climatic variables and stored in environmental archives. Extracting the data from these archives allows retrieval of the information from earlier times. Obtaining accurate proxy information is a key means to test model predictions of the past climate, and only after such validation can the models be used to reliably forecast future changes in our warming world. The polar ice sheets of Greenland and Antarctica are one major climate archive, which record information about local air temperatures by means of the isotopic composition of the water molecules embedded in the ice. However, this temperature proxy is, as any indirect climate data, not a perfect recorder of past climatic variations. Apart from local air temperatures, a multitude of other processes affect the mean and variability of the isotopic data, which hinders their direct interpretation in terms of climate variations. This applies especially to regions with little annual accumulation of snow, such as the Antarctic Plateau. While these areas in principle allow for the extraction of isotope records reaching far back in time, a strong corruption of the temperature signal originally encoded in the isotopic data of the snow is expected. This dissertation uses observational isotope data from Antarctica, focussing especially on the East Antarctic low-accumulation area around the Kohnen Station ice-core drilling site, together with statistical and physical methods, to improve our understanding of the spatial and temporal isotope variability across different scales, and thus to enhance the applicability of the proxy for estimating past temperature variability. The presented results lead to a quantitative explanation of the local-scale (1–500 m) spatial variability in the form of a statistical noise model, and reveal the main source of the temporal variability to be the mixture of a climatic seasonal cycle in temperature and the effect of diffusional smoothing acting on temporally uncorrelated noise. These findings put significant limits on the representativity of single isotope records in terms of local air temperature, and impact the interpretation of apparent cyclicalities in the records. Furthermore, to extend the analyses to larger scales, the timescale-dependency of observed Holocene isotope variability is studied. This offers a deeper understanding of the nature of the variations, and is crucial for unravelling the embedded true temperature variability over a wide range of timescales.
    Type of Medium: Dissertations
    Pages: xxi, 197 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Contents: 1 General introduction. - 1.1 Challenges of isotope-based temperature reconstructions. - 1.2 Thesis overview. - 1.3 Author contributions. - 2 Theoretical background. - 2.1 The isotopic composition of firn and ice. - 2.1.1 Fractionation of water isotopologues. - 2.1.2 Relationship with temperature. - 2.1.3 Measuring of the isotopic composition. - 2.2 Processes within the firn column. - 2.2.1 The firn column of polar ice sheets. - 2.2.2 The density of firn. - 2.2.3 The temperature profile of firn. - 2.2.4 Vapour diffusion in firn. - 2.3 Internal climate variability. - 3 Regional climate signal vs.local noise: a two-dimensional view of water isotopes. - 3.1 Introduction. - 3.2 Data and methods. - 3.3 Results. - 3.3.1 Trench isotope records. - 3.3.2 Single-profile representativity. - 3.3.3 Mean trench profiles. - 3.3.4 Spatial correlation structure. - 3.3.5 Statistical noise model. - 3.4 Discussion. - 3.4.1 Local noise vs. regional climate signal. - 3.4.2 Representativity of isotope signals. - 3.4.3 Implications. - 3.5 Conclusions. - 3.6 Appendix A: Derivation of noise model. - 3.6.1 Definitions. - 3.6.2 Derivation of model correlations. - 3.6.3 Estimation of parameters. - 3.7 Appendix B: Noise level after diffusion. - 4 Constraints on post-depositional isotope modifications in east antarctic firn. - 4.1 Introduction. - 4.2 Data and methods. - 4.2.1 Sampling and measurements. - 4.2.2 Trench depth scale. - 4.2.3 Spatial variability of trench profiles. - 4.2.4 Quantification of downward advection, densification and diffusion. - 4.2.5 Statistical tests. - 4.3 Results. - 4.3.1 Comparison of T15 and T13 isotope data. - 4.3.2 Expected isotope profile changes. - 4.3.3 Temporal vs. spatial variability. - 4.4 Discussion. - 4.4.1 Densification, diffusion and stratigraphic noise. - 4.4.2 Additional post-depositional modifications. - 4.5 Conclusions. - 5 On the similarity and apparent cycles of isotope variations. - 5.1 Introduction. - 5.2 Data and Methods. - 5.2.1 Data. - 5.2.2 Spectral analysis. - 5.2.3 Rice’s formula. - 5.2.4 Cycle length and amplitude estimation. - 5.2.5 Model for vertical isotope profiles. - 5.3 Results. - 5.3.1 Spectral analysis of isotope profiles. - 5.3.2 Theoretical and observed cycle length. - 5.3.3 Illustrative examples. - 5.3.4 Depth dependency of cycle length. - 5.3.5 Simulated vs. observed isotope variations. - 5.4 Discussion and summary. - 5.5 Conclusions. - 5.6 Appendix A: Input sensitivity. - 5.7 Appendix B: Additional results. - 5.8 Appendix C: Spectral significance testing. - 6 Timescale-dependency of antarctic isotope variations. - 6.1 Introduction. - 6.2 Data and methods. - 6.2.1 DML and WAIS isotope records. - 6.2.2 Spectral model. - 6.2.3 Timescale-dependent signal-to-noise ratio. - 6.2.4 Effects of diffusion and time uncertainty. - 6.2.5 Present-day temperature decorrelation. - 6.3 Results. - 6.3.1 Illustration of model approach. - 6.3.2 DML and WAIS isotope variability. - 6.4 Discussion. - 6.4.1 Interpretation of noise spectra. - 6.4.2 Interpretation of signal spectra. - 6.4.3 Signal-to-noise ratios. - 6.4.4 Differences between DML and WAIS. - 6.5 Conclusions. - 7 Declining temperature variability from LGM to holocene. - 8 General discussion and conclusions. - 8.1 Short-scale spatial and temporal isotope variability. - 8.1.1 Local spatial variability. - 8.1.2 Seasonal to interannual variability. - 8.1.3 Spatial vs. temporal variability. - 8.2 Extension to longer scales. - 8.2.1 Spatial vs. temporal variability on interannual timescales. - 8.2.2 Holocene and longer timescales. - 8.3 Concluding remarks and outlook. - Bibliography. - A Methods to: declining temperature variability from lgm to holocene. - A.1 Temperature proxy data. - A.2 Model-based temperature and variability change. - A.3 Temperature recalibration of proxy records. - A.3.1 Recalibration of ice-core records. - A.3.2 Recalibration of marine records. - A.4 Variance and variance ratio estimation. - A.5 Noise correction. - A.5.1 Testing effect of noise correction. - A.6 Effect of ecological adaption and bioturbation. - A.7 Effect of proxy sampling locations. - B Layering of surface snow and firn: noise or seasonal signal?. - B.1 Introduction. - B.2 Materials and methods. - B.2.1 Firn-core density profiles. - B.2.2 Trench density profiles. - B.2.3 Dielectric profiling and density estimates. - B.2.4 Comparison of DEP and CT density. - B.2.5 Ion measurements. - B.3 Results. - B.3.1 2-D trench density data. - B.3.2 Spatial correlation structure. - B.3.3 Comparison of mean density, isotope and impurity profiles. - B.3.4 Spectral analysis of vertical density data. - B.4 Discussion. - B.4.1 Spatial variability. - B.4.2 Representativeness of single profiles. - B.4.3 Seasonal cycle in snow density. - B.4.4 Density layering in firn and impurities. - B.5 Conclusions. - Acknowledgements - Danksagung.
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  • 15
    Call number: AWI P5-18-91710
    Type of Medium: Monograph available for loan
    Pages: 24 S. , Ill.
    Edition: Stand: September 2015
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - Einleitung. - 1. Strategische Ziele der Arktisforschung. - 2. Die zentralen Fragen der Arktisforschung. - 2.1. Vergangenheit, Gegenwart und Zukunft des Klimawandels in der Arktis. - 2.2. Beitrag des grönländischen Inlandeises zur Meeresspiegelerhöhung. - 2.3. Rückgang des arktischen Meereises. - 2.4. Permafrost und Gashydrate als unbekannte Größen im Klimasystem. - 2.5. Anpassung polarer Organismen an die arktische Umwelt im Wandel. - 2.6. Chancen und Risiken zunehmender wirtschaftlicher Nutzung der Arktis. - 3. Stand der deutschen Polarforschung. - 3.1. Partner der deutschen Arktisforschung. - 3.2. Regionale Schwerpunkte der deutschen Arktisforschung. - 3.3. Positionierung im internationalen Umfeld. - 4. Umsetzung der Arktisforschungsstrategie. - 4.1. Forschung für Nachhaltigkeit. - 4.2. Wissenstransfer in die Gesellschaft. - 4.3. Technologietransfer. - 4.4. Nachwuchsförderung. - Anmerkungen. - Impressum.
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  • 16
    Call number: ZSP-760/A-15
    In: Terra Antartica reports, No. 15
    Type of Medium: Series available for loan
    Pages: 15 Seiten , Illustrationen , 8 Kartenbeilagen, 1 CD-ROM
    ISBN: 978-88-88395-12-8
    Series Statement: Terra Antartica reports 15
    Language: English
    Note: 1 Kartenbeilage unter dem Titel: Mount Melbourne Quadrangle (Victoria Land) 2012 / P. C. Pertusati, G. Musumeci, R. Carosi, M. Meccheri 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Reeves Névé Quadrangle (Victoria Land) 2012 / R. Casnedi, P. C. Pertusati, F. Salvini 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Mount Murchison Quadrangle (Victoria Land) 1997 / G. Capponi, M. Meccheri & P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Mount Joyce Quadrangle (Victoria Land) 1999 / G. Capponi, L. Crispini, M. Meccheri, G. Musumeci & P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Relief Inlet Quadrangle (Victoria Land) 1999 / G. Capponi, L. Crispini, M. Meccheri, G. Musumeci & P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Coulman Island Quadrangle (Victoria Land) 1997 / G. Capponi, M. Meccheri & G. Oggiano 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Sequence Hills Quadrangle (Victoria Land) 2012 / R. Carosi, M. Meccheri, G. Musumeci, P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Freyberg Mountains Quadrangle (Victoria Land) 2012 / G. Capponi, M. Meccheri, P. C. Pertusati 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series
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  • 17
    Monograph available for loan
    Monograph available for loan
    Hoboken, NJ : Wiley Blackwell
    Call number: AWI G3-18-91739
    Type of Medium: Monograph available for loan
    Pages: xxiii, 515 Seiten , Illustrationen, Diagramme, Karten , 26 cm
    Edition: Fourth edition
    Edition: edition first published 2018
    ISBN: 9781119132783 , 9781119132790 (electronic) , 9781119132813 (electronic)
    Language: English
    Note: Contents: Preface to Fourth Edition. - Preface to Third Edition. - Preface to Second Edition. - Preface to First Edition. - Acknowledgments. - PART I THE PERIGLACIAL DOMAIN. - 1 Introduction. - 1.1 The Periglacial Concept. - 1.2 Diagnostic Criteria. - 1.3 Periglacial Environments. - 1.4 The Periglacial Domain. - 1.5 The Periglacial Domain and the Cryosphere. - 1.6 Disciplinary Considerations. - 1.6.1 The Growth of Geocryology. - 1.6.2 The Challenge of Quaternary Science. - 1.6.3 Periglacial Geomorphology or Cold-Region Geomorphology?. - 1.7 Societal Considerations. - 1.8 The Growth of Periglacial Knowledge. - 2 Periglacial Climates. - 2.1 Boundary Conditions. - 2.2 Cold Deserts. - 2.3 Regional Climates. - 2.3.1 High Arctic Climates. - 2.3.2 Continental Climates. - 2.3.3 Alpine Climates. - 2.3.4 Montane Climates. - 2.3.5 Climates of Low Annual Temperature Range. - 2.3.6 Antarctica: A Special Case. - 2.4 Snow and Ice. - 2.5 Wind. - 2.6 Ground Climates. - 2.6.1 The 'n'-Factor. - 2.6.2 The Thermal Offset. - 2.6.3 The Ground Temperature Regime. - 2.7 Periglacial Climates and Global Climate Change. - 2.7.1 Basic Facts. - 2.7.2 Why Climate-Cryosphere Interactions Accelerate Climate Warming. - 3 Periglacial Ecosystems. - 3.1 General Statement. - 3.2 Biogeographic Zonation and Major Vegetation Types. - 3.3 Adaptations to Cold, Snow, Wind and Aridity. - 3.4 The Effect of Vegetation. - 3.5 The Polar Deserts. - 3.5.1 The High Arctic Polar Deserts. - 3.5.2 The High Arctic Polar Semi-Deserts. - 3.6 The Polar Desert-Tundra Transition. - 3.7 The Low-Arctic Tundra. - 3.8 The Forest-Tundra Bioclimatic Boundary (The Tree Line). - 3.9 The Boreal Forest. - 3.10 The Alpine and Montane Ecosystems. - 3.11 Antarctica - A Special Case. - 3.12 Periglacial Ecosystems and Climate Change. - PART II FROZEN GROUND AND PERMAFROST. - 4 Ground Freezing, Permafrost and the Active Layer. - 4.1 Introduction. - 4.2 Ground Freezing. - 4.2.1 Basic Concepts. - 4.2.2 Ice Segregation. - 4.2.3 "The Frozen Fringe'. - 4.2.4 Frost Heave. - 4.3 Perennially-Frozen Ground (Permafrost). - 4.4 Moisture and Ice Within Permafrost. - 4.5 Thermal and Physical Properties. - 4.5.1 The Geothermal Regime. - 4.5.2 The TTOP Model. - 4.5.3 Physical Properties. - 4.5.4 Thermal Properties. - 4.6 Permafrost Hydrology. - 4.6.1 Aquifers. - 4.6.2 Hydrochemistry. - 4.6.3 Groundwater Icings. - 4.7 The Active Layer. - 4.7.1 Terminology. - 4.7.2 The Active-Layer Thermal Regime. - 4.7.3 The Transient Layer. - 4.7.4 The Stefan Equation. - 5 Permafrost Distribution and Stability. - 5.1 Introduction. - 5.2 Controls over Permafrost Distribution. - 5.2.1 Relief and Aspect. - 5.2.2 Rock Type. - 5.2.3 Vegetation. - 5.2.4 Snow Cover. - 5.2.5 Fire. - 5.2.6 Lakes and Surface Water Bodies. - 5.3 Spatial Extent of Permafrost and Frozen Ground. - 5.3.1 Latitudinal Permafrost. - 5.3.2 Alpine (Mountain) Permafrost. - 5.3.3 Montane Permafrost. - 5.3.4 Seasonally-Frozen Ground. - 5.4 Sub-Sea and Relict Permafrost. - 5.4.1 Sub-Sea Permafrost. - 5.4.2 Relict (Terrestrial) Permafrost. - 5.5 Permafrost and Ecosystems. - 5.6 Permafrost Monitoring and Mapping. - 5.6.1 CALM and GTN-P (TSP). - 5.6.2 BTS and Mountain Permafrost Probability Mapping. - 5.7 Climate Warming and Permafrost. - 5.7.1 Evidence for Warming Permafrost. - 5.7.2 Evidence for Thawing Permafrost. - 6 Ground Ice and Cryostratigraphy. - 6.1 Introduction. - 6.2 Quantitative Parameters. - 6.3 Epigenetic, Syngenetic and Polygenetic Permafrost. - 6.4 Classification. - 6.4.1 The Russian Approach. - 6.4.2 The North American Approach. - 6.5 Main Ground Ice Types. - 6.5.1 Pore Ice. - 6.5.2 Segregated Ice. - 6.5.3 Intrusive Ice. - 6.5.4 Vein Ice. - 6.5.5 Other Types of Ice. - 6.6 Ice Distribution. - 6.6.1 Amounts. - 6.6.2 Distribution with Depth. - 6.6.3 Ice in Bedrock. - 6.6.4 Ice in Poorly-Lithified Sediments. - 6.7 Cryostratigraphy and Cryolithology. - 6.7.1 Cryostructural Analysis. - 6.7.2 Cryostructures of Epigenetic and Syngenetic Permafrost. - 6.7.3 Thaw Unconformities. - 6.7.4 Aggradational Ice. - 6.7.5 Icy Bodies and Ice, Sand and Soil Pseudomorphs. - 6.8 Ice Crystallography. - 6.9 Ice Geochemistry. - 6.10 Massive Ice and Massive-Icy Bodies. - 6.10.1 Nature and Extent. - 6.10.2 Intra-Sedimental Ice. - 6.10.3 Buried Glacier Ice. - 6.11 Cryostratigraphy and Past Environments. - 7 Aggradational Permafrost Landforms. - 7.1 Introduction. - 7.2 How Does Permafrost Aggrade?. - 7.2.1 The Illisarvik Drained-Lake Experiment. - 7.3 Thermal-Contraction-Crack Polygons. - 7.3.1 Coefficients of Thermal Expansion and Contraction. - 7.3.2 Ice, Sand and Soil ('Ground') Wedges. - 7.3.3 Development of the Polygon Net. - 7.3.4 Polygon Morphology. - 7.3.5 Controls over Cracking. - 7.3.6 Climatic Significance. - 7.4 Ice and Sand Wedges. - 7.4.1 Epigenetic Wedges. - 7.4.2 Syngenetic Wedges. - 7.4.3 Anti-Syngenetic Wedges. - 7.4.4 Growth and Deformation of Wedges. - 7.5 Organic Terrain. - 7.5.1 Palsas. - 7.5.2 Peat Plateaus. - 7.6 Frost Mounds. - 7.6.1 Perennial-Frost Mounds. - 7.6.2 Hydraulic (Open) System Pingos. - 7.6.3 Hydrostatic (Closed) System Pingos. - 7.6.4 Other Perennial-Frost Mounds. - 7.6.5 Seasonal-Frost Mounds. - 7.6.6 Hydrolaccoliths and Other Frost-Induced Mounds. - 8 Thermokarst Processes and Landforms. - 8.1 Introduction. - 8.2 Thawing Ground. - 8.2.1 Thaw Strain and Thaw Settlement. - 8.2.2 Potential Depths of Soil Freezing and Thawing. - 8.2.3 The Development of Thermokarst. - 8.3 Causes of Thermokarst. - 8.3.1 General Comments. - 8.3.2 Specific Causes. - 8.4 Thaw-Related Processes. - 8.4.1 Thermokarst Subsidence (Thaw Settlement). - 8.4.2 Thermal Erosion. - 8.4.3 Other Processes. - 8.5 Thermokarst Sediments and Structures. - 8.5.1 Involuted Structures. - 8.5.2 Retrogressive-Thaw-Slumps and Debris-Flow Deposits. - 8.5.3 Ice-Wedge Pseudomorphs and Composite-Wedge Casts. - 8.5.4 Ice, Silt, Sand and Gravel Pseudomorphs. - 8.6 Thermokarst Landscapes. - 8.6.1 The Alas-Thermokarst Relief of Central Yakutia. - 8.6.2 The Western North American Arctic. - 8.6.3 The Ice-Free Areas of Continental Antarctica. - 8.7 Ice-Wedge Thermokarst Relief. - 8.7.1 Low-Centred Polygons. - 8.7.2 High-Centred Polygons. - 8.7.3 Badland Thermokarst Relief. - 8.8 Thaw Lakes and Depressions. - 8.8.1 Lakes and Taliks. - 8.8.2 Morphology. - 8.8.3 Growth and Drainage. - 8.8.4 Oriented Thaw Lakes. - Part III Periglacial Geomorphology. - 9 Cold-Climate Weathering. - 9.1 Introduction. - 9.2 General Weathering Facts. - 9.3 Freezing and Thawing Indices. - 9.4 Rock (Frost?) Shattering. - 9.4.1 Frost Action and Ice Segregation. - 9.4.2 Insolation and Thermal Shock. - 9.4.3 Perspective. - 9.5 Chemical Weathering. - 9.5.1 Karkevagge. - 9.5.2 Solution and Karstification. - 9.5.3 Salt Weathering. - 9.6 Cryogenic Weathering. - 9.6.1 Cryogenic Disintegration. - 9.6.2 The Coefficient of Cryogenic Contrast. - 9.6.3 Physico-Chemical Changes. - 9.6.4 Problematic Phenomena. - 9.7 Cryobiological Weathering. - 9.8 Rates of Cold-Climate Bedrock Weathering. - 9.9 Cryosols and Cryopedology. - 9.9.1 Cryosols. - 9.9.2 Classification. - 9.9.3 Cryosolic Micromorphology. - 10 Mass-Wasting Processes and Active-Layer Phenomena. - 10.1 Introduction. - 10.2 Slow Mass-Wasting Processes. - 10.2.1 Solifluction. - 10.2.2 Frost Creep. - 10.2.3 Gelifluction. - 10.2.4 Solifluction Deposits and Phenomena. - 10.3 Rapid Mass-Wasting Processes. - 10.3.1 Active-Layer-Detachment Slides. - 10.3.2 Debris Flows, Slush Flows and Avalanches. - 10.3.3 Rockfall. - 10.4 Snow Hydrology and Slopewash Processes. - 10.4.1 Snow Hydrology and Snowbanks. - 10.4.2 Surface and Subsurface Wash. - 10.5 Active-Layer Phenomena. - 10.5.1 Frost Heaving. - 10.5.2 Bedrock Heave. - 10.5.3 Upward Heaving of Stones and Objects. - 10.5.4 Stone Tilting. - 10.5.5 Ne
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  • 18
    Monograph available for loan
    Monograph available for loan
    Bremen : Übersee-Museum Bremen
    Call number: AWI P6-18-91708
    Type of Medium: Monograph available for loan
    Pages: 176 Seiten , Illustrationen , 24 cm
    Edition: [1. Auflage]
    ISBN: 978-3-89946-286-9
    Series Statement: TenDenZen 2018,26
    Language: German
    Note: Inhalt: Grußwort - Antje Boetius. - Vorwort - Michaela Grein. - Die Welt teilhaben lassen - Luc Jacquet über die Sonderausstellung „Antarctica". - Die Geschichte der Antarktisforschung. - Die Entdeckung und Erforschung der Antarktis / Diedrich Fritzsche. - Die Gründung des Alfred-Wegener-Instituts für Polarforschung / Gotthilf Hempel. - Frauen in der Antarktis / Gotthilf Hempel. - Geologie und Klima. - Der geologische Bau der Antarktis / Andreas Läufer. - Einfluss des Ozeans auf das Schmelzen der Eisschelfe / Sunke Schmidtko. - Aurora australis - Polarlichter in der Antarktis / Michaela Grein. - Lebensräume und Organismengruppen. - Antarktische Makroalgen / Katharina Zacher & Christian Wiencke. - Leben am Meeresboden und Wiederbesiedlungsdynamik / Julian Gutt. - Die Schwämme des antarktischen Meeres / Dorte Janussen. - Schuppenwürmer in der Antarktis / Michael Stiller. - Meiofauna: Kleine Tiere - große Wirkung / Gritta Veit-Köhler & Friederike Säring. - Der antarktische Krill, Euphausia superba, im Nahrungsnetz des Südpolarmeers / Bettina Meyer. - Der Kaiserpinguin - Bedrohte Tierart und Stellvertreter für den Südozean / Daniel P. Zitterbart. - Fliegende Vögel der Antarktis / Hans-Ulrich Peter. - Antarktische Robben / Horst Bornemann & Joachim Plötz. - Pioniere und Überlebenskünstler: Die Flechten / Ludger Kappen. - Die Evolution der Wälder in Antarktika / Laura Jane Tilley. - Pflanzen in Antarktika / Michaela Grein. - Nutzung und Schutz der Antarktis. - Umweltschutz in der Antarktis / Heike Herata. - Meeresschutz in der Antarktis / Bob Zuur. - Tourismus in der Antarktis / Heinz Klöser. - Die Autorinnen und Autoren.
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  • 19
    Call number: PIK N 456-18-91895 ; AWI A5-18-91895
    Type of Medium: Monograph available for loan
    Pages: xv, 569 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9780128117149
    Language: English
    Note: Contents: Contributors. - Preface. - Acknowledgements. - PART I SETTING THE SCENE. - 1. Introduction: Why Sub-seasonal to Seasonal Prediction (S2S)? / Frédéric Vitart, Andrew W. Robertson. - 1 History of Numerical Weather and Climate Forecasting. - 2 Sub-seasonal to Seasonal Forecasting. - 3 Recent National and International Efforts on Sub-seasonal to Seasonal Prediction. - 4 Structure of This Book. - 2. Weather Forecasting: What Sets the Forecast Skill Horizon? / Zoltan Toth, Roberto Buizza. - 1 Introduction. - 2 The Basics of Numerical Weather Prediction. - 3 The Evolution of NWP Technique. - 4 Enhancement of Predictable signals. - 5 Ensemble Techniques: Brief Introduction. - 6 Expanding the forecast skill Horizon. - 7 Concludmg Remarks: Lessons for S2S Forecasting. - Acknowledgements. - 3. Weather Within Climate: Sub-seasonal Predictability of Tropical Daily Rainfall Characteristics / Vincent Moron, Andrew W. Robertson, Lei Wang. - 1 Introduction. - 2 Data and Methods. - 3 Results. - 4 Discussion and Concluding Remarks. - 4. Identifying Wave Processes Associated With Predictability Across Time Scales: An Empirical Normal Mode Approach / Gilbert Brunet, John Methven. - 1 Introduction. - 2 Partitioning Atmospheric Behavior Using Its Conservation Properties. - 3 The ENM Approach to Observed Data and Models and Its Relevance to S2S Dynamics and Predictability. - 4 Conclusion. - Acknowledgments. - PART II SOURCES OF S2S PREDICTABILITY. - 5. The Madden-Julian Oscillation / Steven J. Woolnough. - 1 Introduction. - 2 The Real-Time Multivariate MJO Index. - 3 Observed MJO Structure. - 4 The Relationship Between the MJO and Tropical and Extratropical Weather. - 5 Theories and Mechanisms for MJO Initiation, Maintenance, and Propagation. - 6 The Representation of the MJO in Weather and Climate Models. - 7 MJO Prediction. - 8 Future Priorities for MJO Research for S2S Prediction. - Acknowledgments. - 6. Extratropical Sub-seasonal to Seasonal Oscillations and Multiple Regimes: The Dynamical Systems View / Michael Ghil, Andreas Groth, Dmitri Kondrashov, Andrew W. Robertson. - 1 Introduction and Motivation. - 2 Multiple Midlatitude Regimes and Low-Frequency Oscillations. - 3 Extratropical Oscillations in the S2S Band. - 4 Low-Order, Data-Driven Modeling, Dynamical Analysis, and Prediction. - 5 Concluding Remarks. - Acknowledgments. - 7. Tropical-Extratropical Interactions and Teleconnections / Hai Lin, Jorgen Frederiksen, David Straus, Christiana Stan. - 1 Introduction. - 2 Tropical Influence on the Extratropical Atmosphere. - 3 Extratropical Influence on the Tropics. - 4 Tropical-Extratropical, Two-Way Interactions. - 5 Summary and Discussion. - Appendix. Technical Matters Relating to Section 4.2. - 8. Land Surface Processes Relevant to Sub-seasonal to Seasonal (S2S) Prediction / Paul A. Dirmeyer, Pierre Gentine, Michael B. Ek, Gianpaolo Balsamo. - 1 Introduction. - 2 Process of Land-Atmosphere Interaction. - 3 A Brief History of Land-Surface Models. - 4 Predictability and Prediction. - 5 Improving Land-Driven Prediction. - 9. Midlatitude Mesoscale Ocean-Atmosphere Interaction and Its Relevance to S2S Prediction / R. Saravanan, P. Chang. - 1 Introduction. - 2 Data and Models. - 3 Mesoscale Ocean-Atmosphere Interaction in the Atmospheric Boundary Layer. - 4 Local Tropospheric Response. - 5 Remote Tropospheric Response. - 6 Impact on Ocean Circulation. - 7 Implications for S2S Prediction. - 8 Summary and Conclusions. - Acknowledgments. - 10. The Role of Sea Ice in Sub-seasonal Predictability / Matthieu Chevallier, François Massonnet, Helge Goessling, Virginie Guémas, Thomas Jung. - 1 Introduction. - 2 Sea Ice in the Coupled Atmosphere-Ocean System. - 3 Sea Ice Distribution, Seasonality, and Variability. - 4 Sources of Sea Ice Predictability at the Sub-seasonal to Seasonal Timescale. - 5 Sea Ice Sub-seasonal to Seasonal - Predictability and Prediction Skill in Models. - 6 Impact of Sea Ice on Sub-seasonal Predictability. - 7 Concluding Remarks. - Acknowledgments. - 11. Sub-seasonal Predictability and the Stratosphere / Amy Butler, Andrew Charlton-Perez, Daniela I. V. Domeisen, Chaim Garfinkel, Edwin P. Gerber, Peter Hitchcock, Alexey Yu. Karpechko, Amanda C. Maycock, Michael Sigmond, Isla Simpson, Seok-Woo Son. - 1 Introduction. - 2 Stratosphere-Troposphere Coup ling in the Tropics. - 3 Stratosphere-Troposphere Coupling in the Extratropics. - 4 Predictability Related to Extratropical Stratosphere-Troposphere Coupling. - 5 Summary and Outlook. - PART Ill S2S MODELING AND FORECASTING. - 12. Forecast System Design, Configuration, and Complexity / Yuhei Takaya. - 1 Introduction. - 2 Requirements and Constraints of the Operational Sub-seasonal Forecast. - 3 Effect of Ensemble Size and Lagged Ensemble. - 4 Real-Time Forecast Configuration. - 5 Reforecast Configuration. - 6 Summary and Concluding Remarks. - Acknowledgments. - 13. Ensemble Generation: The TIGGE and S2S Ensembles / Roberto Buizza. - 1 Global Sub-seasonal and Seasonal Prediction Is an Initial Value Problem. - 2 Ensembles Provide More Complete and Valuable Information Than Single States. - 3 A Brief Introduction to Data Assimilation. - 4 A Brief Introduction to Model Uncertainty Simulation. - 5 An Overview of Operational, Global, Sub-seasonal, and Seasonal Ensembles, and Their Initialization and Generation Methods. - 6 Ensembles: Considerations About Their Future. - 7 Summary and Key Lessons. - 14. GCMs With Full Representation of Cloud Microphysics and Their MJO Simulations / In-Sik Kang, Min-Seop Ahn, Hiroaki Miura, Aneesh Subramanian. - 1 Introduction. - 2 Global CRM. - 3 Superparameterized GCM. - 4 GCM With Full Representation of Cloud Microphysics and Scale-Adaptive Convection. - 5 Summary and Conclusion. - Acknowledgments. - 15. Forecast Recalibration and Multimodel Combination / Stefan Siegert, David B. Stephenson. - 1 Introduction. - 2 Statistical Methods for Forecast Recalibration. - 3 Regression Methods. - 4 Forecast Combination. - 5 Concluding Remarks. - Acknowledgments. - 16. Forecast Verification for S2S Timescales / Caio A. S. Coelho, Barbara Brown, Laurie Wilson, Marion Mittermaier, Barbara Casati. - 1 Introduction. - 2 Factors Affecting the Design of Verification Studies. - 3 Observational References. - 4 Review of the Most Common Verification Measures. - 5 Types of S2S Forecasts and Current Verification Practices. - 6 Summary, Challenges, and Recommendations in S2S Verification. - PART IV S2S APPLICATIONS. - 17. Sub-seasonal to Seasonal Prediction of Weather Extremes / Frédérik Vitart, Christopher Cunningham, Michael Deflorio, Emanuel Dutra, Laura Ferranti, Brian Golding, Debra Hudson, Charles Jones, Christophe Lavaysse, Joanne Robbins, Michael K. Tippett. - 1 Introduction. - 2 Prediction of Large-Scale, Long-Lasting Extreme Events. - 3 Prediction of Mesoscale Events. - 4 Display and Verification of Sub-seasonal Forecasts of Extreme Events. - 5 Conclusions. - 18. Pilot Experiences in Using Seamless Forecasts for Early Action: The "Ready-Set-Go!" Approach in the Red Cross / Juan Bazo, Roop Singh, Mathieu Destrooper, Erin Coughlan de Perez. - 1 Introduction. - 2 Why Sub-seasonal?. - 3 Case Study: Peru El Niño. - 4 Reflections on the Use of S2S Forecasts. - 5 Conclusions. - 19. Communication and Dissemination of Forecasts and Engaging User Communities / Joanne Robbins, Christopher Cunningham, Rutger Dankers, Matthew Degennaro, Giovanni Dolif, Robyn Duell, Victor Marchezini, Brian Mills, Juan Pablo Sarmiento, Amber Silver, Rachel Trajber, Andrew Watkins. - 1 Introduction. - 2 Sector-Specific Methods and Practices in S2S Forecast Communication, Dissemination, and Engagement. - 3 Guiding principles for improved communication Practices. - 4 Summary and Recommendations for Future Research. - 20. Seamless Prediction of Monsoon Onset and Active/Break Phases / A.
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  • 20
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : International Arctic Science Committee
    Call number: AWI A4-19-92792
    Type of Medium: Monograph available for loan
    Pages: 99 Seiten , Illustrationen
    Edition: April 2018
    Language: English
    Note: TABLE OF CONTENTS SUMMARY 1. BACKGROUND AND OVERARCHING GOALS OF MOSAiC 2. MEASUREMENTS AND REQUIREMENTS 2.1 Atmosphere (team ATMOS) 2.2 Sea Ice and Snow Cover (team ICE) 2.3 Ocean (team OCEAN) 2.4 Bio-geochemical System (team BGC) 2.5 Ecosystem (team ECO) 2.6 Cross-team coordination 3. OBSERVATIONAL SCALES AND SCIENTIFIC-TECHNICAL IMPLEMENTATION 3.1 Installations, Labs, and Containers on Polarstern 3.2 Major Installations on/in/under the Central lee Camp 3.3 Deployment and Operation ofthe Distributed Network 3.4 Airborne Observations 3.5 Hovercraft Observations 3.6. Other Main Platforms 3.7 Intensive Observation Periods 3.8 Events 4. PRACTICAL/ LOGISTICAL ASPECTS 4.1 Detailed Time Line (2016-2022) 4.2 Drift Trajectory and Re-supply 4.3 Personnel and Personnel Exchange 4.4 Routine Operations during the Drift 4.5 Governance Structure 4.6 Rescue and Alternative Plans 4.7 Safety Aspects during the Drift 4.8 Impacts of Polarstern on Measurements and Environment 4.9 Outreach and Media Concept 4.10 Preparation and summary workshops, conferences 5. IMPLEMENTATION OF REMOTE SENSING 5.1 Pre-drift Coordination of the Remote Sensing Program 5.2 Acquisition of Satellite Data during the Drift 5.3 Coordination with In-situ Measurements 6. IMPLEMENTATION OF NUMERICAL MODELS 6.1 Operational Forecast and Reanalysis Products of the MOSAiC Drift 6.2 Data Assimilation Studies 6.3 Process and Regional Modeling of the Sub-systems 6.4 Coupled Climate Modeling 7. DATA POLICY AND MANAGEMENT PLAN 7.1 Outcome ofthe St. Petersburg Implementation Workshop 7.2 The MOSAiC Data Group: Development ofthe Data Management Plan 7.3 The Technical Concept for Supporting the Data Life Cycle in MOSAiC 7.4 The Role of PANGAEA as MOSAiC Data Repository 7.5 Project Data Management and Publication 8. LINKS TO EXTERNAL PROGRAMS AND PROJECTS 8.1 Cooperation with External Projects and Programs 8.2 Cooperation with Parallel Experiments 9. APPENDIX 9.1 Preliminary Tables of Parameters for Sections 2.1 to 2.5 9.2 Preliminary Table of Partners 9.3 List of Abbreviations
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  • 21
    Call number: AWI G3-19-92414
    Description / Table of Contents: Permafrost, defined as ground that remains frozen for at least two consecutive years, is a prominent feature of polar regions. In the Northern Hemisphere, approximately 23 million km2 of the ground are affected by permafrost. Climatic warming, which has a greater effect on the Arctic than on any other region on Earth, leads to permafrost thaw, caused by gradual deepening of the seasonal unfrozen layer (active layer), thermokarst formation (i.e. land subsidence due to ground ice loss) and thermo-erosion. In the course of thaw, formerly freeze-locked organic carbon (OC) is mobilized and mineralized into greenhouse gases (GHGs), fostering further climate warming – a process known as permafrost carbon feedback. Current climate models focus on GHG release from gradual deepening of the active layer and neglect the OC turnover during lateral transport induced by thermokarst and abrupt thermo-erosion. As such, the accelerated erosion of Arctic permafrost coasts, which make up ~34 % of the global coasts, deliver vast amounts of OC into the Arctic Ocean. However, little is known about the amounts of labile and fast bioavailable dissolved OC (DOC), the impact of thermokarst on mobilized organic matter (OM) characteristics, and the release of GHGs from eroding permafrost coasts. To fill that knowledge gap, the main objectives of the thesis are to investigate (i) how much DOC is mobilized from coastal erosion, (ii) how thermokarst and -erosion alters OM characteristics upon thaw on transit to the ocean, and (iii) how much GHGs are emitted from the nearshore zones of eroding permafrost coasts. Field work and sampling took place along the Yukon coast and on Qikiqtaruk (Herschel Island) in the western Canadian Arctic. An interdisciplinary approach was used to quantify OM (OC and nitrogen) as well as to identify degradation processes. The methods used included sedimentology, geo- and hydrochemistry, remote sensing, statistical analyses, and gas chromatography. The thesis shows that considerable amounts of DOC are released from eroding permafrost coasts. Although OC fluxes into the ocean are dominated by DOC from Arctic rivers and particulate OC (POC), labile DOC derived from permafrost plays an important role as it is quickly available for biogeochemical cycling and turnover into GHGs. During transit from land to ocean OM characteristics are substantially altered by thermokarst formation and thermo-erosion. In mudpools, originating from in-situ thawed permafrost, as well as in thaw streams draining thermokarst features towards the ocean, mobilized OM issubject to dilution with melted ground ice and degradation, which result in a decrease of OM contents by more than 50 %. The turnover of OC continues in the nearshore zone. The biochemically most labile OC portions are rapidly lost within months and mineralized into GHGs. The production of GHGs in the ocean is 60 to 80 % as efficient as on land and primarily in form of carbon dioxide (CO2), due to aerobic conditions in the nearshore zone. During each open water season in the Arctic approximately 0.7 to 1.2 Tg of CO2 are emitted from the coastal fringe. The remaining OM is buried in nearshore and shelf sediments, potentially remobilized by waves, currents and ice scouring at later stages. To conclude, the thesis shows that eroding permafrost coasts release large amounts of OC, from which considerable portions are labile DOC. In the course of thermokarst formation and thermo-erosion, OM is diluted and the most labile portions subject to rapid turnover into GHGs. This shows that eroding permafrost coasts are a major yet neglected source of CO2 to the atmosphere. With increasing temperatures and longer sea ice-free conditions projected for the Arctic, the erosion of permafrost coasts accelerates. Consequently, the transfer of OC to the ocean accompanied by GHG production increases, which is expected to have drastic impacts for the climate and coastal ecosystems.
    Type of Medium: Dissertations
    Pages: IX, 106, A1-A-57 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Table of contents Abstract Zusammenfassung Abbreviations and nomenclatureI 1. Introduction 1.1 Scientific background 1.1.1 Permafrost and ground ice 1.1.2 Organic carbon pools and fluxes into the Arctic Ocean 1.1.3 Climate warming and permafrost thaw 1.1.4 Permafrost degradation and coastal erosion 1.1.5 Study area Yukon coast and Qikiqtaruk 1.2 Knowledge gaps 1.3 Aims and objectives 1.4 Thesis structure and author's contribution 2. Eroding permafrost coasts release low amounts of dissolved organic carbon (DOC) from ground ice into the nearshore zone of the Arctic Ocean 2.1 Abstract 2.2 Introduction 2.3 Study area 2.4 Methods 2.4.1 Field work 2.4.2 DOC concentration 2.4.3 DOC flux estimation 2.5 Results 2.5.1 Segmentation of the coast - literature synthesis 2.5.2 DOC concentration 2.5.3 DOC stocks and fluxes 2.6 Discussion 2.6.1 DOC concentrations in ground ice 2.6.2 DOC fluxes from the YC 2.6.3 DOC fluxes and the Arctic carbon budget 2.7 Conclusion and Outlook 2.8 Acknowledgements 3.Transformation of terrestrial organic matter along thermokarst-affected permafrost coasts in the Arctic 3.1 Abstract 3.2 Introduction 3.3 Study area 3.3 Methods 3.3.1 Field work 3.3.2 Sedimentology, stratigraphy, and vegetation 3.3.3 Organic matter 3.3.4 Statistics 3.3.5 Transformation of organic matter 3.3.6 Fate of organic matter in the nearshore zone 3.4 Results 3.4.1 Sedimentology, stratigraphy, and vegetation 3.4.2 Organic matter 3.4.3 C/N-ratios and δ13C 3.4.4 Biomarkers 3.5 Discussion 3.5.1 Transformation of organic matter in the disturbed zone 3.5.2 Fate of organic matter in the nearshore zone 3.5.3 Environmental impact of the RTS 3.6 Conclusion 3.7 Acknowledgements 4. Rapid greenhouse gas release from eroding permafrost coasts 4.1 Summary 4.2 Background 4.3 Study site 4.4 Sampling and incubation setup 4.5 Findings and discussion 4.6 Conclusion 4.7 Methods 4.7.1 Incubation conditions 4.7.2 Gas measurements 4.7.3 Geo- and hydrochemical analysis 4.8 Acknowledgements 5. Synthesis 5.1 Mobilization of permafrost OC pools by coastal erosion 5.2 Transformation of permafrost OM on transit from land to sea 5.3 Fate and pathways of permafrost OC in the nearshore zone 5.4 Conclusion and outlook References Appendix I: Dissolved organic carbon (DOC) in Arctic ground ice I-1 Abstract I-2 Introduction I-3 Study area and study sites I-4 Material and methods I-4-1 Laboratory analyses I-4-2 Statistical methods I-5 Results I-5-1 DOC and DIC concentrations I-5-2 Correlation matrix I-5-3 Principal components I-5-4 Univariate Tree Model (UTM) I-6 Discussion I-6-1 DOC stocks in ground ice and relevance to carbon cycling I-6-2 Carbon sequestration and origin in relation to inorganic geochemistry I-6-3 DOC mobility and quality upon permafrost degradation I-7 Conclusions and outlook I-8 Acknowledgements Appendix II: Supplementary material for Chapter 2 II-1 Supplementary table - Ground ice and geochemical data II-2 Supplementary table - Coastal segments and DOC flux Appendix III: Supplementary material for Chapter 3 III-1 Normalized Differenced Vegetation Index map III-2 Photograph of a massive ice bed in a RTS III-3 Calculation of biomarker proxies III-4 Supplementary table - Summary of geochemical data III-5 Supplementary table - Summary of statistical analysis AppendixI V: Supplementary material for Chapter 4 IV-1 Design of the incubation experiment IV-2 Photograph of a standard incubation setup IV-3 Conversion of gas amounts into mass IV-4 Total and daily aerobic CH4 production IV-5 Histogram summarizing OC losses and CO2 emissions IV-6 Supplementary table - Summary of TOC, DOC, and pH data IV-7 Supplementary table - Summary of TN, TOC/TN, and δ13C-TOC data IV-8 Supplementary table - Summary of total CO2 and CH4 production data IV-9 Supplementary table - Comparison of incubation setups IV-10 Supplementary table - Summary of daily CO2 production data IV-11 Supplementary table - Summary of daily CH4 production data Acknowledgements-Danksagung
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  • 22
    Call number: AWI G3-19-92460
    Description / Table of Contents: The Yukon Coast in Canada is an ice-rich permafrost coast and highly sensitive to changing environmental conditions. Retrogressive thaw slumps are a common thermoerosion feature along this coast, and develop through the thawing of exposed ice-rich permafrost on slopes and removal of accumulating debris. They contribute large amounts of sediment, including organic carbon and nitrogen, to the nearshore zone. The objective of this study was to 1) identify the climatic and geomorphological drivers of sediment-meltwater release, 2) quantify the amount of released meltwater, sediment, organic carbon and nitrogen, and 3) project the evolution of sediment-meltwater release of retrogressive thaw slumps in a changing future climate. The analysis is based on data collected over 18 days in July 2013 and 18 days in August 2012. A cut-throat flume was set up in the main sediment-meltwater channel of the largest retrogressive thaw slump on Herschel Island. In addition, two weather stations, one on top of the undisturbed tundra and one on the…
    Type of Medium: Monograph available for loan
    Pages: 163 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Table of Contents Abstract Kurzfassung Abbreviations and nomenclature 1. Introduction 2. Scientific Background 2.1. Permafrost 2.2.Retrogressive Thaw Slumps 2.3. Inputs of Freshwater, Sediment and Carbon into the Canadian Beaufort Sea 3. Study Area 3.1. Regional Setting: Yukon Coast and Herschel Island 3.2. Retrogressive Thaw Slumps 4. Material and Methods 4.1. Field Work 4.1.1. Terrain Photography 4.1.2. Differential Global Positioning System (DGPS) 4.1.3. Light Detection And Ranging (LiDAR) and Digital Elevation Model (DEM) 4.1.4. Micrometeorology 4.1.5. Discharge Measurement 4.1.6. Multiple Regression-Statistical Relationships between Micrometeorological Variables and Discharge 4.1.7. Sampling 4.2. Laboratory Analyses 4.2.1. Sedimentological Analyses 4.2.2. Hydrochemical Analyses 4.3. Fluxes of Sediment and (In-) Organic Matter 5. Results 5.1. Field Work 5.1.1. Terrain Photography 5.1.2. Differential Global Positioning System (DGPS) 5.1.3. Light Detecting And Ranging (LiDAR) and Digital Elevation Model (DEM) 5.1.4. Micrometeorology 5.1.5. Discharge 5.1.6. Multiple Regression - Statistical Relationships between Micrometeorology and Discharge 5.2. Laboratory Analyses 5.2.1. Sedimentological Analyses 5.2.2. Hydrochemical Analyses 5.3. Fluxes of Sediment-meltwater 6. Discussion 6.1. Microclimatological and Geomorphological Factors Controlling Discharge 6.1.1. Diurnal Variations 6.1.2. Seasonal Variations 6.2. Contribution of Retrogressive Thaw Slumps to the Sediment Budget of the Yukon Coast 6.2.1. Origin of Outflow Material 6.2.2. Slump D in the Regional Context 6.2.3. Seasonal Sediment Budget Compilation for Slump D 6.2.4. Retrogressive Thaw Slump Occurrence along the Yukon Coast 6.2.5. Input to the Beaufort Sea 6.3. Projected Climatic Change and its Impact on Retrogressive Thaw Slump Outflow 6.4. Uncertainties and Limitations 6.5. Future Research 7. Conclusion 8. Appendix 8.1. Field Work 8.1.1. Slump D's northern headwall profile 8.1.2. Collinson Head slump 8.1.3. Herschel Island West Coast slump 8.1.4. Roland Bay slump 8.1.5. Kay Point slump 8.2. Laboratory Work 8.2.1. Volumetric Ice Content 8.2.2. Grain Size 8.3. Evolution of Slump D 8.3.1. Geo Eye satellite of Slump D 8.3.2. Aerial Oblique Photography of Slump D 8.3.3. LiDAR of Slump D 8.3.4. Time Lapse Photography of Slump D's Headwall 9. References 10. Financial and technical support 11. Acknowledgement - Danksagung
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  • 23
    Call number: AWI G3-19-92415
    Type of Medium: Dissertations
    Pages: VIII, 154, xv Seiten , Illustrationen, Diagramme, Karten
    Language: English
    Note: Table of contents Abstract Zusammenfassung 1 Motivation 2 Introduction 2.1 Arctic climate changes and their impacts on Coastal processes 2.2 Shoreline retreat along Arctic coasts 2.3 Impacts of Coastal erosion 2.3.1 Material fluxes 2.3.2 Retrogressive thaw slumps 2.3.3 Socio-economic impacts 2.4 Objectives 2.5 Study area 2.6 Thesis structure 2.7 Authors’ contributions 3 Variability in rates of Coastal change along the Yukon coast, 1951 to 2015 3.1 Introduction 3.2 Study Area 3.3 Data and Methods 3.3.1 Remote sensing data 3.3.2 Field survey data 3.3.3 Classification of shoreline 3.3.4 Transect-wise analyses of shoreline movements through time 3.4 Results 3.4.1 Temporal variations in shoreline change rates 3.4.2 Alongshore rates of change 3.4.3 Shoreline dynamics along field sites 3.4.4 Dynamics of lagoons, barrier Islands and spits (gravel features) 3.4.5 Yukon Territory land loss 3.5 Discussion 3.5.1 Temporal variations in shoreline change rates 3.5.2 Alongshore rates of change 3.5.3 Dynamics of lagoons, barrier Islands, and spits (gravel features) 3.5.4 Expected shoreline changes as a consequence of future climate warming 3.6 Conclusions Context 4 Coastal erosion of permafrost Solls along the Yukon Coastal Plain and Kuxes oforganic carbon to the Canadian Beaufort Sea 4.1 Introduction 4.2 Study Area 4.3 Methods 4.3.1 Sample collection and laboratory analyses 4.3.2 Soll organic carbon determinations 4.3.3 Flux of organic soil carbon and Sediments 4.3.4 Fate of the eroded soil organic carbon 4.4 Results 4.4.1 Ground lce 4.4.2 Organic carbon contents 4.4.3 Material fluxes 4.5 Discussion 4.5.1 Ground lce 4.5.2 Organic carbon contents 4.5.3 Material fluxes 4.5.4 Organic carbon in nearshore Sediments 4.6 Conclusion Context 5 Terrain Controls on the occurrence of Coastal retrogressive thaw slumpsalong the Yukon Coast, Canada 5.1 Introduction 5.2 Study Area 5.3 Methods 5.3.1 Mapping of RTSs and landform Classification 5.3.2 Environmental variables 5.3.3 Univariate regression trees 5.4 Results 5.4.1 Characteristics of RTS along the coast 5.4.2 Density and areal coverage od RTSs along the Yukon Coast 5.5 Discussion 5.5.1 Characteristics and distribution of RTSs along the Yukon Coast 5.5.2 Terrain factors explaining RTS occurrence 5.5.3 Coastal processes 5.6 Conclusions Context 6 Impacts of past and fiiture Coastal changes on the Yukon coast - threats forcultural sites, infrastructure and travel routes 6.1 Introduction 6.2 Study Area 6.3 Methods 6.3.1 Data for shoreline projections 6.3.2 Shoreline projection for the conservative scenario (S1) 6.3.3 Shoreline Projection for the dynamic scenario (S2) 6.3.4 Positioning and characterizing of cultural sites 6.3.5 Calculation of losses under the S1 and S2 scenarios 6.3.6 Estimation of future dynamics in very dynamic areas 6.4 Results and discussion 6.4.1 Past and future shoreline change rates 6.4.2 Cultural sites 6.4.3 Infrastructure and travel routes 6.5 Conclusions 7 Discussion 7.1 The importance of understanding climatic drivers of Coastal changes 7.2 The influence of shoreline change rates on retrogressive thaw slump activity 7.3 On the calculation of carbon fluxes from Coastal erosion along the Yukon coast 7.4 Impacts of present and future Coastal erosion on the natural and human environment 7.5 Synthesis 8 Summary and Conclusions Bibliography Supporting Material Data Set ds01 Table S1 Table S3 Abbreviations and Nomendature Acknowledgements
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    Call number: AWI G8-19-92587
    Description / Table of Contents: Arctic tundra ecosystems are experiencing warming twice the global average and Arctic vegetation is responding in complex and heterogeneous ways. Shifting productivity, growth, species composition, and phenology at local and regional scales have implications for ecosystem functioning as well as the global carbon and energy balance. Optical remote sensing is an effective tool for monitoring ecosystem functioning in this remote biome. However, limited field-based spectral characterization of the spatial and temporal heterogeneity limits the accuracy of quantitative optical remote sensing at landscape scales. To address this research gap and support current and future satellite missions, three central research questions were posed: • Does canopy-level spectral variability differ between dominant low Arctic vegetation communities and does this variability change between major phenological phases? • How does canopy-level vegetation colour images recorded with high and low spectral resolution devices relate to phenological changes in leaf-level photosynthetic pigment concentrations? • How does spatial aggregation of high spectral resolution data from the ground to satellite scale influence low Arctic tundra vegetation signatures and thereby what is the potential of upcoming hyperspectral spaceborne systems for low Arctic vegetation characterization? To answer these questions a unique and detailed database was assembled. Field-based canopy-level spectral reflectance measurements, nadir digital photographs, and photosynthetic pigment concentrations of dominant low Arctic vegetation communities were acquired at three major phenological phases representing early, peak and late season. Data were collected in 2015 and 2016 in the Toolik Lake Research Natural Area located in north central Alaska on the North Slope of the Brooks Range. In addition to field data an aerial AISA hyperspectral image was acquired in the late season of 2016. Simulations of broadband Sentinel-2 and hyperspectral Environmental and Mapping Analysis Program (EnMAP) satellite reflectance spectra from ground-based reflectance spectra as well as simulations of EnMAP imagery from aerial hyperspectral imagery were also obtained. Results showed that canopy-level spectral variability within and between vegetation communities differed by phenological phase. The late season was identified as the most discriminative for identifying many dominant vegetation communities using both ground-based and simulated hyperspectral reflectance spectra. This was due to an overall reduction in spectral variability and comparable or greater differences in spectral reflectance between vegetation communities in the visible near infrared spectrum. Red, green, and blue (RGB) indices extracted from nadir digital photographs and pigment-driven vegetation indices extracted from ground-based spectral measurements showed strong significant relationships. RGB indices also showed moderate relationships with chlorophyll and carotenoid pigment concentrations. The observed relationships with the broadband RGB channels of the digital camera indicate that vegetation colour strongly influences the response of pigment-driven spectral indices and digital cameras can track the seasonal development and degradation of photosynthetic pigments. Spatial aggregation of hyperspectral data from the ground to airborne, to simulated satel-lite scale was influenced by non-photosynthetic components as demonstrated by the distinct shift of the red edge to shorter wavelengths. Correspondence between spectral reflectance at the three scales was highest in the red spectrum and lowest in the near infra-red. By artificially mixing litter spectra at different proportions to ground-based spectra, correspondence with aerial and satellite spectra increased. Greater proportions of litter were required to achieve correspondence at the satellite scale. Overall this thesis found that integrating multiple temporal, spectral, and spatial data is necessary to monitor the complexity and heterogeneity of Arctic tundra ecosystems. The identification of spectrally similar vegetation communities can be optimized using non-peak season hyperspectral data leading to more detailed identification of vegetation communities. The results also highlight the power of vegetation colour to link ground-based and satellite data. Finally, a detailed characterization non-photosynthetic ecosystem components is crucial for accurate interpretation of vegetation signals at landscape scales.
    Type of Medium: Dissertations
    Pages: vi, 126 Seiten , Illustrationen
    Language: English
    Note: Dissertation, Universität Potsdam, 2019 , Table of Contents Abstract Zusammenfassung Abbreviations 1 Introduction 1.1 Scientific Background and Motivation 1.1.1 Arctic Tundra Vegetation 1.1.2 Remote Sensing of Arctic Tundra Vegetation 1.1.3 Hyperspectral Remote Sensing of Arctic Vegetation 1.2 Aims and Objectives 1.3 Study Area and Data 1.3.1 Toolik Lake Research Natural Area 1.3.2 In-situ Canopy-level Spectral Data 1.3.3 True-colour Digital Photographs 1.3.4 Leaf-level Photosynthetic Pigment Data 1.3.5 Airborne AISA Imagery 1.3.6 Simulated EnMAP and Sentinel-2 Reflectance Spectra 1.3.7 Simulated EnMAP Imagery 1.4 Thesis Structure and Author Contributions 1.4.1 Chapter 2 -A Phenological Approach to Spectral Differentiation of Low-Arctic Tundra Vegetation Communities, North Slope Alaska 1.4.2 Chapter 3 -Monitoring Pigment-driven Vegetation Changes in a Low Arctic Tundra Ecosystem Using Digital Cameras 1.4.3 Implications of Litter and Non-vascular Components on Multiscale Hyperspectral Data in a low-Arctic Ecosystem 2 A Phenological Approach to Spectral Differentiation of Low Arctic Tundra Vegetation Communities, North Slope Alaska 2.1 Abstract 2.2 Introduction 2.3 Materials and Methods 2.3.1 Study Site and Low Arctic Vegetation Types 2.3.2 Ground-Based Data and Sampling Protocol 2.3.3 EnMAP and Sentinel-2 Surface Reflectance Simulation 2.3.4 Stable Wavelength Identification Using the InStability Index 2.4 Results 2.4.1 Spectral Characteristics by Phenological Phase 2.4.2 InStability Index and Wavelength Selection of Ground-based Spectra 2.4.3 InStability Index and Wavelength Selection of Simulated Satellite Reflectance Spectra 2.5 Discussion 2.5.1 Phenological Phase and Wavelength Stability of Ground-based Spectra 2.5.2 Phenological Phase and Wavelength Stability of Satellite Resampled Spectra 2.5.3 Influence of Spatial Scale 2.6 Conclusions 2.7 Acknowledgements 2.8 Supplementary Material 2.8.1 Data Publication 3 Monitoring Pigment-driven Vegetation Changes in a Low Arctic Tundra Ecosystem Using Digital Cameras 3.1 Abstract 3.2 Introduction 3.3 Methods 3.3.1 Study Site 3.3.2 Digital Photographs 3.3.3 Field-based Spectral Data 3.3.4 Vegetation Pigment Concentration 3.3.5 Data Analyses 3.4 Results 3.4.1 RGB Indices as a Surrogate for Pigment-driven Spectral Indices 3.4.2 RGB Indices as a Surrogate for Leaf-level Pigment concentration 3.5 Discussion 3.6 Conclusions 3.7 Supplementary Material 3.7.1 Data Publication 4 Implications of Litter and Non-vascular Components on Multiscale Hyperspectral Data in a Low Arctic Ecosystem 4.1 Abstract 4.2 Introduction 4.3 Materials and Methods 4.3.1 Study Site 4.4 Remote Sensing Data 4.4.1 Ground-based Image Spectroscopy Data 4.4.2 Airborne AISA Hyperspectral Data 4.4.3 EnMAP Simulation 4.4.4 Spectral Comparison by Wavelength 4.4.5 Linear Mixture Analysis 4.5 Results 4.5.1 Spatial Scaling of Spectral Signals 4.6 Discussion 4.7 Conclusions 4.8 Acknowledgements 5 Synthesis and Discussion 5.1 Phenological Phase: does phenology influence the spectral variability of dominant low Arctic vegetation communities? 5.2 Vegetation Colour: How does canopy-level vegetation colour relate to phenological changes in leaf-level photosynthetic pigment concentration? 5.3 Intrinsic Ecosystem Components: How does spatial aggregation of high spectral resolution data influence low Arctic tundra vegetation signals? 5.4 Key Innovations 5.5 Limitations and Technical Considerations 5.6 Outlook: Opportunities for Future Research 6 References Acknowledgements
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    Monograph available for loan
    Monograph available for loan
    Berlin : Verlag für Geowissenschaften
    Call number: AWI E1-15-89214
    Description / Table of Contents: Alfred Wegener (1880-1930) war einer der bedeutendsten deutschen Naturwissenschaftler des vergangenen Jahrhunderts. Er untersuchte die Erdatmosphäre mit Drachen und Fesselballonen, erforschte das Wesen der gefürchteten Windhosen, fuhr vier Mal auf wissenschaftliche Expeditionen nach Grönland und stellte einen Weltrekord im bemannten Ballonflug auf. In diesem Buch wird das Leben dieses vielseitigen Forschers erzählt. Daneben wird sein wissenschaftliches Hauptwerk, die Kontinentaldrifttheorie, und seine Theorie zur Entstehung der Mondkrater durch Meteoritenbombardement beleuchtet, an die er Ideen über die Entstehung der Erde selbst knüpfte.
    Type of Medium: Monograph available for loan
    Pages: 208 S. , Ill., Kt.
    Edition: 1. Aufl.
    ISBN: 978-3-9814603-0-8 , 3981460308
    Language: German
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    Monograph available for loan
    Monograph available for loan
    Hamburg : maribus
    Associated volumes
    Call number: AWI G2-15-89284
    In: World ocean review
    Type of Medium: Monograph available for loan
    Pages: 151 S. , zahlr. Ill., graph. Darst., Kt.
    ISBN: 9783866482524
    Series Statement: World ocean review 4
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - Kapitel 1: Konzepte für eine bessere Welt. - Was ist Nachhaltigkeit?. - Der Wert der Natur. - Conclusio: „Nachhaltigkeit“ – ein schwer zu definierender Begriff. - Kapitel 2: Was das Meer zu leisten vermag. - Das Gute im Meer. - Der bedrohte Ozean. - Conclusio: Ökosystemleistungen des Meeres in Gefahr. - Kapitel 3: Die Politik und das Meer. - Von der Schwierigkeit, das Meer zu verwalten. - Conclusio: Das Ideal der guten Meerespolitik. - Kapitel 4: Hoffnung für den Ozean. - Fahrplan für eine nachhaltige Zukunft?. - Meeresschutz ist möglich. - Conclusio: Wie Meeresschutz funktionieren kann. - Gesamt-Conclusio. - Glossar. - Mitwirkende. - Quellenverzeichnis. - Abbildungsverzeichnis. - Index. - Abkürzungen. - Partner und Danksagung. - Impressum.
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    Monograph available for loan
    Monograph available for loan
    Hamburg : maribus
    Associated volumes
    Call number: AWI G2-15-89285
    In: World ocean review
    Type of Medium: Monograph available for loan
    Pages: 151 S. , zahlr. Ill, graph. Darst.
    ISBN: 9783866482531
    Series Statement: World ocean review 4
    Language: English
    Note: Contents: Preface. - Chapter 1: Concepts for a better world. - What is sustainability?. - The value of nature. - Conclusion: “Sustainability” – a difficult concept to define. - Chapter 2: How the sea serves us. - The bounty of the sea. - Oceans under threat. - Conclusion: Marine ecosystem services at risk. - Chapter 3: Politics and the oceans. - On the difficulty of governing the sea. - Conclusion: The ideal of good marine policy. - Chapter 4: Hope for the oceans. - Roadmap towards a sustainable future?. - Protecting the seas is possible. - Conclusion: How marine conservation can work. - Overall conclusion. - Glossary. - Contributors. - Bibliography. - Table of figures. - Index. - Abbreviations. - Partners and Acknowledgements. - Publication details.
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    Monograph available for loan
    Monograph available for loan
    Berlin : Matthes & Seitz
    Call number: AWI E1-15-89047
    Description / Table of Contents: Georg Forster (1754-1794) war eine der faszinierendsten Gestalten seiner Zeit: glänzender Schriftsteller, Naturforscher, Entdecker, Zeichner, Übersetzer und entschiedener Revolutionär. Auf seiner Weltumsegelung mit James Cook berührte er Eisberge mit den eigenen Händen, lief den Strand von Tahiti entlang, besuchte fremde Völker, lebte unter »Menschenfressern« und überquerte Ozeane und den Äquator. Und er stand im Zentrum des politischen Geschehens, als er - inspiriert von der Französischen Revolution - 1793 die »Mainzer Republik« ausrief, die erste Republik auf deutschem Boden. Anschaulich und fesselnd portraitiert Jürgen Goldstein dieses Ausnahmeleben, in dem sich »Freiheit« und »Naturgewalt« berührten. Niemand ist auf vergleichbare Weise das erfahrungsgetriebene Experiment eingegangen, die Natur mit dem Politischen kurzzuschließen. Die Funken, die Forster aus seinen Leitvorstellungen schlug, erhellten für einen Weltaugenblick die Aussicht, es könne so etwas wie natürliche Revolutionen geben. Jürgen Goldstein, geboren 1962, lehrt als Professor für Philosophie an der Universität Koblenz-Landau. Maßgeblich von Hans Blumenberg inspiriert, widmen sich seine Studien der Genese und dem Profil der Moderne. Seine Bücher befassen sich mit der Herausbildung der neuzeitlichen Subjektivität und Rationalität, der politischen Philosophie des 20. Jahrhunderts und der Geschichte der Naturwahrnehmung.
    Description / Table of Contents: Wagemutiger Entdeckungsreisender, empfindsamer Naturbetrachter, glühender Revolutionär: Georg Forster befuhr mit James Cook die Weltmeere, verfasste glänzende Reiseerzählungen und stürzte sich mit provokanten Ansichten in die politischen Debatten seiner Zeit. Er war in Mainz Mitbegründer der ersten Republik auf deutschem Boden und starb - gescheitert und vereinsamt - im Pariser Exil. In seiner ebenso fesselnden wie kenntnisreichen Biographie entwirft Jürgen Goldstein mit Eleganz und Tiefenschärfe ein anschauliches Panorama von Forsters rastlosem Leben zwischen Euphorie und Elend - das Leben eines Weltbürgers, der davon überzeugt war, dass sich die Freiheit eines Tages mit Naturgewalt ihren Wag bahnen müsse.
    Type of Medium: Monograph available for loan
    Pages: 301 S. , 22 cm
    Edition: 1. Aufl.
    ISBN: 978-3-95757-090-1
    Language: English
    Note: Inhalt: Auftakt. - Ein gefährliches Wort: Natur. - 1. 1754-1772. ANFÄNGE. - Wie ein unbeschriebenes Blatt. - Erste Eindrücke von Weite. - Zur rechten Zeit am rechten Ort. - 2. 1772-1775. ANSICHTEN DER NATUR: DIE REISE UM DIE WELT. - Wahrnehmungsmuster. - Die große Erzählung. - Das Meer. - Entfernungen. - Strapazen. - Wagnisse im Eis. - Das sonnige Arkadien. - Erste und letzte Anblicke. - Edle Wilde?. - Unter Menschenfressern. - Mord und Totschlag. - Eine Gemeinschaft von Gleichen. - Die gekränkten Rechte der Menschheit. - 3. 1776-1788. ZWISCHENSPIELE. - Blue devils. - Der Balsam der Natur. - Eine physische Anthropologie. - Ein Streit um Menschenrassen. - Politisches Wetterleuchten: Cook, der Staatsmann. - 4. 1789-1793. ANSICHTEN DES POLITISCHEN: DIE REVOLUTION. - Pariser Unruhen und politische Öffentlichkeit. - Geschichtszeichen der neuen Welt: Revolutionen. - Politische Ansichten vom Niederrhein. - Natur als Schicksal. - Das Prinzip des politischen Wandels: Gärung. - Die französische Mainzer Freiheit. - Die Mainzer Republik. - Kundige der unterirdischen Gänge: Forster und Goethe. - 5. 1793-1794. DAS ENDE: DIE GROßE RATLOSIGKEIT. - Das ungeheure Haupt der Revolution: Paris. - Das kalte Fieber des Terrors. - Tänzer am Rande des Unsinns: Adam Lux. - Zurück zur Natur: Menschenwürde. - Die Revolution ist die Revolution. - Verlassen wie ein Kind. - Eine Quelle sonderbarer Beschauung. - Schluss. - Das Mahagoni-Schränkchen. - Anmerkungen. - Literatur.
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    Call number: AWI S5-16-89899
    Type of Medium: Monograph available for loan
    Pages: XXVIII, 2336 Seiten
    Edition: 7. Auflage
    ISBN: 9783452285713 (Gb.)
    Series Statement: Heymanns Taschenkommentare
    Language: German
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    Call number: PIK N 456-17-91009 ; AWI A5-18-91009
    In: Geophysical monograph, 226
    Type of Medium: Monograph available for loan
    Pages: XIII, 386 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 1119067847 , 9781119067849
    Series Statement: Geophysical Monograph Series ; 226
    Language: English
    Note: Contents: TITLE PAGE -- COPYRIGHT PAGE -- CONTENTS -- CONTRIBUTORS -- PREFACE -- ACKNOWLEDGMENTS -- PART I FORCINGS OF CLIMATE EXTREMES -- CHAPTER 1 THE CHANGING EL NIÑO-SOUTHERN OSCILLATION AND ASSOCIATED CLIMATE EXTREMES -- 1.1. INTRODUCTION -- 1.2. CHANGES IN ENSO PROPERTIES -- 1.3. CHANGES IN ENSO DYNAMICS -- 1.4. CHANGES IN ENSO TELECONNECTIONS AND ASSOCIATED CLIMATE EXTREMES -- 1.5. ENSO IN THE FUTURE -- 1.6. SUMMARY -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 2 WEATHER EXTREMES LINKED TO INTERACTION OF THE ARCTIC AND MIDLATITUDES -- 2.1. INTRODUCTION -- 2.2. ARCTIC EFFECTS ON MIDLATITUDE EXTREMES -- 2.3. MIDLATITUDE EFFECTS ON ARCTIC EXTREMES -- 2.4. DISCUSSION AND CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 3 IMPACT OF AEROSOLS ON REGIONAL CHANGES IN CLIMATE EXTREMES -- 3.1. INTRODUCTION -- 3.2. DIRECT AND INDIRECT EFFECTS OF AEROSOLS ON CLOUDS AND RADIATION -- 3.3. AEROSOL IMPACT ON REGIONAL CLIMATE CHANGE -- 3.4. Mitigation scenarios for aerosol emissions -- 3.5. AEROSOL EFFECT ON TEMPERATURE AND PRECIPITATION EXTREMES -- 3.6. FUTURE RESEARCH NEEDS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 4 WEAKENED FLOW, PERSISTENT CIRCULATION, AND PROLONGED WEATHER EXTREMES IN BOREAL SUMMER -- 4.1. INTRODUCTION -- 4.2. RESONANT CIRCULATION REGIMES -- 4.3. REAL EVENTS -- 4.4. CONCLUSIONS AND DISCUSSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 5 LAND PROCESSES AS THE FORCING OF EXTREMES: A REVIEW -- 5.1. INTRODUCTION -- 5.2. FORCINGS OF LAND PROCESSES ON CLIMATE EXTREMES -- 5.3. SUMMARY -- ACKNOWLEDGMENTS -- REFERENCES -- PART II PROCESSES OF CLIMATE EXTREMES -- CHAPTER 6 TIMING OF ANTHROPOGENIC EMERGENCE IN CLIMATE EXTREMES -- 6.1. INTRODUCTION -- 6.2. DEFINING TIME OF EMERGENCE -- 6.3. DATA AND METHODS -- 6.4. RESULTS -- 6.5. DISCUSSION -- 6.6. CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES CHAPTER 7 RECENT INCREASES IN EXTREME TEMPERATURE OCCURRENCE OVER LAND -- 7.1. INTRODUCTION -- 7.2. DATA AND METHODOLOGY -- 7.3. RESULTS -- 7.4. CONCLUSIONS -- REFERENCES -- CHAPTER 8 WHY FUTURE SHIFTS IN TROPICAL PRECIPITATION WILL LIKELY BE SMALL: THE LOCATION OF THE TROPICAL RAIN BELT AND THE HEMISPHERIC CONTRAST OF ENERGY INPUT TO THE ATMOSPHERE -- 8.1. INTRODUCTION -- 8.2. THE RELATIONSHIP BETWEEN ITCZ POSITION AND HEMISPHERIC CONTRAST OF ATMOSPHERIC HEATING -- 8.3. RELATIONSHIP BETWEEN THE SEASONAL CYCLE OF ITCZ MIGRATION AND THE ANNUAL MEAN PRECIPITATION DISTRIBUTION -- 8.4. IMPLICATIONS FOR FUTURE ITCZ SHIFTS UNDER GLOBAL WARMING -- REFERENCES -- CHAPTER 9 WEATHER-CLIMATE INTERACTIONS AND MJO INFLUENCES -- 9.1. INTRODUCTION -- 9.2. THE INTERACTIONS BETWEEN THE MJO, BACKGROUND STATE, AND SYNOPTIC WEATHER -- 9.3. A CASE STUDY ON INTERACTIONS BETWEEN THE MADDEN-JULIAN OSCILLATION AND EL NIÑO -- 9.4. INTERACTIONS BETWEEN THE MJO AND BREAKING WAVES -- 9.5. INTERACTIONS BETWEEN THE MJO, TROPICAL CYCLONES, AND THE EXTRATROPICAL CIRCULATION -- 9.6. SUMMARY -- REFERENCES -- CHAPTER 10 RECENT CLIMATE EXTREMES ASSOCIATED WITH THE WEST PACIFIC WARMING MODE -- 10.1. INTRODUCTION -- 10.2. BACKGROUND -- 10.3. DATA AND METHODS -- 10.4. SUMMARY AND DISCUSSION -- REFERENCES -- CHAPTER 11 CONNECTIONS BETWEEN HEAT WAVES AND CIRCUMGLOBAL TELECONNECTION PATTERNS IN THE NORTHERN HEMISPHERE SUMMER -- 11.1. INTRODUCTION -- 11.2. DATA AND METHODS -- 11.3. DISTRIBUTION OF HEAT WAVES -- 11.4. PLANETARY WAVES ASSOCIATED WITH THE HEAT WAVES -- 11.5. SUMMARY AND DISCUSSION -- ACKNOWLEDGMENTS -- REFERENCES -- PART III REGIONAL CLIMATE EXTREMES -- CHAPTER 12 NORTH AMERICAN DROUGHT AND LINKS TO NORTHERN EURASIA: THE ROLE OF STATIONARY ROSSBY WAVES -- 12.1. INTRODUCTION -- 12.2. REANALYSIS DATA AND THE GEOS-5 AGCM EXPERIMENTS -- 12.3. RESULTS -- 12.4. SUMMARY AND CONCLUSIONS ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 13 THE CALIFORNIA DROUGHT: TRENDS AND IMPACTS -- 13.1. INTRODUCTION -- 13.2. THE PROLONGED DROUGHT OF 2012-2016 -- 13.3. ROLE OF ENSO CYCLE -- 13.4. ARCTIC INFLUENCES -- 13.5. DROUGHT IMPACTS ON CALIFORNIA -- 13.6. CONCLUDING REMARKS -- REFERENCES -- CHAPTER 14 OBSERVED TRENDS IN US TORNADO FREQUENCY -- 14.1. INTRODUCTION -- 14.2. STORM DATA TORNADO DATABASE -- 14.3. US TORNADO CLIMATOLOGY -- 14.4. CHANGES IN US TORNADO STATISTICS -- 14.5. CONCLUDING REMARKS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 15 MECHANISMS EXPLAINING RECENT CHANGES IN AUSTRALIAN CLIMATE EXTREMES -- 15.1. INTRODUCTION -- 15.2. AUSTRALIAN RAINFALL EXTREMES OF 2010-2012 -- 15.3. AUSTRALIA'S TEMPERATURE EXTREMES OF 2013 -- 15.4. SUMMARY AND CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 16 UNRAVELING EAST AFRICA'S CLIMATE PARADOX -- 16.1. INTRODUCTION -- 16.2. THE NATURE OF THE RECENT EAST AFRICAN LONG RAINS DECLINE -- 16.3. LINKS TO PACIFIC DECADAL VARIABILITY -- 16.4. PHYSICAL CONSIDERATIONS -- 16.5. CLIMATE MODEL SIMULATIONS OF EAST AFRICAN CLIMATE -- 16.6. CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 17 A PHYSICAL MODEL FOR EXTREME DROUGHT OVER SOUTHWEST ASIA -- 17.1. INTRODUCTION -- 17.2. PRECIPITATION PATTERNS -- 17.3. SST RELATIONSHIPS -- 17.4. ATMOSPHERIC TELECONNECTIONS -- 17.5. SUMMARY -- APPENDIX: DATA -- REFERENCES -- PART IV PREDICTION OF CLIMATE EXTREMES -- CHAPTER 18 EXTRATROPICAL PRECURSORS OF THE EL NIÑO-SOUTHERN OSCILLATION -- 18.1. INTRODUCTION -- 18.2. OVERVIEW OF PRECURSORS AND THEIR IMPACT ON ENSO -- 18.3. DATA AND DEFINITIONS -- 18.4. EVALUATION OF PRECURSOR VARIABILITY AND COVARIABILITY -- 18.5. RELATIONSHIP BETWEEN PRECURSORS AND ENSO -- 18.6. DIAGNOSING PRECURSORS AS ENSO PREDICTORS -- 18.7. RELATIONSHIP OF EXTRATROPICAL PRECURSORS TO 2014 AND 2015 EL NIñO -- 18.8. SUMMARY AND DISCUSSION -- REFERENCES -- CHAPTER 19 NORTH ATLANTIC SEASONAL HURRICANE PREDICTION: UNDERLYING SCIENCE AND AN EVALUATION OF STATISTICAL MODELS -- 19.1. INTRODUCTION -- 19.2. STATISTICALLY BASED SEASONAL HURRICANE OUTLOOK MODELS -- 19.3. CONCLUSIONS -- REFERENCES -- CHAPTER 20 PREDICTING SUBSEASONAL PRECIPITATION VARIATIONS BASED ON THE MADDEN-JULIAN OSCILLATION -- 20.1. INTRODUCTION -- 20.2. THE MJO INFLUENCE ON THE VARIABILITY OF PRECIPITATION -- 20.3. FORECASTING THE MJO -- 20.4. THE MJO AND PREDICTABILITY OF PRECIPITATION -- 20.5. CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- CHAPTER 21 PREDICTION OF SHORT-TERM CLIMATE EXTREMES WITH A MULTIMODEL ENSEMBLE -- 21.1. INTRODUCTION -- 21.2. PREDICTION SKILL -- 21.3. PREDICTABILITY -- 21.4. SUMMARY AND DISCUSSION -- REFERENCES -- CHAPTER 22 TOWARD PREDICTING US TORNADOES IN THE LATE 21ST CENTURY -- 22.1. PROJECTING CHANGES IN US TORNADO ACTIVITY USING ENVIRONMENTAL PROXIES -- 22.2. SHORT-TERM TORNADO PREDICTION USING HIGH RESOLUTION MODELS AND APPLICATIONS TO DYNAMICAL DOWNSCALING -- 22.3. CONCLUDING REMARKS -- ACKNOWLEDGMENTS -- REFERENCES -- INDEX
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    Call number: AWI A11-16-90009
    In: Forschungsbericht / Deutsches Zentrum für Luft- und Raumfahrt ; 2016-01, 2016-01
    Description / Table of Contents: Recent climate model simulations indicated that sulfate (SO4) formed from ship emissions may be one of the major contributors to the negative anthropogenic aerosol radiative forcing. Due to increasingly stringent regulations on the maximum sulfur content of ship fuels this contribution is expected to decrease strongly in the future. Possibly, nitrate (NO3) formation will compensate for part of the reduction, but measurements indicate that it may be crucial to include coarse mode particle interactions with condensable trace gases in order to quantify this effect. However, none of the aerosol (sub)models previously used for such assessments accounted for the coarse mode particle effects. This provided the motivation to extend one of those submodels, namely MADE, in the present work. The new submodel, MADE3, is based on the second generation of MADE, called MADE-in. It includes nine lognormal modes to represent three size ranges with three types of aerosol particles each. The associated increase in complexity w.r.t. to MADE and MADE-in required a complete revision of the code and careful reexamination of the underlying physical assumptions, as only the fine modes had been considered in the gas–particle interactions in the predecessor submodels. The main new features of MADE3 are the ability of coarse mode particles to take up condensing vapors and to coagulate with fine mode particles, and the gas–particle partitioning of chlorine, which is mainly contained in sea spray (SS) particles. In order to test the algorithms used in the new submodel it was run in a box model setup and the results were compared to those obtained in an analogous setup with the much more detailed, particle-resolved aerosol model PartMC-MOSAIC. The comparison was performed for an idealized marine boundary layer test case and showed improved performance of MADE3 over MADE in the representation of coarse mode particles and total aerosol composition. Subsequently, MADE3 was implemented into the atmospheric chemistry general circulation model EMAC. Due to the new mode structure this required extensive adaptations to other submodels, specifically to the one used for cloud and precipitation processing of aerosol particles. EMAC does not track interstitial aerosol particles separately from those immersed in cloud droplets, ice crystals, or precipitation. Hence, a sophisticated scheme was devised and implemented for the assignment of the in-cloud or in-precipitation aerosol to one of four possible modes, instead of just one possible mode in the MADE case. The coupled model, EMAC with MADE3, was thoroughly evaluated by comparison of simulation output to station network measurements of near-surface aerosol component mass concentrations, to airborne measurements of vertical aerosol mass mixing ratio and number concentration profiles, to ground-based and airborne measurements of particle size distributions, and to station network and satellite measurements of aerosol optical depth. Satisfactory agreement with the observations was obtained and it was thus shown that MADE3 is ready for application within EMAC. The results from an identically designed simulation with the predecessor submodel MADE led to the conclusion that a fraction of the secondary aerosol species partitions to the coarse modes in MADE3 and is thus removed more quickly from the atmosphere. Furthermore, a new evaluation method was developed, which allows for comparison of model output to size-resolved electron microscopy measurements of particle composition. Both submodels, MADE3 and MADE, were finally used in EMAC simulations of the effect of ship emissions on the atmospheric aerosol. As in previous studies for year 2000 conditions, SO4 was found to be the dominant species in the fine modes in this context. In contrast to SO4, the major fraction of ship emissions-induced near-surface NO3 was found to partition to the coarse modes in the MADE3 simulations. A similar amount of fine mode NO3 as in the present and former MADE simulations was also formed. Hence, fine mode particle growth due to ship emissions was also similar, and was reduced in idealized simulations of a future low-sulfur fuel scenario. Particle volume concentration decreased by about 1 % due to ship emissions in the MADE3 simulations, but not in the MADE simulations. This finding was independent of the fuel sulfur content. In summary, the inclusion of coarse mode particle interactions and the gas–particle partitioning of chlorine could alter prior conclusions on the climate effect of ship emissions-induced aerosol perturbations, mainly due to the differences in NO3 formation. This climate effect will be re-quantified in a follow-up study by coupling the MADE3 aerosol to a two-moment cloud microphysics scheme. Further planned applications of the new submodel include the quantification of climate effects of aerosol perturbations via their influence on ice clouds as well as simulations with boundary conditions specific to measurement campaigns. Results from the latter may lead to further model improvements and can also provide guidance for the interpretation of measurement results.
    Type of Medium: Dissertations
    Pages: xiv, 170 Seiten , 42 Illustrationen und Diagramme
    Edition: Als Manuskript gedruckt
    Series Statement: Forschungsbericht / DLR, Deutsches Zentrum für Luft- und Raumfahrt 2016-01
    Language: English
    Note: Contents: Abstract. - Kurzfassung. - 1 Introduction. - 1.1 Motivation. - 1.2 Scientific questions. - 1.3 Method. - 2 Background and state of the science. - 2.1 The atmospheric aerosol. - 2.1.1 Relevance. - 2.1.2 Aerosol processes. - 2.1.3 Aerosol properties. - 2.2 The influence of ship emissions. - 2.3 Aerosol modeling. - 2.3.1 Selected results. - 2.3.2 Motivation to expand on previous work. - 2.3.3 The computational approach. - 2.3.4 Existing aerosol microphysics submodels. - 2.3.5 MADE3 as a successor of MADE and MADE-in. - 3 The aerosol submodel MADE3. - 3.1 Aerosol characteristics. - 3.1.1 Modes. - 3.1.2 Species. - 3.1.3 Mathematical representation of aerosol characteristics. - 3.2 Aerosol processes. - 3.2.1 Gas–particle partitioning. - 3.2.2 Condensation of H2SO4 and organic vapors. - 3.2.3 New particle formation. - 3.2.4 Coagulation. - 3.2.5 Renaming. - 3.2.6 Aging of insoluble particles. - 4 Box model tests. - 4.1 Model description: MADE vs. MADE3. - 4.2 Model description: PartMC-MOSAIC. - 4.3 Test case scenario. - 4.4 Results: MADE3 vs. MADE. - 4.4.1 Size distributions. - 4.4.2 Composition. - 4.5 Results: MADE3 vs. PartMC-MOSAIC. - 4.5.1 Size distributions. - 4.5.2 Composition. - 4.6 Summary and conclusions. - 5 MADE3 in the atmospheric chemistry general circulation model EMAC. - 5.1 Basic settings. - 5.2 Emissions. - 5.3 Transport. - 5.4 Gas phase chemistry. - 5.5 Cloud formation. - 5.5.1 Stratiform clouds. - 5.5.2 Convective clouds. - 5.6 Cloud and precipitation processing of the aerosol. - 5.7 Wet deposition. - 5.8 Dry deposition. - 5.9 Sedimentation. - 5.10 Optical properties. - 6 Evaluation of simulated tropospheric aerosol properties. - 6.1 Data comparability. - 6.2 The MADE3 aerosol within EMAC. - 6.2.1 Near-surface mass concentrations. - 6.2.2 Vertical distributions. - 6.2.3 Size distributions. - 6.2.4 Aerosol optical depth. - 6.2.5 Global tropospheric burdens and residence times. - 6.2.6 Summary and conclusions. - 6.3 Comparison to MADE. - 6.4 New features of MADE3. - 7 Effects of oceanic ship emissions on atmospheric aerosol particles. - 7.1 Effects of year 2000 emissions. - 7.1.1 Near-surface concentrations. - 7.1.2 Near-surface size distributions. - 7.1.3 Tropospheric burdens. - 7.2 Effects of an idealized fuel sulfur content reduction. - 7.3 Summary and conclusions. - 8 Summary, conclusions, and outlook. - Appendix. - A.1 Particle evolution in the box model study. - A.2 Gas phase chemical mechanism. - A.3 Liquid phase chemical mechanism. - A.4 Mode assignment of cloud residual aerosol. - A.4.1 Terminology. - A.4.2 Basic assumptions. - A.4.3 Algorithm for residual assignment. - A.5 Year 2000 aerosol in EMAC with MADE3. - A.6 Near-surface mass concentration evaluation. - References. - Acronyms, symbols, and species names. - Acronyms. - Symbols. - Tracers and chemical species. - Danksagung.
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  • 32
    Monograph available for loan
    Cambridge, United Kingdom : Cambridge University Press
    Call number: AWI A2-17-90931
    Description / Table of Contents: Climate change is one of the greatest threats facing humanity; a definitive manifestation of the well-worn links between progress and devastation. This book explores the complex relationship that the corporate world has with climate change, and examines the central role of corporations in shaping political and social responses to the climate crisis. The book's principal message is that despite the need for dramatic economic and political change, corporate capitalism continues to rely upon the maintenance of 'business as usual'. The authors explore the different processes through which corporations engage with climate change. Key discussion points include climate change as business risk; corporate climate politics; the role of justification and compromise; and managerial identity and emotional reactions to climate change. Written for researchers and graduate students, this book moves beyond descriptive and normative approaches to provide a sociologically and critically informed theory of corporate responses to climate change.
    Type of Medium: Monograph available for loan
    Pages: XIII, 254 Seiten , Diagramm , 23 cm
    Edition: 1st published 2015, Reprinted 2016
    ISBN: 9781107435131 (paperback) , 9781107078222 (hardback)
    URL: Cover
    Language: English
    Note: Contents: List of figures. - List of tables. - Foreword by Clive Hamilton. - Acknowledgements. - 1. Climate change and corporate capitalism. - 2. Creative self-destruction and the incorporation of critique. - 3. Climate change and the corporate construction of risk. - 4. Corporate political activity and climate coalitions. - 5. Justification, compromise, and corruption. - 6. Climate change, managerial identity and narrating the self. - 7. Emotions, corporate environmentalism and climate change. - 8. Political myths and pathways forward. - 9. Imagining alternatives. - Appendix. - References. - Index.
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  • 33
    Call number: AWI G1-17-90601
    Description / Table of Contents: This innovative study presents concepts and problems in soil physics, and provides solutions using original computer programs. It provides a close examination of physical environments of soil, including an analysis of the movement of heat, water and gases. The authors employ the programming language Python, which is now widely used for numerical problem solving in the sciences. In contrast to the majority of the literature on soil physics, this text focuses on solving, not deriving, differential equations for transport. Using numerical procedures to solve differential equations allows the solution of quite difficult problems with fairly simple mathematical tools. Numerical methods convert differential into algebraic equations, which can be solved using conventional methods of linear algebra. Each chapter introduces a soil physics concept, and proceeds to develop computer programs to solve the equations and illustrate the points made in the discussion. Problems at the end of each chapter help the reader practise using the concepts introduced. The text is suitable for advanced undergraduates, graduates and researchers of soil physics. It employs an open source philosophy where computer code is presented, explained and discussed, and provides the reader with a full understanding of the solutions. Once mastered, the code can be adapted and expanded for the user's own models, fostering further developments. The Python tools provide a simple syntax, Object Oriented Programming techniques, powerful mathematical and numerical tools, and a user friendly environment.
    Type of Medium: Monograph available for loan
    Pages: X, 449 Seiten , Illustrationen
    Edition: First edition
    ISBN: 0199683093 , 9780199683093
    Language: English
    Note: Contents: 1 Introduction. - 2 Basic Physical Properties of Soil. - 2.1 Geometry of the Soil Matrix. - 2.2 Soil Structure. - 2.3 Fractal Geometry. - 2.4 Geometry of the Pore Space. - 2.5 Specific Surface Area. - 2.6 Averaging. - 2.7 Bulk Density, Water Content and Porosity. - 2.8 Relationships between Variables. - 2.9 Typical Values of Physical Properties. - 2.10 Volumes and Volumetric Fractions for a Soil Prism. - 2.11 Soil Solid Phase. - 2.12 Soil Texture. - 2.13 Sedimentation Law. - 2.14 Exercises. - 3 Soil Gas Phase and Gas Diffusion. - 3.1 Transport Equations. - 3.2 The Diffiisivity of Gases in Soil. - 3.3 Computing Gas Concentrations. - 3.4 Simulating One-Dimensional Steady-State Oxygen Diffusion in a Soil Profile. - 3.5 Numerical Implementation. - 3.6 Exercises. - 4 Soil Temperature and Heat Flow. - 4.1 Differential Equations for Heat Conduction. - 4.2 Soil Temperature Data. - 4.3 Numerical Solution of the Heat Flow Equation. - 4.4 Soil Thermal Properties. - 4.5 Numerical Implementation. - 4.6 Exercises. - 5 Soil Liquid Phase and Soil-Water Interactions. - 5.1 Properties of Water. - 5.2 Soil Water Potential. - 5.3 Water Potential-Water Content Relations. - 5.4 Liquid- and Vapour-Phase Equilibrium. - 5.5 Exercises. - 6 Steady-State Water Flow and Hydraulic Conductivity. - 6.1 Forces on Water in Porous Media. - 6.2 Water Flow in Saturated Soils. - 6.3 Saturated Hydraulic Conductivity. - 6.4 Unsaturated Hydraulic Conductivity. - 6.5 Exercises. - 7 Variation in Soil Properties. - 7.1 Frequency Distributions. - 7.2 Probability Density Functions. - 7.3 Transformations. - 7.4 Spatial Correlation. - 7.5 Approaches to Stochastic Modelling. - 7.6 Numerical Implementation. - 7.7 Exercises. - 8 Transient Water Flow. - 8.1 Mass Conservation Equation. - 8.2 Water Flow. - 8.3 Infiltration. - 8.4 Numerical Simulation of Infiltration. - 8.5 Numerical Implementation. - 8.6 Exercises. - 9 Triangulated Irregular Network. - 9.1 Digital Terrain Model. - 9.2 Triangulated Irregular Network. - 9.3 Numerical Implementation. - 9.4 Main. - 9.5 Triangulation. - 9.6 GIS Functions. - 9.7 Boundary. - 9.8 Geometrical Properties of Triangles. - 9.9 Delaunay Triangulation. - 9.10 Refinement. - 9.11 Utilities. - 9.12 Visualization. - 9.13 Exercise. - 10 Water Flow in Three Dimensions. - 10.1 Governing Equations. - 10.2 Numerical Formulation. - 10.3 Coupling Surface and Subsurface Flow. - 10.4 Numerical Implementation. - 10.5 Simulation. - 10.6 Visualization and Results. - 10.7 Exercises. - 11 Evaporation. - 11.1 General Concepts. - 11.2 Simultaneous Transport of Liquid and Vapour in Isothermal Soil. - 11.3 Modelling evaporation. - 11.4 Numerical Implementation. - 11.5 Exercises. - 12 Modelling Coupled Transport. - 12.1 Transport Equations. - 12.2 Partial Differential Equations. - 12.3 Surface Boundary Conditions. - 12.4 Numerical Implementation. - 12.5 Exercises. - 13 Solute Transport in Soils. - 13.1 Mass Flow. - 13.2 Diffusion. - 13.3 Hydrodynamic Dispersion. - 13.4 Advection-Dispersion Equation. - 13.5 Solute-Soil Interaction. - 13.6 Sources and Sinks of Solutes. - 13.7 Analytical Solutions. - 13.8 Numerical Solution. - 13.9 Numerical Implementation. - 13.10 Exercises. - 14 Transpiration and Plant-Water Relations. - 14.1 Soil Water Content and Soil Water Potential under a Vegetated Surface. - 14.2 General Features of Water Flow in the SPAC. - 14.3 Resistances to Water Flow within the Plant. - 14.4 Effect of Environment on Plant Resistance. - 14.5 Detailed Consideration of Soil and Root Resistances. - 14.6 Numerical Implementation. - 14.7 Exercises. - 15 Atmospheric Boundary Conditions. - 15.1 Radiation Balance at the Exchange Surface. - 15.2 Boundary-Layer Conductance for Heat and Water Vapour. - 15.3 Evapotranspiration and the Penman-Monteith Equation. - 15.4 Partitioning of Evapotranspiration. - 15.5 Exercise. - Appendix A: Basic Concepts and Examples of Python Programming. - A.1 Basic Python. - A.2 Basic Concepts of Computer Programming. - A.3 Data Representation: Variables. - A.4 Comments Rules and Indendation. - A.5 Arithmetic Expression. - A.6 Functions. - A.7 Flow Control. - A.8 File Input and Output. - A.9 Arrays. - A.10 Reading Date Time. - A.11 Object-Oriented Programming in Python. - A.12 Output and Visualization. - A.13 Exercises. - Appendix B: Computational Tools. - B.1 Numerical Differentiation. - B.2 Numerical Integration. - B.3 Linear Algebra. - B.4 Exercises. - List of Symbols. - List of Python Variables. - List of Python Projects. - References. - Index.
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  • 34
    Monograph available for loan
    Monograph available for loan
    Potsdam : Bibliothek Wissenschaftspark Albert Einstein
    Call number: AWI G3-18-91414 ; M 18.91414
    Description / Table of Contents: This project started in October 2015 with a crazy idea : prepare and submit a funding application for an international, multidisciplinary and non-traditional scientific outreach project… within the next 48 hours. Well, it worked out. A group of highly motivated young researchers from Canada and Europe united to combine arts and science and produce a series of outreach comic strips about permafrost (frozen ground). The aim of the project is to present and explain scientific research conducted across the circumpolar Arctic, placing emphasis on field work and the rapidly changing northern environment. The target audience is kids, youth, parents and teachers, with the general goal of making permafrost science more fun and accessible to the public. Because guess what : permafrost represents an area of more than twenty million km2 in the Northern Hemisphere, a huge area. As the climate warms, permafrost thaws and becomes unstable for houses, roads and airports. This rapid thawing of previously frozen ground also disrupts plant and animal habitats, impacts water quality and the ecology of lakes, and releases carbon into the atmosphere as greenhouse gases, making climate change even stronger. Hence permafrost and its response to climate change concerns us all. The project received initial support from the International Permafrost Association (IPA) as a targeted ‘Action Group’, and since then several other sponsors have joined the project. Here we are, now, two years after this first idea. What you are about to read is the result of an iterative process of exchanging ideas between artists and scientists. We first made an application call and received 49 applications from artists in 16 countries. Through a formal review process, we then selected two artists to work on this project: Noémie Ross from Canada, and Heta Nääs from Finland. With input from scientists, Noémie and Heta created fantastic cartoons that explain some of the changes happening to the environment in permafrost areas, how they affect people and wildlife, and what scientists are doing to better understand these changes to help people find innovative ways to adapt. We wish everyone plenty of fun reading this booklet and we would like to thank all those who supported this project.
    Type of Medium: Monograph available for loan
    Pages: 27 Seiten , Illustrationen
    ISBN: 978-2-9816972-0-2
    Language: English
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  • 35
    Call number: ZSP-760/A-16
    In: Terra Antartica reports, No. 16
    Type of Medium: Series available for loan
    Pages: 15 Seiten , Illustrationen , 4 Kartenbeilagen, 1 Erläuterungsheft (4 S.)
    ISBN: 978-88-88395-13-5
    Series Statement: Terra Antartica reports 16
    Language: English
    Note: 1 Kartenbeilage unter dem Titel: Northern Foothills and Inexpressible Island Area (Victoria Land, Antarctica) : Satellite Image Map = Northern Foothills E Area Di Inexpressible Island (Terra Vittoria, Antartide) / Flavio Borfecchia & Massimo Frezzotti 〈1 : 50.000〉 , 1 Kartenbeilage unter dem Titel: Satellite Image Mosaic of the Terra Nova Bay Area (Victoria Land, Antarctica) = Mosaico Di Immagini Da Satellite Dell'Area Di Baia Terra Nova (Terra Vittoria, Antartide) / Massimo Frezzotti, Maria Christina Salvatore & Luca Vittuari 〈1 : 250.000〉 , 1 Kartenbeilage unter dem Titel: Mount Melbourne Quadrangle (Victoria Land) = Foglio Mount Melbourne (Terra Vittoria) / Editor Carlo Baroni 〈1 : 250.000〉 aus der Antarctic Geomorphological and Glaciological 1:250.000 Map Series , 1 Kartenbeilage unter dem Titel: Mount Melbourne Quadrangle (Victoria Land) 2012 / P. C. Pertusati, G. Musumeci, R. Carosi, M. Meccheri 〈1 : 250.000〉 aus der Antarctic Geological 1:250.000 Map Series , This case with the aim to celebrate 30 years of Italian research in Antarctica, contains four geothematic maps of the Terra Nova bay area where the Italian Programma Nazionale di Ricerche in Antartide begun its activities in 1985 and the Italian coastal station Mario Zucchelli was constructed.
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  • 36
    Monograph available for loan
    Monograph available for loan
    Bonn : Bundesministerium für Bildung und Forschung (BMBF), Referat System Erde
    Call number: AWI P1-18-91711
    Type of Medium: Monograph available for loan
    Pages: 38 Seiten , Illustrationen
    Edition: Stand: Mai 2016 (unveränderter Nachdruck Januar 2017)
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - 1. Einführung. - 2. Herausforderungen an die Küsten-, Meeres- und Polarforschung. - 3. Politischer und programmatischer Rahmen. - 4. Internationale Einbindung der Küsten-, Meeres- und Polarforschung. - 5. Agendaprozesse in der Küsten-, Meeres- und Polarforschung. - 6. Programmstruktur. - 7. Wissenschaftliches Programm. - 7.1 Globaler Wandel und Klima geschehen. - 7.2 Ökosystemfunktion und Biodiversität. - 7.3 Globale Stoffkreisläufe und Energieflüsse. - 7.4 Umgang mit Naturgefahren. - 7.5 Nachhaltige Ressourcennutzung. - 7.6 Governance und Partizipation. - 8. Forschungsinfrastrukturen. - 8.1 Forschungsflotte und Großgeräte. - 8.2 Mess- und Beobachtungstechnik. - 8.3 Daten- und Informationsinfrastrukturen. - 8.4 Modellierungsinfrastruktur. - 9. Innovative Technologien. - 10. Umsetzung des Forschungsprogramms. - 10.1 Zuwendungsgeber, Projektstruktur und Förderhöhe. - 10.2 Auswahlverfahren und Förderbestimmungen. - 10.3 Evaluation. - 11. Weitere Informationen und Ansprechpartner. - Impressum.
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  • 37
    Call number: AWI S5-18-91741
    Type of Medium: Monograph available for loan
    Pages: xcix, 2868 Seiten
    Edition: 10., vollständig überarbeitete und erweiterte Auflage
    ISBN: 9783452282750 (238.00 EUR)
    Series Statement: Heymanns Kommentare zum gewerblichen Rechtsschutz
    Language: German
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  • 38
    Call number: AWI G3-18-91864(ger) ; AWI G3-18-91864(eng) ; AWI G3-18-91864(rus)
    Type of Medium: Monograph available for loan
    Pages: 3 Bände in einem Schuber (204 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 978-3-88808-716-5 (ger) , 978-3-88808-714-1 (eng) , 978-3-88808-715-8 (rus)
    Language: German , English , Russian
    Note: Inhalt: Einführung und Hintergrund der terrestrischen Expeditionen in Sibirien / Hans-Wolfgang Hubberten, Dmitry Yu. Bolshiyanov, Mikhail N. Grigoriev, Volker Rachold, Eva-Maria Pfeiffer. - 1. Auf dem Weg zu den Lena-Expeditionen 1993-1997. - Seesedimente auf Taimyr und Sewernaja Semlja als Klima-Archiv / Pier Paul Overduin, Dmitry Yu. Bolshiyanov, Martin Melles. - Erste Studien zu Energie-, Wasser- und Spurengasflüssen in Tundraböden: Labas-See und Lewinson-Lessing-See, Taimyr-Halbinsel / Eva-Maria Pfeiffer, Julia Boike, Mikhail P. Zhurbenko, Dmitry Yu. Bolshiyanov. - Untersuchungen von Permafrost-Sequenzen in der Taimyr-Tiefebene (1994-1996) / Christine Siegert, Alexander Yu. Dereviagin. - Kohlenstoff in den arktischen Wüstenböden von Sewernaja Semlja / Eva-Maria Pfeiffer, Mikhail P. Zhurbenko, Dimitry Yu. Bolshiyanov. - Hydrologie, Geochemie und Sedimenttransport in den Flüssen Sibiriens - Das SYSTEM LAPTEV SEA Projekt 1994-1997 / Volker Rachold. - 2. Der Beginn der Lena-Expeditionen 1998-2002. - lnitiierung des Forschungsprojekts Lenadelta: Wissenschaftliche Strategie, Kooperation und Logistik / Volker Rachold, Martin Antonow, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Eva-Maria Pfeiffer. - Die ersten Jahre der boden- und klimabezogenen Permafrostforschung auf Samoilow und Umgebung (Untersuchungen 1998-2001) / Eva-Maria Pfeiffer, Julia Boike, Günter Stoof, Lars Kutzbach, Mikhail N. Grigoriev, lrina A. Yakshina, Anno N. Kurchatova, Dmitry Yu. Bolshiyanov. - Bykowski-Halbinsel: Die erste Landexpedition mit Fokus auf das Paläoklima / Lutz Schirrmeister, Guido Grosse, Viktor V. Kunitsky, Christine Siegert, Hanno Meyer. - Schiffsexpeditionen von 1998 bis 2002 zur Untersuchung von Erosion und Geomorphologie der Küste mit Dunai, Neptun, Sofron Danilov und Pavel Bashmakov / Volker Rachold, Waldemar Schneider, Mikhail N. Grigoriev, Hans-Wolfgong Hubberten, Felix E. Are, Dmitry Yu. Bolshiyanov. - Untersuchung von Seen auf Arga: Geschichte und Entstehung des Lenadeltas / Georg Schwamborn, Mikhail N. Grigoriev, Volker Rachold, Vladimir E. Tumskoy, Lutz Schirrmeister, Guido Grosse. - Mikrobieller Kohlenstoffumsatz in der Auftauschicht und im Permafrost / Susanne Liebner, Christian Knoblauch, Eva-Maria Pfeiffer, Svetlana Yu. Evgrafova, Dirk Wagner. - Feldarbeit für die Rekonstruktion der Paläoumwelt / Lutz Schirrmeister, Tatyana V. Kuznetsova, Andrei A. Andreev, Frank Kienast, Dmitry Yu. Bolshiyanov. - 3. Prozessstudien zur Permafrostdynamik 2002-2005. - Submarine Permafrostbohrungen während der COAST 2005 Expedition / Volker Rachold, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Waldemar Schneider. - Die frühe Forschungsstation Insel Samoilow und ihre Erweiterung 2005 / Hans-Wolfgang Hubberten, Julia Boike, Eva-Maria Pfeiffer, Günter Stoof, Alexander Yu. Gukav. - Installation des Samoilow Observatoriums - wissenschaftliches Monitoring von Klimadaten, Permafrostböden und Treibhausgasen (Untersuchungen 2002-2006) / Lars Kutzbach, Christian Wille, Torsten Sachs, David Holl, Günter Stoof Julia Boike, Mikhail N. Grigoriev, Eva-Maria Pfeiffer. - Mikrobieller Stickstoffumsatz in der Auftauschicht und den tieferen Permafrostsedimenten des Lenadeltas / Claudia Fiencke, Tina Sanders, Fabian Beermann, Elena E. Lebedeva, Eva-Maria Pfeiffer. - Geokryologische und paläoökologische Studien an den Küsten der Laptewsee / Lutz Schirrmeister, Christine Siegert, Guido Grosse, Hanno Meyer, Mikhail N. Grigoriev, Viktor V. Kunitsky. - Langzeitbeobachtungen der pelagischen Fauna in Seen und Tümpeln des Lenadeltas / Ekaterina N. Abramova, lrina I. Vishnyakova, Grigory A. Soloviev, Anna A. Abramova. - 4. Umsetzung neuer Forschungsthemen 2007-2012. - Die Dynamik der arktischen Küsten / Frank Günther, Mikhail N. Grigoriev, P. Paul Overduin, Hugues Lantuit, Hans-Wolfgang Hubberten. - Feldarbeit und Erstellung numerischer Modelle von submarinem Permafrost und Gashydraten / Hans-Wolfgang Hubberten, Pier Paul Overduin, Sebastian Wetterich, Mikhail N. Grigoriev. - Permafrostdegradation, Thermokarst und Thermoerosion - Feldforschung auf der Insel Kurungnach / Anne Morgenstern, lrina V Fedorova, Antonina A. Chetverova, Frank Günther, Mathias Ulrich, Fabian Beermann, Sebastian Zubrzycki, Sofia A. Antonova, Samuel Stettner, Julia Boike. - Mit Kettensäge zum Klimamodell - Eiskeile als Winterklima-Archive / Hanno Meyer, Thomas Opel, Alexander Yu. Dereviagin. - Veränderungen nordsibirischer Seen und Baumgrenzen in der Vergangenheit und Gegenwart als Reaktion auf Erwärmung / Ulrike Herzschuh, Luidmila A. Pestryakova, Laura S. Epp, Larisa A. Frolova, Ruslan M. Gorodnichev, Birgit Heim, Florion Jeltsch, Juliane Klemm, Stefan Kruse, Larisa B. Nazarova, Bastian Niemeyer, Anatolii N. Nikolaev, Kathleen R. Stoof-Leichsenring, Ralph Tiedemann, Mareike Wieczoreck, Evgenij S. Zakharov, Heike H. Zimmermann. - Kohlenstoff in Permafrost - Quantifizierung der Menge an organischem Material in Sibirien / Jens Strauss, Lutz Schirrmeister, Sebastian Zubrzycki, Alexander L. Kholodov, Mikhail N. Grigoriev, Viktor V. Kunitsky, Matthias Fuchs, Eva-Maria Pfeiffer, Guido Grosse. - Expeditionen mit Gummibooten und kleinen Flussbooten - Hydrologie und Geomorphologie des Lenadeltas / Dmitry Yu. Bolshiyanov, lrina V Fedorova, Julia Boike. - Mobilisierung und Ablagerung von Kohlenstoff im Lena-Flusssystem / Gesine Mollenhauer, Maria Winterfeld, Boris P. Koch, lrina V. Fedorova. - Holozäne Seen rund um das Lenadelta / Bernhard Diekmann, Boris Biskaborn, Luidmila A. Pestryakova, Dmitry A. Subetto, Dmitry Yu. Bolshiyanov, Ulrike Herzschuh, Georg Schwamborn, Volker Rachold. - Logistisch komplexe Einsätze - Beobachtungen von Energie und Treibhausgasflüssen aus der Luft mittels Helipod / Torsten Sachs, Eric Larmanau, Katrin Kohnert, Andrei Serafimavich. - Lena Expeditionen: Einbindung neuer deutscher Forschungsgruppen / Birgit Heim, Hans-Wolfgang Hubberten, Pier Paul Overduin, lrina V. Fedorova. - Ein Jahrzehnt der Küstenforschung im Lenadelta / lngeborg Bussmann, Dmitry Yu. Bolshiyanov, lrina V Fedorova, Mikhail N. Grigoriev, Alexander Yu. Gukov, Gerhard Kattner, Alexandra Kraberg, Denis V. Moiseev, Pier Paul Overduin, Lasse Sander, Karen H. Wiltshire. - 5. Neue Horizonte für Lena-Expeditionen - Die neue Forschungsstation Insel Samoilow. - Ministerpräsident W. W. Putin besucht die Insel Samoilow (P-Day) / Hanno Meyer, Thomas Opel, Alexander Yu. Dereviagin, Svetlana Yu. Evgrafava, Waldemar Schneider, Alexander S. Makarov, Mikhail N. Grigoriev. - Die neue Forschungsstation Insel Samoilow: Bau, Eröffnungsfeier, Anlage und Betrieb / Mikhail N. Grigoriev, Hans-Wolfgang Hubberten, Igor N. Yeltsov, Anne Morgenstern. - Samoilow in internationalen Programmen und Netzwerken - FLUXNET, GTN-P, INTERACT / Anne Morgenstern, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Julia Boike, Lars Kutzbach. - Kurzer Überblick über die russisch-deutschen Permafrost-Projekte CARBOPERM und KoPf / Eva-Maria Pfeiffer, Hans-Wolfgang Hubberten, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Sebastian Zubrzycki, Ulrike Herzschuh, Guido Grosse. - Einsatz von Fernerkundung im Gebiet der Laptewsee / Guido Grosse, Birgit Heim, Sofia Antonova, Julia Boike, Astrid Bracher, Alexey N. Fague, Frank Günther, Thomas Krumpen, Moritz Langer, Anne Morgenstern, Sina Muster, lngmar Nitze, Torsten Sachs. - Multidisziplinäre Studien auf Samoilow und Kurungnach: Geophysik, Fernerkundung, Geologie sowie botanische und Bodenstudien / Igor N. Yeltsov, Alexey N. Faguet, Leonid V. Tsibizov, Vladimir A. Kashirtsev, Vladimir V. Olenchenko, Andrey A. Kartozia, Nikolay N. Lashchinskiy. - Terrestrische Permafrost-Bohrkampagnen: Tiefe Einblicke in die Vergangenheit / Jens Strauss, Mikhail N. Grigoriev, Paul Overduin, Georgii Maximov, Guido Grosse, Alexey N. Fague, Leonid Tsibizov, Lutz Schirrmeister. - Langzeitmessungen der Energie-, Wasser-, und Treibhausgasflüsse zwischen Land und Atmosphäre von 2002 bis heute und darüber hinaus / David Holl, Ju , Contents: Introduction and Background to Terrestrial Expeditions in Siberia / Hans-Wolfgang Hubberten, Dmitry Yu. Bolshiyanov, Mikhail N. Grigoriev, Volker Rachold, Eva-Maria Pfeiffer. - 1. On the Way to the Lena Expeditions 1993-1997. - Lake Sediments on Taymyr and Severnaya Zemlya as a Climate Archive / Pier Paul Overduin, Dmitry Yu. Bolshiyanov, Martin Melles. - First Energy, Water, and Flux Studies of Tundra Soils - Labaz and Levinson-Lessing Lake, Taymyr Peninsula / Eva-Maria Pfeiffer, Julia Boike, Mikhail P. Zhurbenko, Dmitry Yu. Bolshiyanov. - Exploring Permafrost Sequences in the Taymyr Lowland (1994-1996) / Christine Siegert, Alexander Yu. Dereviagin. - Carbon in Arctic Desert Soils of Severnaya Zemlya / Eva-Maria Pfeiffer, Mikhail P. Zhurbenko, Dimitry Yu. Bolshiyanov. - Hydrology, Geochemistry, and Sediment Transport of the Siberian Rivers - The SYSTEM LAPTEV SEA Project 1994-1997 / Volker Rachold. - 2. The Beginning of the Lena Expeditions 1998-2002. - Initiation of the Research Project Lena Delta: Science Strategy, Cooperation, and Logistics / Volker Rachold, Martin Antonow, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Eva-Maria Pfeiffer. - The First Years of Soil and Climate-Related Permafrost Research on Samoylov Island and Surroundings (Investigations 1998- 2001) / Eva-Maria Pfeiffer, Julia Boike, Günter Stoof, Lars Kutzbach, Mikhail N. Grigoriev, lrina A. Yakshina, Anno N. Kurchatova, Dmitry Yu. Bolshiyanov. - Bykovsky Peninsula: The First Land Expedition with a Focus on Paleoclimate / Lutz Schirrmeister, Guido Grosse, Viktor V. Kunitsky, Christine Siegert, Hanno Meyer. - The 1998-2002 Ship-Based Expeditions for Coastal Erosion and Geomorphological Studies with Dunay, Neptun, Sofron Danilov, and Pavel Bashmakov / Volker Rachold, Waldemar Schneider, Mikhail N. Grigoriev, Hans-Wolfgang Hubberten, Felix E. Are, Dmitry Yu. Bolshiyanov. - Lake Studies on Arga: History and Formation of the Lena Delta / Georg Schwamborn, Mikhail N. Grigoriev, Volker Rachold, Vladimir E. Tumskoy, Lutz Schirrmeister, Guido Grosse. - Microbial Carbon Turnover in the Active Layer and in Permafrost / Susanne Liebner, Christian Knoblauch, Eva-Maria Pfeiffer, Svetlana Yu. Evgrajova, Dirk Wagner. - Fieldwork for Reconstructing the Paleo-Environment / Lutz Schirrmeister, Tatyana V. Kuznetsova, Andrei A. Andreev, Frank Kienast, Dmitry Yu. Bolshiyanov. - 3. Process Studies of Permafrost Dynamics 2002-2006. - Subsea Permafrost Drilling During the COAST 2005 Expedition / Volker Rachold, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Waldemar Schneider. - The Early Samoylov Station and Its Extension in 2005 / Hans-Wolfgang Hubberten, Julia Boike, Eva-Maria Pfeiffer, Günter Stoof, Alexander Yu. Gukov. - Installation of the Samoylov Observatory - Permafrost-Affected Soils and Greenhouse Gases (Investigations 2002-2006) / Lars Kutzbach, Christian Wille, Torsten Sachs, David Holl, Günter Stoof, Julia Boike, Mikhail N. Grigoriev, Eva-Maria Pfeiffer. - Microbial Nitrogen Turnover in the Active Layer and Deeper Permafrost Sediments of the Lena River Delta / Claudia Fiencke, Tina Sanders, Fabian Beermann, Elena E. Lebedeva, Eva-Maria Pfeiffer. - Geocryological and Paleoenvironmental Studies on the Coasts of the Laptev Sea / Lutz Schirrmeister, Christine Siegert, Guido Grosse, Hanno Meyer, Mikhail N. Grigoriev, Viktor V. Kunitsky. - Long-Term Observations of the Pelagic Fauna in Lakes and Ponds in the Lena Delta / Ekaterina N. Abramova, lrina I. Vishnyakova, Grigory A. Soloviev, Anna A. Abramova. - 4. Implementation of New Research Topics 2007-2012. - Arctic Coastal Dynamics / Frank Günther, Mikhail N. Grigoriev, Pier Paul Overduin, Hugues Lantuit, Hans-Wolfgang Hubberten. - Field Work and Numerical Modelling for Subsea Permafrost and Gas Hydrates / Hans-Wolfgang Hubberten, Pier Paul Overduin, Sebastian Wetterich, Mikhail N. Grigoriev. - Permafrost Degradation, Thermokarst and Thermal Erosion Fieldwork on Kurungnakh Island / Anne Morgenstern, Irina V. Fedorova, Antonina A. Chetverova, Frank Günther, Mathias Ulrich, Fabian Beermann, Sebastian Zubrzycki, Sofia A. Antonova, Samuel Stettner, Julia Boike. - With the Chainsaw to Climate Modelling - Ice Wedges as a Winter Climate Archive / Hanno Meyer, Thomas Opel, Alexander Yu. Dereviagin. - Past and Present Treeline and Lake Changes in Northern Siberia in Response to Warming / Ulrike Herzschuh, Luidmila A. Pestryakova, Laura S. Epp, Larisa A. Frolova, Ruslan M. Gorodnichev, Birgit Heim, Florion Jeltsch, Juliane Klemm, Stefan Kruse, Larisa B. Nazarova, Bastian Niemeyer, Anatolii N. Nikolaev, Kathleen R. Stoof-Leichsenring, Ralph Tiedemann, Mareike Wieczoreck, Evgenij S. Zakharov, Heike H. Zimmermann. - Organic Matter Matters- Quantifying the Amount of Carbon in Northern Siberia / Jens Strauss, Lutz Schirrmeister, Sebastian Zubrzycki, Alexander L. Kholodov, Mikhail N. Grigoriev, Viktor V. Kunitsky, Matthias Fuchs, Eva-Maria Pfeiffer, Guido Grosse. - Expeditions with Rubber Boats and Small River Vessels - Hydrology and Geomorphology of the Lena Delta / Dmitry Yu. Bolshiyanov, lrina V Fedorova, Julia Boike. - Mobilization and Deposition of Carbon in the Lena River System / Gesine Mollenhauer, Maria Winterfeld, Boris P. Koch, lrina V. Fedorova. - Holocene Lakes Around the Lena Delta / Bernhard Diekmann, Boris Biskaborn, Luidmila A. Pestryakova, Dmitry A. Subetto, Dmitry Yu. Bolshiyanov, Ulrike Herzschuh, Georg Schwamborn, Volker Rachold. - Complex Logistical Operations - Airborne Energy and Greenhouse Gas Flux Observations by Helipod / Torsten Sachs, Eric Larmanau, Katrin Kohnert, Andrei Serafimavich. - Lena Expeditions: Integration of New German Research Groups / Birgit Heim, Hans-Wolfgang Hubberten, Pier Paul Overduin, lrina V. Fedorova. - A Decade of Coastal Research in the Lena Delta / lngeborg Bussmann, Dmitry Yu. Bolshiyanov, lrina V Fedorova, Mikhail N. Grigoriev, Alexander Yu. Gukov, Gerhard Kattner, Alexandra Kraberg, Denis V. Moiseev, Pier Paul Overduin, Lasse Sander, Karen H. Wiltshire. - 5. New Horizons for Lena Expeditions - The New Research Station Samoylov Island. - Prime Minister V. V. Putin Visits Samoylov Island (P-Day) / Hanno Meyer, Thomas Opel, Alexander Yu. Dereviagin, Svetlana Yu. Evgrafava, Waldemar Schneider, Alexander S. Makarov, Mikhail N. Grigoriev. - The New Research Station Samoylov Island: Construction, Opening Ceremony, Facilities, and Operation / Mikhail N. Grigoriev, Hans-Wolfgang Hubberten, Igor N. Yeltsov, Anne Morgenstern. - Samoylov in International Programs and Networks - FLUX NET, GTN-P, INTERACT / Anne Morgenstern, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Julia Boike, Lars Kutzbach. - Short Overview of the Russian-German Permafrost Projects CARBOPERM and KoPf / Eva-Maria Pfeiffer, Hans-Wolfgang Hubberten, Mikhail N. Grigoriev, Dmitry Yu. Bolshiyanov, Sebastian Zubrzycki, Ulrike Herzschuh, Guido Grosse. - Application of Remote Sensing in the Laptev Sea Region / Guido Grosse, Birgit Heim, Sofia Antonova, Julia Boike, Astrid Bracher, Alexey N. Fague, Frank Günther, Thomas Krumpen, Moritz Langer, Anne Morgenstern, Sina Muster, lngmar Nitze, Torsten Sachs. - Multidisciplinary Studies on Samoylov and Kurungnakh: Geophysics, Remote Sensing, Geology, Botanical, and Soil Studies / Igor N. Yeltsov, Alexey N. Faguet, Leonid V. Tsibizov, Vladimir A. Kashirtsev, Vladimir V. Olenchenko, Andrey A. Kartozia, Nikolay N. Lashchinskiy. - Deep lnsights into the Past Terrestrial Permafrost Drilling Campaigns / Jens Strauss, Mikhail N. Grigoriev, Paul Overduin, Georgii Maximov, Guido Grosse, Alexey N. Fague, Leonid Tsibizov, Lutz Schirrmeister. - Long-Term Measurements of Land-Atmosphere Fluxes of Energy, Water, and Greenhouse Gases from 2002 until Today and Beyond / David Holl, Julia Boike, Torsten Sachs, Peter Schreiber, Niko Bornemann, Christian Wille, Eva-Maria Pfeiffer, Irina V. Fedorova, Lars Kutzbach. - Carbon Turnover of Thawing Permafrost in the Lena Delta / , Russische Ausgabe in kyrillischer Schrift
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  • 39
    Call number: AWI G6-19-92375
    In: Berichte / Christian-Albrechts-Universität zu Kiel, Institut für Geowissenschaften, Nr. 9
    Type of Medium: Monograph available for loan
    Pages: 278 Seiten , Illustrationen
    ISSN: 0175-9302
    Series Statement: Berichte / Christian-Albrechts-Universität zu Kiel, Institut für Geowissenschaften 9
    Language: German
    Note: Zugleich: Dissertation, Christian-Albrechts-Universität zu Kiel, 1999 , INHALTSVERZEICHNIS 1. Einleitung 1.1 Kenntnisstand und offene Fragen 1.2 Fragestellung und Ziele dieser Arbeit 2. Umweltbedingungen in den Arbeitsgebieten 2.1 Hydrographie, Eisverhältnisse und NAO 2.2 Zur Variation von Wassertiefe und Breite der Dänemarkstraße und zur Vereisung Islands während des letzten Glazials 3. Methoden 3.1 Auswahl der Kernstationen 3.2 Probennahme und Analysen (Übersicht) 3.3 Zur Rekonstruktion von Paläobedingungen im Oberflächenwasser Zur Aussage stabiler Isotopenverhältnisse in planktischen Foraminiferen Zur Messung stabiler Isotopenverhältnisse Zur Massenspektrometrie Zur Rekonstruktion von Oberflächentemperaturen Alkane und Alkohole als Maß für Staubeintrag Eistranspmtiertes Material und vulkanische Aschen 3.4 Zur Rekonstruktion von Paläobedingungen im Zwischen-/ Tiefenwasser Häufigkeit von Cibicides- und anderen benthischen Arten (inkl. Taxonomie) Stabile Isotopenverhältnisse in benthischen Foraminiferen 3.5 AMS 14C-Datierungen Probenreinigung 3. 6 Hauptelementanalysen von vulkanischen Asche-Leithorizonten 3. 7 Geomagnetische Meßgrößen und magnetische Suszeptibiltät 3.8 Techniken zur Spektralanalyse 4. Methodische Ergebnisse 4.1 Zum Einfluß der Probenreinigung auf δ18O-/ δ13C-Werte 4.2 Probleme bei der langfristigen Reproduzierbarkeit von δ18O-Zeitreihen 4.3 Einfluß der Korngröße und Artendefinition planktischer Foraminiferen auf SST-Rekonstruktionen in hohen Breiten 4.4 Vergleich der stabilen Isotopenwerte von Cibicides lobatulus und Cibicidoides wuellerstorfi 5. Stratigraphische Grundlagen und Tiefenprofile der Klimasignale 5.1 Stratigraphische Korrelation zwischen parallel-gekernten GKG- und SL-/KL-Profilen 5.2 Flanktische δ18O-/ δ13C-Kurven, 14C-Alter und biostratigraphische Fixpunkte Westliches Islandbecken Kern PS2644 Kern PS2646 Kern PS2647 Kern 23351 Vøring-Plateau Kern 23071 Kern 23074 5.3 Benthische δ18O-/ δ13C-Werte in Kern PS2644 5.4 Siliziklastische Sedimentkomponenten: Eistransportiertes Material Westliches Islandbecken Kern PS2644 Kern PS2646 Kern PS2647 Vøring-Plateau Kern 23071 Kern 23074 5.5 Vulkanische Glasscherben in Kern PS2644: Wind- und Eiseintrag 5.6 Geochemie und Alter einzelner Tephralagen als Leithorizonte Westliches Islandbecken Kern PS2644 Kern PS2646 Kern PS2647 Vøring-Plateau Kern 23071 Kern 23074 5.7 Magnetische Suszeptibilität in den Kernen PS2644, PS2646 und PS2647 Kern PS2644 Kern PS2646 und PS2647 5.8 Geomagnetische Feldintensität und Richtungsänderungen in Kern PS2644 5.9 Variation von Planktonfauna und -flora Westliches Islandbecken: Kern PS2644 Kern PS2646 und PS2647 Vøring-Plateau: Kern 23071 und 23074 5.10 Benthische Foraminiferen in Kern PS2644 6. Entwicklung von Temperatur und Salzgehalt nördlich der Dänemark-Straße 6.1 Variation der Oberflächentemperatur nach Planktonforaminiferen 6.2 Variation der Oberflächentemperatur nach Uk37 6.3 Variation der Oberflächensalinität 7. Die Feinstratigraphie von Kern PS2644 als Basis für eine Eichung der 14C-Altersskala 22 - 55 ka 7.1 Korrelation zwischen den Klimasignalen in Kern PS2644 und der GISP2-Klimakurve zum Kalibrieren der 14C-Alter und Erstellen eines Altersmodells Tephrachronologische Marker Korrelationsparameter und -regeln Sonderfälle/ Probleme bei der Korrelation 7.2 Alters-stratigraphische Korrelation der Klimakurven von Kern 23071 und 23074 7.3 Variation der Altersanomalien zwischen 20 und 55 14C-ka 7.4 Variabilität des planktischen 14C-Reservoiralters in Schmelzwasserbeeinflußten Seegebieten Variation der planktischen 14C-Alter unmittelbar an der Basis von Heinrich-Ereignis 4 Unterschiede zwischen planktischen und benthischen 14C-Altern in der westlichen Islandsee. Zur Erklärung der inversen Altersdifferenzen 7.5 Differenz zwischen 14C- und Kalenderalter: Zeitliche Variation unter Einfluß des Erdmagnetfeldes - Modell und Befund 7.6 Sedimentationsraten der Kerne 23071, 23074 und PS2644 nach dem GISP2-Altersmodell Vøring-Plateau: Kerne 23071 und 23074 Südwest-Islandsee: Kern PS2644 8. Klimaoszillationen im Europäischen Nordmeer in der Zeit und Frequenzdomäne 8.1 "Der Einzelzyklus" in den Klimakurven von Kern PS2644 8.2 Zur Veränderlichkeit der Warm- und Kaltextreme sowie Zyklenlänge Besonderheiten in der Zyklenlänge Variation der Kalt-(Stadiale) Variation der Interstadiale 8.3 Periodizitäten der Klimasignale im Frequenzband der D.-Oe.-Zyklen. Der D.-Oe.-Zyklus von 1470 J., seine Multiplen und harmonischen Schwingungen Weitere Frequenzen: 1000-1150 Jahre- und 490- 510 Jahre-Zyklizitäten Höhere Frequenzen im Bereich von Jahrhunderten und Dekaden 8.4 Phasenbeziehungen und (örtliche) Steuemngsmechanismen der Dansgaard-Oeschger-Zyklen 9. Schlußfolgerungen Danksagung Literaturverzeichnis Anhang
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  • 40
    Call number: AWI G3-19-92383
    Description / Table of Contents: In ice-rich permafrost regions, changes in the permafrost thermal regime cause surface disturbances. These changes are amplified by the increase in air temperatures recorded in the Arctic in the past decades. Thermokarst is a process that leads to surface subsidence and formation of characteristic landforms following thawing of ice-rich permafrost or melting of massive ice. Thermokarst is widespread on hillslopes and the number of associated landforms is increasing in the Arctic. Through this process large amounts of material are eroded and transported to the sea or accumulate along hillslopes. While hillslope thermokarst modifies terrestrial and aquatic ecosystems, there is limited understanding of its environmental impact at a regional scale. In this thesis we quantify the environmental impacts of hillslope thermokarst on the valley and nearshore ecosystems along the Yukon Coast, Canada. Using supervised machine learning, we identified geomorphic factors that favour the development of coastal retrogressive thaw slump (RTS), one of the most dynamic hillslope thermokarst landform. Coastal geomorphology and ground ice type and content play a major role in RTS occurrence. Using aerial photographs and satellite imagery, we traced the evolution of RTSs between 1952 and 2011. During this time, the number and areal coverage of RTSs increased by 73%. RTSs eroded and partly released to the nearshore zone organic carbon contained in millions of cubic meters of material. Our results show that 56% of the RTSs identified along the coast in 2011 have eroded 16.6 × 10^6 m3 of material; a large part (45%) was transported alongshore due to coastal processes. Moreover, we show that RTSs are a major contributor to the carbon budget in the nearshore ecosystem: 17% of the coastal RTSs identified in 2011 contributed annually up to 0.6% of the organic carbon released by coastal retreat along the Yukon Coast. To assess the impact of hillslope thermokarst on the terrestrial ecosystem, we measured the spatial distribution of soil organic carbon (SOC) and total nitrogen (TN) along hillslopes in three Arctic valleys. We highlight the high spatial variability in the distribution of SOC and TN in the valleys. This distribution is caused by complex soil processes occurring along the hillslopes. Hillslope thermokarst impacts the degradation of organic matter and affects the storage of SOC and TN.
    Type of Medium: Dissertations
    Pages: xvii, 103 Seiten , Illustrationen
    Language: English
    Note: Dissertation, Universität Potsdam, 2018 , Contents Acknowledgements Abstract (English/Deutsch/Français) List of figures List of tables 1 Introduction 1.1 Scientic background 1.1.1 The Arctic coast, permafrost and climate change 1.1.2 Organic carbon in permafrost soils 1.1.3 Hillslope thermokarst processes 1.2 Aims 1.3 Study region 1.4 Methods 1.4.1 Mapping 1.4.2 Spline interpolation and volumes estimations 1.4.3 Fieldwork 1.4.4 Geochemical analyses 1.4.5 Statistical analyses 1.5 Thesis outline 1.6 Authors’ contributions 2 Synthesis 2.1 Retrogressive thaw slumps are widely spread in ice-rich permafrost areas 2.2 Retrogressive thaw slumps contribute signicantly to the nearshore or-ganic carbon 2.3 Thermokarst impacts the distribution of soil organic carbon along hill-slopes 2.4 Outlook . 3 Terrain Controls on the Occurrence of Coastal RTSs 3.1 Abstract 3.2 Introduction 3.3 Study area 3.4 Methods 3.4.1 Mapping of retrogressive thaw slumps and landform classication 3.4.2 Environmental variables 3.4.3 Univariate regression trees 3.5 Results 3.5.1 Characteristics of retrogressive thaw slumps 3.5.2 Density and areal coverage of retrogressive thaw slumps 3.6 Discussion 3.6.1 Characteristics and distribution of retrogressive thaw slumps 3.6.2 Terrain factors explaining retrogressive thaw slump occurrence 3.6.3 Coastal Processes 3.7 Conclusion 4 RTSs release sediments and organic carbon into the Arctic Ocean 4.1 Abstract 4.2 Introduction 4.3 Study Area 4.4 Methods 4.4.1 Evolution of retrogressive thaw slumps 4.4.2 Volume Estimations 4.4.3 Estimates of soil and dissolved organic carbon values 4.5 Results 4.5.1 Evolution of retrogressive thaw slumps between 1952 and 2011 4.5.2 Eroded material and estimated amount of mobilized SOC and DOC 4.6 Discussion 4.6.1 Increase in slump activity 4.6.2 Eroded material from retrogressive thaw slumps and organic car-bon uxes 4.6.3 Impact of retrogressive thaw slumps on the coastal ecosystem 4.7 Conclusion 5 Snapshot of carbon and nitrogen distribution in Arctic valleys 5.1 Abstract 5.2 Introduction 5.3 Study Area 5.4 Methods 5.4.1 Spatial analyses 5.4.2 Sampling Scheme 5.4.3 Geochemical analyses 5.4.4 Environmental variables and statistical analyses 5.5 Results 5.5.1 Geomorphology of the valleys 5.5.2 Spatial distribution of carbon and nitrogen 5.5.3 Correlations between soil characteristics and geochemical variables 5.6 Discussion 5.6.1 Variability in soil and geochemical properties in Arctic valleys 5.6.2 Hillslope Processes 5.7 Conclusion 6 Eidessttatliche Erklärung A Appendix A.1 Chapter 3 A.2 Chapter 4 A.3 Chapter 5 Bibliography
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  • 41
    Call number: AWI G3-19-92384
    Description / Table of Contents: Widespread landscape changes are presently observed in the Arctic and are most likely to accelerate in the future, in particular in permafrost regions which are sensitive to climate warming. To assess current and future developments, it is crucial to understand past environmental dynamics in these landscapes. Causes and interactions of environmental variability can hardly be resolved by instrumental records covering modern time scales. However, long-term environmental variability is recorded in paleoenvironmental archives. Lake sediments are important archives that allow reconstruction of local limnogeological processes as well as past environmental changes driven directly or indirectly by climate dynamics. This study aims at reconstructing Late Quaternary permafrost and thermokarst dynamics in central-eastern Beringia, the terrestrial land mass connecting Eurasia and North America during glacial sea-level low stands. In order to investigate development, processes and influence of thermokarst dynamics, several sediment cores from extant lakes and drained lake basins were analyzed to answer the following research questions: 1. When did permafrost degradation and thermokarst lake development take place and what were enhancing and inhibiting environmental factors? 2. What are the dominant processes during thermokarst lake development and how are they reflected in proxy records? 3. How did, and still do, thermokarst dynamics contribute to the inventory and properties of organic matter in sediments and the carbon cycle? Methods applied in this study are based upon a multi-proxy approach combining sedimentological, geochemical, geochronological, and micropaleontological analyses, as well as analyses of stable isotopes and hydrochemistry of pore-water and ice. Modern field observations of water quality and basin morphometrics complete the environmental investigations. The investigated sediment cores reveal permafrost degradation and thermokarst dynamics on different time scales. The analysis of a sediment core from GG basin on the northern Seward Peninsula (Alaska) shows prevalent terrestrial accumulation of yedoma throughout the Early to Mid Wisconsin with intermediate wet conditions at around 44.5 to 41.5 ka BP. This first wetland development was terminated by the accumulation of a 1-meter-thick airfall tephra most likely originating from the South Killeak Maar eruption at 42 ka BP. A depositional hiatus between 22.5 and 0.23 ka BP may indicate thermokarst lake formation in the surrounding of the site which forms a yedoma upland till today. The thermokarst lake forming GG basin initiated 230 ± 30 cal a BP and drained in Spring 2005 AD. Four years after drainage the lake talik was still unfrozen below 268 cm depth. A permafrost core from Mama Rhonda basin on the northern Seward Peninsula preserved a full lacustrine record including several lake phases. The first lake generation developed at 11.8 cal ka BP during the Lateglacial-Early Holocene transition; its old basin (Grandma Rhonda) is still partially preserved at the southern margin of the study basin. Around 9.0 cal ka BP a shallow and more dynamic thermokarst lake developed with actively eroding shorelines and potentially intermediate shallow water or wetland phases (Mama Rhonda). Mama Rhonda lake drainage at 1.1 cal ka BP was followed by gradual accumulation of terrestrial peat and top-down refreezing of the lake talik. A significant lower organic carbon content was measured in Grandma Rhonda deposits (mean TOC of 2.5 wt%) than in Mama Rhonda deposits (mean TOC of 7.9 wt%) highlighting the impact of thermokarst dynamics on biogeochemical cycling in different lake generations by thawing and mobilization of organic carbon into the lake system. Proximal and distal sediment cores from Peatball Lake on the Arctic Coastal Plain of Alaska revealed young thermokarst dynamics since about 1,400 years along a depositional gradient based on reconstructions from shoreline expansion rates and absolute dating results. After its initiation as a remnant pond of a previous drained lake basin, a rapidly deepening lake with increasing oxygenation of the water column is evident from laminated sediments, and higher Fe/Ti and Fe/S ratios in the sediment. The sediment record archived characterizing shifts in depositional regimes and sediment sources from upland deposits and re-deposited sediments from drained thaw lake basins depending on the gradually changing shoreline configuration. These changes are evident from alternating organic inputs into the lake system which highlights the potential for thermokarst lakes to recycle old carbon from degrading permafrost deposits of its catchment. The lake sediment record from Herschel Island in the Yukon (Canada) covers the full Holocene period. After its initiation as a thermokarst lake at 11.7 cal ka BP and intense thermokarst activity until 10.0 cal ka BP, the steady sedimentation was interrupted by a depositional hiatus at 1.6 cal ka BP which likely resulted from lake drainage or allochthonous slumping due to collapsing shore lines. The specific setting of the lake on a push moraine composed of marine deposits is reflected in the sedimentary record. Freshening of the maturing lake is indicated by decreasing electrical conductivity in pore-water. Alternation of marine to freshwater ostracods and foraminifera confirms decreasing salinity as well but also reflects episodical re-deposition of allochthonous marine sediments. Based on permafrost and lacustrine sediment records, this thesis shows examples of the Late Quaternary evolution of typical Arctic permafrost landscapes in central-eastern Beringia and the complex interaction of local disturbance processes, regional environmental dynamics and global climate patterns. This study confirms that thermokarst lakes are important agents of organic matter recycling in complex and continuously changing landscapes.
    Type of Medium: Dissertations
    Pages: XII, 128 Seiten , Illustrationen , 1 DVD
    Language: English
    Note: Enthält 5 Publikationen: 1) Mid Wisconsin to Holocene permafrost and landscape dynamics based on a drained lake basin core from the northern Seward Peninsula, northwest Alaska / Josefine Lenz, Guido Grosse, Benjamin M. Jones [und 5 weitere] 2) Evidence of multiple thermokarst lake generations from an 11,800-year old permafrost core on the northern Seward Peninsula, Alaska / Josefine Lenz, Sebastian Wetterich, Benjamin M. Jones [und 3 weitere] 3) Impacts of shore expansion and catchment characteristics on lacustrine thermokarst records in permafrost lowlands, Alaska Arctic Coastal Plain / Josefine Lenz, Sebastian Wetterich, Benjamin M. Jones [und 5 weitere] 4) Periglacial landscape dynamics in the western Canadian Arctic: Results from a thermokarst lake record on a push moraine (Herschel Island, Yukon) / Josefine Lenz, Michael Fritz, Lutz Schirrmeister [und 4 weitere] 5) Regional environmental change versus local signal preservation in Holocene thermokarst lake sediments: A case study from Herschel Island, Yukon (Canada) / Michael Fritz, Ingmar Unkel, Josefine Lenz [und 6 weitere] , Table of contents Abstract Zusammenfassung Abbreviations and nomenclature 1 Thesis organization 1.1 Overview of chapters 1.2 Author contribution 2 Introduction 2.1 Scientific background 2.1.1 Arctic environments and permafrost in the study region of Beringia 2.1.2 Permafrost degradation and its global feedbacks 2.1.3 Thermokarst lakes and basins as paleoenvironmental archives 2.2 Aims and approaches 3 Mid Wisconsin to Holocene permafrost and landscape dynamics based on a drained lake basin core from the northern Seward Peninsula, northwest Alaska 3.1 Abstract 3.2 Introduction 3.3 Study area 3.4 Material and methods 3.5 Results 3.5.1 Core stratigraphy 3.5.2 Cryostratigraphy 3.5.3 Grain size distribution 3.5.4 Magnetic susceptibility 3.5.5 Biogeochemical characteristics 3.5.6 Tephra 3.5.7 Palaeoecology 3.5.8 Geochronology 3.6 Discussion 3.7 Conclusions 4 Evidence of multiple thermokarst lake generations from an 11,800-year old permafrost core on the northern Seward Peninsula, Alaska 4.1 Abstract 4.2 Introduction 4.3 Study area 4.4 Material and methods 4.5 Results 4.5.1 Geochronology 4.5.2 Cryolithological description 4.5.3 Geochemical results 4.5.4 Bioindicators 4.5.5 Characteristics of intra-sedimentary ice and comparison with modern waters 4.6 Discussion 4.6.1 Thermokarst lake dynamics 4.6.2 Regional lake dynamics and global environmental change 4.6.3 Carbon cycling 4.7 Conclusions 5 Impacts of shore expansion and catchment characteristics on lacustrine thermokarst records in permafrost lowlands, Alaska Arctic Coastal Plain 5.1 Abstract 5.2 Introduction 5.3 Study area 5.4 Material and methods 5.5 Results 5.5.1 Sedimentological results of near-shore core P1 5.5.2 Sedimentological and palynological results of lake center-cores P2 (and P3) 5.5.3 Lake age estimation 5.6 Discussion 5.6.1 Thermokarst lake development 5.6.2 Impact of catchment genesis and morphology on the lake sediment record 5.6.3 Carbon degradation 5.7 Conclusions 6 Synthesis 6.1 Study sites in central-eastern Beringia: Similarities and differences 6.2 Permafrost degradation and thermokarst development in central-eastern Beringia 6.2.1 Timing of thermokarst development 6.2.2 Environmental factors supporting and inhibiting thermokarst 6.3 Processes of thermokarst lake development and their imprint in proxy records 6.4 Contribution of thermokarst dynamics to the carbon cycle 6.5 Potentials/limitations of thermokarst lake archives and outlook Bibliography Appendix I: Periglacial landscape dynamics in the western Canadian Arctic: Results from a thermokarst lake record on a push moraine (Herschel Island, Yukon) I-1 Abstract I-2 Introduction I-3 Study area I-4 Material and methods I-5 Results I-5.1 Core lithology I-5.2 Radiography I-5.3 Magnetic susceptibility and water content I-5.4 Grain size distribution I-5.5 Biogeochemical characteristics I-5.6 Geochronology I-6 Discussion I-6.1 Evolution of Lake Herschel I-6.2 Paleoenvironmental implications of the Lake Herschel record I-7 Conclusions Appendix II: Regional environmental change versus local signal preservation in Holocene thermokarst lake sediments: A case study from Herschel Island, Yukon (Canada) II-1 Abstract II-2 Introduction and study area II-3 Material and methods II-3.1 Sediment core II-3.2 Radiocarbon dating and age modelling II-3.3 Pore-water chemistry II-3.4 X-ray fluorescence (XRF) scanning II-3.5 Micropaleontology II-4 Results II-4.1 Chronostratigraphy: The revised age model II-4.2 XRF chemistry II-4.3 Pore-water chemistry II-4.4 Calcareous microfossils II-4.5 Pollen II-5 Discussion II-5.1 Sedimentation history of Lake Herschel II-5.2 Limnological, sedimentary and geochemical properties predefine the habitat I-5.3 Autochthonous versus allochthonous deposition of calcareous microfossils II-5.4 Regional pollen-based reconstruction of vegetation and climate II-6 Conclusions Acknowledgements
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  • 42
    Monograph available for loan
    Monograph available for loan
    Köln : Carl Heymanns Verlag
    Call number: AWI S5-19-92101
    Type of Medium: Monograph available for loan
    Pages: XXI, 311 Seiten , Illustrationen
    ISBN: 9783452291295 , 3452291294
    Language: German
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  • 43
    Series available for loan
    Series available for loan
    Offenbach/M. : Deutscher Wetterdienst
    Associated volumes
    Call number: ZSP-652-102
    In: Promet, Heft 102
    Description / Table of Contents: In diesem Heft sind Beiträge zusammengestellt, die wichtige Prozesse im arktischen Klimasystem beschreiben und die sich auf Prozesse in der Atmosphäre konzentrieren. Die Vorgänge und Veränderungen in der Arktis sind gekoppelt mit dem globalen Klimasystem. Dabei gehen die Wirkungen in beide Richtungen. Großräumige atmosphärische Fernwirkungen, wie Arktische Oszillation (AO), Nordatlantische Oszillation (NAO) oder Pazifik-Nordamerika-Oszillation (PNA), sind Beispiele dieser Kopplungen. Diese beeinflussen die Arktis und die mittleren Breiten und werden andererseits in ihrer Ausprägung von Vorgängen in beiden Regionen beeinflusst. Große ozeanische Strömungssysteme („Conveyor Belt“) verbinden alle Weltmeere. Ein Zweig führt über den Golfstrom und den Nordatlantischen Strom bis in den Arktischen Ozean, wo die Wassermassen durch Abkühlung und Eisbildung modifiziert werden und zum großen Teil als Tiefenwasser in den Nordatlantik zurückkehren und somit zum Antrieb der thermohalinen Zirkulation (THC) beitragen. Aus der Arktis mit der transpolaren Drift durch die Framstraße treibendes Meereis beeinflusst über die Arktis hinaus den Salzgehalt und die Dichteschichtung im Nordatlantik. Abschmelzende Gletscher erhöhen den Meeresspiegel weltweit. Die Arktis ist also kein isoliertes System. Das Wechselspiel aller Komponenten des arktischen Klimasystems miteinander und mit dem globalen Klimasystem ist zu komplex und umfangreich, als dass es in einem Prometheft umfassend abgehandelt werden kann. Wir beschränken uns hier daher auf die Diskussion wichtiger Prozesse in der Atmosphäre und der Wechselwirkung zwischen der Atmosphäre und dem Meereis.
    Type of Medium: Series available for loan
    Pages: 92 Seiten , Illustrationen, Diagramme, Karten
    ISSN: 0340-4552
    Series Statement: Promet Heft 102
    Language: German
    Note: Inhalt Vorwort „Zu diesem Heft“ / B. BRÜMMER 1. Athmosphärische Bedingungen und Energiehaushalt der Arktis im Jahresgang / B. BRÜMMER 2. Regionale und globale Wechselwirkung zwischen arktischem Meereis und der atmosphärischen Zirkulation / K. DETHLOFF, A. RINKE, D. HANDORF, R. JAISER, W. DORN, A. SOMMERFELD 3. Arktische Verstärkung und Wolken / M. WENDISCH, A. EHRLICH 4. Arktische Zyklonen: Häufigkeit und Wirkung auf das Meereis / B. BRÜMMER 5. Polare Kaltluftausbrüche / M. GRYSCHKA 6. Arktische Polynjen / S. WILLMES, G. HEINEMANN, A. PREUSSER 7. Turbulente Energie- und Impulsflüsse in der atmosphärischen Grenzschicht über dem polaren Ozean / C. LÜPKES, A. SCHMITT, V. GRYANIK 8 Der katabatische Wind über Grönland / G. HEINEMANN Buchbesprechung Examina im Jahr 2017
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  • 44
    Monograph available for loan
    Monograph available for loan
    Cham : Springer
    Call number: AWI P9-20-93591
    Description / Table of Contents: This book focuses in detail on all ecologically important aspects of the Kongsfjorden system such as the marine and atmospheric environment including long-term monitoring, Ecophysiology of individual species, structure and function of the ecosystem, ecological processes and biological communities. The contributed articles include review articles and research articles that have a wider approach and bring the current research up-to-date. This book will form a baseline for future work.
    Type of Medium: Monograph available for loan
    Pages: xiii, 562 Seiten , Illustrationen, Karten , 24 cm
    ISBN: 978-3-319-46423-7
    Series Statement: Advances in polar ecology 2
    Language: English
    Note: Contents: 1 The ecosystem of Kongsfjorden, Svalbard / Haakon Hop and Christian Wiencke Part I. Atmospheric conditions 2 The atmosphere above Ny-Ålesund : climate and global warming, ozone and surface UV radiation / Marion Maturilli, Inger Hanssen-Bauer, Roland Neuber, Markus Rex, and Kåre Edvardsen Part II. Oceanography, sea ice and underwater light regime 3 The Kongsfjorden Transect : seasonal and inter-annual variability in hydrography / Vigdis Tverberg, Ragnheid Skogseth, Finlo Cottier, Arild Sundfjord, Waldemar Walczowski, Mark E. Inall, Eva Falck, Olga Pavlova, and Frank Nilsen 4 Changes in sea-ice extent and thickness in Kongsfjorden, Svalbard (2003-2016) / Olga Pavlova, Sebastian Gerland, and Haakon Hop 5 The underwater light climate in Kongsfjorden and its ecological implications / Alexey K. Pavlov, Eva Leu, Dieter Hanelt, Inka Bartsch, Ulf Karsten, Stephen R. Hudson, Jean-Charles Gallet, Finlo Cottier, Jonathan H. Cohen, Jørgen Berge, Geir Johnsen, Marion Maturilli, Piotr Kowalczuk, Sławomir Sagan, Justyna Meler, and Mats A. Granskog Part III. Pelagic production, phytoplankton and zooplankton 6 Phytoplankton seasonal dynamics in Kongsfjorden, Svalbard and the adjacent shelf / Else N. Hegseth, Philipp Assmy, Józef M. Wiktor, Józef Wiktor Jr., Svein Kristiansen, Eva Leu, Vigdis Tverberg, Tove M. Gabrielsen, Ragnheid Skogseth, and Finlo Cottier 7 Zooplankton in Kongsfjorden (1996-2016) in relation to climate change / Haakon Hop, Anette Wold, Mikko Vihtakari, Malin Daase, Slawomir Kwasniewski, Marta Gluchowska, Silke Lischka, Friedrich Buchholz and Stig Falk-Petersen Part IV. Benthic microbes, macroalgae and fauna 8 Living on cold substrata : new insights and approaches in the study of microphytobenthos ecophysiology and ecology in Kongsfjorden / Ulf Karsten, Iris Schaub, Jana Woelfel, Duygu S. Sevilgen, Carolin Schlie, Burkhard Becker, Angela Wulff, Martin Graeve, and Heiko Wagner 9 Biodiversity of benthic macro- and microalgae from Svalbard with special focus on Kongsfjorden / Stein Fredriksen, Ulf Karsten, Inka Bartsch, Jana Woelfel, Miriam Koblowsky, Rhena Schumann, Siri Røang Moy, Robert S. Steneck, Józef M. Wiktor, Haakon Hop, and Christian Wiencke 10. Kelps and environmental changes in Kongsfjorden : Stress perception and responses / Kai Bischof, Christian Buschbaum, Stein Frederiksen, Francisco J. L. Gordillo, Sandra Heinrich, Carlos Jiménez, Cornelius Lütz, Markus Molis, Michael Y. Roleda, Max Schwanitz, and Christian Wiencke 11. Ecological drivers of and responses by Arctic benthic communities, with an emphasis on Kongsfjorden, Svalbard / Markus Molis, Frank Beuchel, Jürgen Laudien, Maria Włodarska-Kowalczuk, and Christian Buschbaum Part V. Arctic fjord ecosystem model and autonomous marine observatories. 12. Outline of an Arctic fjord ecosystem model for Kongsfjorden-Krossfjorden, Svalbard / Pedro Duarte, Jan Marcin Weslawski, and Haakon Hop 13. Autonomous marine observatories in Kongsfjorden, Svalbard / Haakon Hop, Finlo Cottier, and Jørgen Berge Part VI. Kongsfjorden as harbinger of the future Arctic 14. Kongsfjorden as harbinger of the future Arctic : knowns, unknowns and research priorities / Kai Bischof, Peter Convey, Pedro Duarte, Jean-Pierre Gattuso, Maria Granberg, Haakon Hop, Clara Hoppe, Carlos Jiménez, Leonid Lisitsyn, Brezo Martinez, Michael Y. Roleda, Peter Thor, Józef M. Wiktor, and Geir Wing Gabrielsen
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  • 45
    Series available for loan
    Series available for loan
    Akureyri : International Arctic Science Committee
    Associated volumes
    Call number: AWI P5-19-92711
    In: IASC ... bulletin, 2019
    Type of Medium: Series available for loan
    Pages: 78 Seiten , Illustrationen
    ISBN: 978-9935-24-531-1
    ISSN: 1654-7594
    Series Statement: IASC Bulletin 2019
    Language: English
    Note: CONTENTS PREFACE 1 IASC Internal Development IASC Organization IASC Council IASC Executive Committee Secretariat ISIRA IASC Medal 2019 2 IASC Working Groups Cross-cutting Activities Launching of MOSAiC, an IASC Flagship Initiative Atmosphere Working Group (AWG) Cryosphere Working Group (CWG) Marine Working Group (MWG) Social and Human Working Group (SHWG) Terrestrial Working Group (TWG) 3 Arctic Science Summit Week 2018 POLAR2018: Where the Poles Come Together Upcoming ASSWs 4 Data and Observations#Arctic Data Committee (ADC) Sustaining Arctic Observing Networks (SAON) 5 Capacity Building IASC Fellowship Program Fellows’ Voices Overview of Supported Early Career Scientists
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  • 46
    Call number: AWI G5-17-90632
    In: Developments in paleoenvironmental research, 20
    Description / Table of Contents: The aim of this edited volume is to introduce the scientific community to paleoenvironmental studies of estuaries, to highlight the types of information that can be obtained from such studies, and to promote the use of paleoenvironmental studies in estuarine management. Readers will learn about the the application of different paleoecological approaches used in estuaries that develop our understanding of their response to natural and human influences. Particular attention is given to the essential steps required for undertaking a paleoecological study, in particular with regard to site selection, core extraction and chronological techniques, followed by the range of indicators that can be used. A series of case studies are discussed in the book to demonstrate how paleoecological studies can be used to address key questions, and to sustainably manage these important coastal environments in the future. This book will appeal to professional scientists interested in estuarine studies and/or paleoenvironmental research, as well as estuarine managers who are interested in the incorporation of paleoenvironmental research into their management programs.
    Type of Medium: Monograph available for loan
    Pages: ix, 700 Seiten , Illustrationen
    ISBN: 978-94-024-0988-8
    Series Statement: Developments in paleoenvironmental research 20
    Language: English
    Note: Contents: 1 Introduction to the Application of Paleoecological Techniques in Estuaries / Kathryn H. Taffs, Krystyna M. Saunders, Kaarina Weckström, Peter A. Gell, and C. Gregory Skilbeck. - PART I ESTARIES AND THEIR MANAGEMENT. - 2 Estuary Form and Function: Implications for Palaeoecological Studies / Peter Scanes, Angus Ferguson, and Jaimie Potts. - 3 Geology and Sedimentary History of Modern Estuaries / C. Gregory Skilbeck, Andrew D. Heap, and Colin D. Woodroffe. - 4 Paleoecological Evidence for Variability and Change in Estuaries: Insights for Management / Krystyna M. Saunders and Peter A. Gell. - PART II CORING AND DATING OF ESTUARINE SEDIMENTS. - 5 Sediment Sampling in Estuaries: Site Selection and Sampling Techniques / C. Gregory Skilbeck, Stacey Trevathan-Tackett, Pemika Apichanangkool, and Peter I. Macreadie. - 6 Some Practical Considerations Regarding the Application of 210Pb and 137Cs Dating to Estuarine Sediments / Thorbjoern Joest Andersen. - 7 Radiocarbon Dating in Estuarine Environments / Jesper Olsen, Philippa Ascough, Bryan C. Lougheed, and Peter Rasmussen. - PART III TECHNIQUES FOR PALAEOENVIRONMENTAL RECONSTRUCTIONS IN ESTUARINES. - 8 Lipid Biomarkers as Organic Geochemical Proxies for the Paleoenvironmental Reconstruction of Estuarine Environments / John K. Volkman and Rienk H. Smittenberg. - 9 C/N ratios and Carbon Isotope Composition of Organic Matter in Estuarine Environments / Melanie J. Leng and Jonathan P. Lewis. - 10 Physical and Chemical Factors to Consider when Studying Historical Contamination and Pollution in Estuaries / Amanda Reichelt-Brushett, Malcolm Clark, and Gavin Birch. - 11 Diatoms as Indicators of Environmental Change in Estuaries / Kathryn H. Taffs, Krystyna M. Saunders, and Brendan Logan. - 12 Dinoflagellate Cysts as Proxies for Holocene Environmental Change in Estuaries: Diversity, Abundance and Morphology / Marianne Ellegaard, Barrie Dale, Kenneth N. Mertens, Vera Pospelova, and Sofia Ribeiro. - 13 Applications of Foraminifera, Testate Amoebae and Tintinnids in Estuarine Palaeoecology / Anupam Ghosh and Helena L. Filipsson. - 14 Ostracods as Recorders of Palaeoenvironmental Change in Estuaries / Jessica M. Reeves. - 15 Application of Molluscan Analyses to the Reconstruction of Past Environmental Conditions in Estuaries / G. Lynn Wingard and Donna Surge. - 16 Corals in Estuarine Environments: Their Response to Environmental Changes and Application in Reconstructing Past Environmental Variability / Francisca Staines-Urías. - 17 Inferring Environmental Change in Estuaries from Plant Macrofossils / John Tibby and Carl D. Sayer. - 18 Applications of Pollen Analysis in Estuarine Systems / Joanna C. Ellison. - PART IV CASE STUDIES. - 19 Palaeo-Environmental Approaches to Reconstructing Sea Level Changes in Estuaries / Brigid V. Morrison and Joanna C. Ellison. - 20 Paleoecology Studies in Chesapeake Bay: A Model System for Understanding Interactions between Climate, Anthropogenic Activities and the Environment / Elizabeth A. Canuel, Grace S. Brush, Thomas M. Cronin, Rowan Lockwood, and Andrew R. Zimmerman. - 21 Paleosalinity Changes in the Río de la Plata Estuary and on the Adjacent Uruguayan Continental Shelf over the Past 1200 Years: An Approach Using Diatoms as a Proxy / Laura Perez, Felipe García-Rodríguez, and Till J.J. Hanebuth. - 22 Application of Paleoecology to Ecosystem Restoration: A Case Study from South Florida’s Estuaries / G. Lynn Wingard. - 23 Paleolimnological History of the Coorong: Identifying the Natural Ecological Character of a Ramsar Wetland in Crisis / Peter A. Gell. - 24 Palaeoenvironmental History of the Baltic Sea: One of the Largest Brackish-water Ecosystems in the World / Kaarina Weckström, Jonathan P. Lewis, Elinor Andrén, Marianne Ellegaard, Peter Rasmussen, and Richard Telford. - Glossary. - Index
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  • 47
    Monograph available for loan
    Monograph available for loan
    Frankfurt am Main : Fachmedien Recht und Wirtschaft ; dfv Mediengruppe
    Associated volumes
    Call number: AWI S5-16-90229
    In: Heidelberger Musterverträge ; 79
    Type of Medium: Monograph available for loan
    Pages: 29 Seiten , 21 cm x 14.8 cm
    Edition: 4., aktualisierte Auflage 2016
    ISBN: 9783800543496 , 978-3-8005-4349-6
    Series Statement: Heidelberger Musterverträge Heft 79
    Language: German
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  • 48
    Call number: AWI Bio-17-90819
    Description / Table of Contents: The authors completed collecting and arranging plates of photomicrographs for common pollen and spores in Quaternary strata. Given China's vast territory, complex vegetation types, a variety of plants, and polen grains with similar morphology probably produced by different plant species in different regions. We have organized this book's photomicrographs of pollen grains and spores in the division of China into five regions, i.e. northwest,northern, southeast, south and southwest China. Photomicrographs of pollen grains and spores in each region are arranged by plant classification system i.e. in order of algae, bryophyte, pteridophyte, gymnosperm, and angiosperm. All 409 plates of color photomicrographs for pollen grains and spores are finally illustrated and described.
    Description / Table of Contents: 本书整理编排了我国第四纪地层常见的孢粉类型显微照相图版,按照西北、北方、东南、华南和西南五个大区编排,并对这些区域的现代植被、第四纪植被史做了简要概述,还重点叙述了各地区第四纪主要孢粉类型、特点以及常见孢粉种类的鉴定形态特征。共分三章,第一章为我国各地区现代植被和第四纪植被概述,重点叙述了古植被与古气候的演变历史;第二章介绍本图鉴中所列出的各地区主要第四纪孢粉类型及其特点,并对不同地区常见孢粉种类
    Type of Medium: Monograph available for loan
    Pages: 620 Seiten , zahlreiche Illustrationen
    ISBN: 9787030505682
    Language: Chinese , Latin
    Note: Contents: Preface. - Chapter 1: Overview of modern and Quaternary vegetation in China. - 1.1 Northwest region / Tang Lingyu and Shen Caiming. - 1.1.1 Overview of modern vegetation. - 1.1.1.1 Gobi desert and desert vegetation in eastern Xinjiang. - 1.1.1.2 Extremely arid desert and shrubland vegetation in the Qaidam Basin. - 1.1.1.3 Arid desert shrub and semi-shrub vegetation in the Hexi Corridor. - 1.1.1.4 Sylvosteppe or pine-oak forest in the transitional region between semi-humid and semi-arid monsoonal climate of temperate zone in the Loess Plateau. - 1.1.2 Overview of Quaternary vegetation. - 1.1.2.1 Vegetation and environment since the early Pleistocene in Qinghai. - 1.1.2.2 Holocene vegetation succession of steppe/meadow in north Xizang (Tibet). - 1.1.2.3 Vegetation and environment since the late Pleistocene in the Loess Plateau. - 1.1.2.4 Vegetation and environment since the early Pleistocene in Xinjiang. - 1.2 Northern region / Tang Lingyu and Li Chunhai. - 1.2.1 Overview of modern vegetation. - 1.2.1.1 Coniferous and broadleaved forest and meadow of temperate zone in Northeast China. - 1.2.1.2 Oak forest of river valley, Chinese pine forest, and shrub steppe in the lower valley of Liaohe River, North China plain, southern Shanxi, and central Shaanxi plain. - 1.2.2 Overview of Quaternary vegetation. - 1.2.2.1 Vegetation and environment since the early Pleistocene in North China. - 1.2.2.2 Vegetation and environment since the early Pleistocene in Northeast China. - 1.3 Southeast region / Shu Junwu and Tang Lingyu. - 1.3.1 Overview of modern vegetation. - 1.3.2 Overview of Quaternary vegetation. - 1.3.2.1 Vegetation succession since the mid-Pleistocene in Hubei. - 1.3.2.2 Vegetation and environment since the late Pleistocene in the lower valley of the Yangtze River. - 1.3 .2.3 Forest succession since the last glaciation in southeast coast of Fujian. - 1.3.2.4 Vegetation and environment since the late Pleistocene in the central Taiwan. - 1.4 South region / Mao Limi, Tang Lingyu and Shen Cairning. - 1.4.1 Overview of modern vegetation. - 1.4.1.1 Vegetation in the southern zone of middle subtropical evergreen broadleaved forest. - 1.4.1.2 Vegetation in the zone of south subtropical evergreen broadleaved forest. - 1.4.1.3 Tropical semi-evergreen monsoonal forest and tropical monsoonal forest. - 1.4.2 Overview of Quaternary vegetation. - 1.4.2.1 Vegetation in the Zhujiang delta and Chaozhou plain since the Pleistocene recorded by pollen and spores. - 1.4.2.2 Vegetation and climate since the late Pleistocene in Leizhou Peninsula and Holocene vegetation and climate in Hainan Island. - 1.4.2.3 Late Quaternary pollen and spores, vegetation and climate records in the South. - 1.4.2.4 Vegetation and climate since the late Pleistocene in Hong Kong. - 1.5 Southwest region / Shu Junwu, Tang Lingyu and Shen Caiming. - 1.5.1 Overview of modern vegetation. - 1.5.1.1 Vegetation of evergreen broadleaved forest in the Yunnan , Guizhou and western Sichuan Plateau. - 1.5.1.2 Vegetation of coniferous forest in southeast Xizang. - 1.5.2 Overview of Quaternary vegetation. - 1.5.2.1 Holocene vegetation in northwest Yunnan. - 1.5.2.2 Vegetation and monsoonal climate history since the late Pleistocene in western and south-central Yunnan. - 1.5.2.3 Holocene vegetation in western Sichuan. - 1.5.2.4 Vegetation and environment since the late Pleistocene in Guizhou. - 1.5.2.5 Vegetation and monsoonal climate history since the late Pleistocene in southeastern Xizang. - Chapter 2 Main types of Quaternary pollen and spores and their characteristics in different regions of China. - 2.1 Northwest region / Tang Lingyu and Mao Limi. - 2.1.1 Types of Quaternary pollen and spores in Northwest China. - 2.1.2 Identifiable features of major Quaternary pollen and spores in Northwest China. - 2.1.2.1 Identifiable features of main Compositae pollen types. - 2.1.2.2 Identifiable features of Artemisia, Tamarix, and Zygophyllum pollen. - 2.1.2.3 Identifiable features of Rhamnus, Hippophae, and Elaeagnus pollen. - 2.1.3 Descriptions of morphological features for major Quaternary spores and pollen in Northwest China. - 2.1.3.1 Photomicrographs for major Quaternary pollen types in Northwest China. - 2.1.3.2 Descriptions of morphological features for major Quaternary pollen types in Northwest China. - 2.2 Northern region / Tang Lingyu. - 2.2.1 Types of Quaternary pollen and spores in Northern China. - 2.2.2 Identifiable features of major Quaternary pollen and spores in Northern China. - 2.2.2.1 Identification keys of pollen morphology for several saccate genera of Pinaceae. - 2.2.2.2 Identifiable features of pollen morphology for genera of Betulaceae. - 2.2.2.3 Identifiable features of tricolpate pollen from Salix and Cruciferae. - 2.2.2.4 Identifiable features of tricolpate pollen from Ranunculaceae and Labiatae. - 2.2.3 Descriptions of morphological features for major Quaternary spores and pollen in Northern China. - 2.2.3.1 Photomicrographs for major Quaternary pollen types in Northern China. - 2.2.3.2 Descriptions of morphological features for major Quaternary pollen types in Northern China. - 2.3 Southeast region / Tang Lingyu and Shu Junwu. - 2.3.1 Types of Quaternary pollen and spores in Southeast China. - 2.3.2 Identifiable features of major Quaternary pollen and spores in Southeast China. - 2.3.2.1 Identifiable features of pollen morphology for Fagaceae. - 2.3.2.2 Identification keys of pollen morphology for several genera of Fagaceae. - 2.3.2.3 Identifiable features of pollen morphology for several genera of Fagaceae. - 2.3.2.4 Identifiable features of pollen morphology for several genera of tropical and subtropical. - 2.3.3 Descriptions of morphological features for major Quaternary pollen and spores in Southeast China. - 2.3.3.1 Photomicrographs for major Quaternary pollen types in Southeast China. - 2.3.3.2 Descriptions of morphological features for major Quaternary pollen types in Southeast China. - 2.4 South region / Mao Limi and Tang Lingyu. - 2.4.1 Types of Quaternary pollen and spores in South China. - 2.4.2 Identifiable features of main Quaternary pollen and spores in South China. - 2.4.2.1 Modern distribution and paleophytogeography of Sonneratia and its identifiable features of pollen morphology. - 2.4.2.2 Modern distribution and paleoecology significance of Rhizophoraceae and its identifiable features of pollen morphology. - 2.4.3 Photomicrographs and descriptions of morphological features for major Quaternary pollen and spores in South China. - 2.4.3.1 Photomicrographs for major Quaternary pollen and spores in South China. - 2.4.3.2 Descriptions of morphological features for major Quaternary pollen and spores in South China. - 2.5 Southwest region / Tang Lingyu and Shu Junwu. - 2.5.1 Types of Quaternary pollen and spores in Southwest China. - 2.5.2 Identifiable feature of main Quaternary pollen and spores in Southwest China. - 2.5.2.1 Plant distribution and pollen features of Pinaceae in Southwest China. - 2.5.2.2 Identification keys of pollen morphology for Pinaceae. - 2.5.3 Descriptions of morphological features for major Quaternary pollen and spores in Southwest China. - 2.5.3.1 Photomicrographs for common pollen in Southwest China. - 2.5.3.2 Descriptions of morphological features for major Quaternary pollen and spores in Southwest China. - Chapter 3 Plates and descriptions of Quaternary pollen and spores in different region of China. - 3.1 Northwest region / Tang Lingyu and Mao Limi. - Spores of the pteridophyte Plates 1-3. - Gymnosperm pollen Plates 3-10. - Angiosperm pollen Plates 11-63. - 3.2 Northern region / Tang Lingyu and Li Chunhai. - Spores of the algae Plates 1-3. - Spores of the bryophyte Plate 4. - Spores of the pteridophyte Plates 5-9. - Gymnosperm pollen Plates 9-24. - Angiosperm pollen Plates 25-63. - 3.3 Southeast region / Tang Lingyu, Zhou Zhongze and
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  • 49
    Series available for loan
    Series available for loan
    Hamburg : maribus gGmbH
    Associated volumes
    Call number: AWI G2-17-91188
    In: World ocean review, 5
    Type of Medium: Series available for loan
    Pages: 207 Seiten , Illustrationen, graphische Darstellungen
    ISBN: 978-3-86648-274-6
    Series Statement: World ocean review 5
    Language: German
    Note: Inhalt: Vorwort. - 1. Die Dynamik der Küsten. - Vom Werden und Vergehen der Küsten. - Die vielen Gesichter der Küsten. - Conclusio: Die Gestalt unserer Küsten – eine lange und wechselvolle Geschichte. - 2. Mit den Küsten leben. - Die Leistung der Küsten. - Küsten unter Druck. - Conclusio: Immense Leistung, immenser Druck 3. Bedrohung durch Klimawandel und Naturgefahren. - Der Klimawandel und die Küsten. - Vom Kampf gegen Naturgefahren. - Conclusio: Klimawandel und Naturgefahren bedrohen die Küsten. - 4. Küsten besser schützen. - Die Kunst, Küsten zu verwalten. - Dem Meeresspiegelanstieg begegnen. - Conclusio: Gemeinsam für eine schonende Nutzung und einen besseren Schutz. - Gesamt-Conclusio. - Glossar. - Abkürzungen. - Quellenverzeichnis. - Abbildungsverzeichnis. - Index. - Mitwirkende. - Partner und Danksagung. - Impressum.
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  • 50
    Call number: AWI P10-17-91055
    Type of Medium: Monograph available for loan
    Pages: 164 S. , Ill., graph. Darst., Kt.
    Language: German
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  • 51
    Monograph available for loan
    Monograph available for loan
    Köln : Carl Heymanns Verlag
    Call number: AWI S5-18-91862
    Type of Medium: Monograph available for loan
    Pages: XXV, 2377 Seiten , 19 cm
    Edition: 5. Auflage
    ISBN: 9783452287168
    Series Statement: Heymanns Taschenkommentare zum gewerblichen Rechtsschutz
    Uniform Title: Gemeinschaftsmarkenverordnung
    Former Title: 1.-4. Auflage unter dem Titel: Gemeinschaftsmarkenverordnung
    Language: German
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  • 52
    Monograph available for loan
    Monograph available for loan
    Bremerhaven : Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
    Call number: AWI A4-19-92164
    Type of Medium: Monograph available for loan
    Pages: 86 Seiten , Illustrationen, Diagramme, Karten
    Edition: Redaktioneller Stand Januar 2018
    Series Statement: Im Fokus / Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
    Language: German
    Note: INHALT: EDITORIAL. - Auf den Spuren des Wandels: Forschung an den Brennpunkten unseres Planeten. - SCHWERPUNKTTHEMA. - Hotspot Arktis – wenn das Eis verschwindet. - OZEANOGRAPHIE. - E-Mails vom Filchner-Schelfeis. - MEEREISVORHERSAGE. - Wenn zwei sich „streiten“. - KLIMAMODELLIERUNG. - Stets die richtige Maschenweite. - HYDROAKUSTIK. - Der Sound des Ozeans. - OZEANOGRAPHIE. - Der Wärme-Pulsschlag des Nordatlantiks. - OZEANOGRAPHIE. - Wohin wandert der Rieseneisberg vom Larsen C-Schelfeis?. - ATMOSPHÄRENFORSCHUNG. - Per Anhalter in die Arktis. - KLIMAMODELLIERUNG. - Die Stärken des Rechnens. - FERNERKUNDUNG. - Die Lücken im Blick. - ATMOSPHÄRENFORSCHUNG. - Die Ozon-Story. - MEEREISPHYSIK. - Messungen aus der Vogelperspektive. - FORSCHUNGSVERBUND. - Den Klimawandel vor der Haustür verstehen. - INFOGRAFIK. - Einblicke in das Klima der Vergangenheit. - MEERESSPIEGELANSTIEG. - Eis weg - Land unter!. - IMPRESSUM.
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  • 53
    Monograph available for loan
    Monograph available for loan
    København : Gyldendal
    Call number: AWI P8-18-91728
    Type of Medium: Monograph available for loan
    Pages: 230 Seiten , Illustrationen, Karten , 30 x 31 cm
    Edition: First edition, first print
    ISBN: 978-87-02-20964-8
    Language: German
    Note: Contents: Introduction. - A changing climate. - The emerging land. - The frozen past. - From ice to sea. - Plant adaptation. - Land of contrasts. - Sheep farming - now and in the future. - Methane in the Arctic. , Parallel texts in Danish and English
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  • 54
    Monograph available for loan
    Monograph available for loan
    Berlin : Springer
    Associated volumes
    Call number: AWI S4-18-91822
    In: Texts in computational science and engineering, 6
    Type of Medium: Monograph available for loan
    Pages: XXXI, 922Seiten , Illustrationen, graphische Darstellungen
    Edition: Fifth edition
    ISBN: 9783662498873 , 9783662498866
    Series Statement: Texts in computational science and engineering 6
    Language: English
    Note: Contents: 1 Computing with Formulas. - 1.1 The First Programming Encounter: a Formula. - 1.1.1 Using a Program as a Calculator. - 1.1.2 About Programs and Programming. - 1.1.3 Tools for Writing Programs. - 1.1.4 Writing and Running Your First Python Program. - 1.1.5 Warning About Typing Program Text. - 1.1.6 Verifying the Result. - 1.1.7 Using Variables. - 1.1.8 Names of Variables. - 1.1.9 Reserved Words in Python. - 1.1.10 Comments. - 1.1.11 Formatting Text and Numbers. - 1.2 Computer Science Glossary. - 1.3 Another Formula: Celsius-Fahrenheit Conversion. - 1.3.1 Potential Error: Integer Division. - 1.3.2 Objects in Python. - 1.3.3 Avoiding Integer Division. - 1.3.4 Arithmetic Operators and Precedence. - 1.4 Evaluating Standard Mathematical Functions. - 1.4.1 Example: Using the Square Root Function. - 1.4.2 Example: Computing with sinh x. - 1.4.3 A First Glimpse of Rounding Errors. - 1.5 Interactive Computing. - 1.5.1 Using the Python Shell. - 1.5.2 Type Conversion. - 1.5.3 IPython. - 1.6 Complex Numbers. - 1.6.1 Complex Arithmetics in Python. - 1.6.2 Complex Functions in Python. - 1.6.3 Unified Treatment of Complex and Real Functions. - 1.7 Symbolic Computing. - 1.7.1 Basic Differentiation and Integration. - 1.7.2 Equation Solving. - 1.7.3 Taylor Series and More. - 1.8 Summary. - 1.8.1 Chapter Topics. - 1.8.2 Example: Trajectory of a Ball. - 1.8.3 About Typesetting Conventions in This Book. - 1.9 Exercises. - 2 Loops and Lists. - 2.1 While Loops. - 2.1.1 A Naive Solution. - 2.1.2 While Loops. - 2.1.3 Boolean Expressions. - 2.1.4 Loop Implementation of a Sum. - 2.2 Lists. - 2.2.1 Basic List Operations. - 2.2.2 For Loops. - 2.3 Alternative Implementations with Lists and Loops. - 2.3.1 While Loop Implementation of a for Loop. - 2.3.2 The Range Construction. - 2.3.3 For Loops with List Indices. - 2.3.4 Changing List Elements. - 2.3.5 List Comprehension. - 2.3.6 Traversing Multiple Lists Simultaneously. - 2.4 Nested Lists. - 2.4.1 A table as a List of Rows or Columns. - 2.4.2 Printing Objects. - 2.4.3 Extracting Sublists. - 2.4.4 Traversing Nested Lists. - 2.5 Tuples. - 2.6 Summary. - 2.6.1 Chapter Topics. - 2.6.2 Example: Analyzing List Data. - 2.6.3 How to Find More Python Information. - 2.7 Exercises. - 3 Functions and Branching. - 3.1 Functions. - 3.1.1 Mathematical Functions as Python Functions. - 3.1.2 Understanding the Program Flow. - 3.1.3 Local and Global Variables. - 3.1.4 Multiple Arguments. - 3.1.5 Function Argument or Global Variable?. - 3.1.6 Beyond Mathematical Functions. - 3.1.7 Multiple Return Values. - 3.1.8 Computing Sums. - 3.1.9 Functions with No Return Values. - 3.1.10 Keyword Arguments. - 3.1.11 Doc Strings. - 3.1.12 Functions as Arguments to Functions. - 3.1.13 The Main Program. - 3.1.14 Lambda Functions. - 3.2 Branching. - 3.2.1 If-else Blocks. - 3.2.2 Inline if Tests. - 3.3 Mixing Loops, Branching, and Functions in Bioinformatics Examples. - 3.3.1 Counting Letters in DNA Strings. - 3.3.2 Efficiency Assessment. - 3.3.3 Verifying the Implementations. - 3.4 Summary. - 3.4.1 Chapter Topics. - 3.4.2 Example: Numerical Integration. - 3.5 Exercises. - 4 User Input and Error Handling. - 4.1 Asking Questions and Reading Answers. - 4.1.1 Reading Keyboard Input. - 4.2 Reading from the Command Line. - 4.2.1 Providing Input on the Command Line. - 4.2.2 A Variable Number of Command-Line Arguments. - 4.2.3 More on Command-Line Arguments. - 4.3 Turning User Text into Live Objects. - 4.3.1 The Magic Eval Function. - 4.3.2 The Magic Exec Function. - 4.3.3 Turning String Expressions into Functions. - 4.4 Option-Value Pairs on the Command Line. - 4.4.1 Basic Usage of the Argparse Module. - 4.4.2 Mathematical Expressions as Values. - 4.5 Reading Data from File. - 4.5.1 Reading a File Line by Line. - 4.5.2 Alternative Ways of Reading a File. - 4.5.3 Reading a Mixture of Text and Numbers. - 4.6 Writing Data to File. - 4.6.1 Example: Writing a Table to File. - 4.6.2 Standard Input and Output as File Objects. - 4.6.3 What is a File, Really?. - 4.7 Handling Errors. - 4.7.1 Exception Handling. - 4.7.2 Raising Exceptions. - 4.8 A Glimpse of Graphical User Interfaces. - 4.9 Making Modules. - 4.9.1 Example: Interest on Bank Deposits. - 4.9.2 Collecting Functions in a Module File. - 4.9.3 Test Block. - 4.9.4 Verification of the Module Code. - 4.9.5 Getting Input Data. - 4.9.6 Doc Strings in Modules. - 4.9.7 Using Modules. - 4.9.8 Distributing Modules. - 4.9.9 Making Software Available on the Internet. - 4.10 Making Code for Python 2 and 3. - 4.10.1 Basic Differences Between Python 2 and 3. - 4.10.2 Turning Python 2 Code into Python 3 Code. - 4.11 Summary. - 4.11.1 Chapter Topics. - 4.11.2 Example: Bisection Root Finding. - 4.12 Exercises. - 5 Array Computing and Curve Plotting. - 5.1 Vectors. - 5.1.1 The Vector Concept. - 5.1.2 Mathematical Operations on Vectors. - 5.1.3 Vector Arithmetics and Vector Functions. - 5.2 Arrays in Python Programs. - 5.2.1 Using Lists for Collecting Function Data. - 5.2.2 Basics of Numerical Python Arrays. - 5.2.3 Computing Coordinates and Function Values. - 5.2.4 Vectorization. - 5.3 Curve Plotting. - 5.3.1 MATLAB-Style Plotting with Matplotlib. - 5.3.2 Matplotlib; Pyplot Prefix. - 5.3.3 SciTools and Easyviz. - 5.3.4 Making Animations. - 5.3.5 Making Videos. - 5.3.6 Curve Plots in Pure Text. - 5.4 Plotting Difficulties. - 5.4.1 Piecewisely Defined Functions. - 5.4.2 Rapidly Varying Functions. - 5.5 More Advanced Vectorization of Functions. - 5.5.1 Vectorization of StringFunction Objects. - 5.5.2 Vectorization of the Heaviside Function. - 5.5.3 Vectorization of a Hat Function. - 5.6 More on Numerical Python Arrays. - 5.6.1 Copying Arrays. - 5.6.2 In-Place Arithmetics. - 5.6.3 Allocating Arrays. - 5.6.4 Generalized Indexing. - 5.6.5 Testing for the Array Type. - 5.6.6 Compact Syntax for Array Generation. - 5.6.7 Shape Manipulation. - 5.7 High-Performance Computing with Arrays. - 5.7.1 Scalar Implementation. - 5.7.2 Vectorized Implementation. - 5.7.3 Memory-Saving Implementation. - 5.7.4 Analysis of Memory Usage. - 5.7.5 Analysis of the CPU Time. - 5.8 Higher-Dimensional Arrays. - 5.8.1 Matrices and Arrays. - 5.8.2 Two-Dimensional Numerical Python Arrays. - 5.8.3 Array Computing. - 5.8.4 Matrix Objects. - 5.9 Some Common Linear Algebra Operations. - 5.9.1 Inverse, Determinant, and Eigenvalues. - 5.9.2 Products. - 5.9.3 Norms. - 5.9.4 Sum and Extreme Values. - 5.9.5 Indexing. - 5.9.6 Transpose and Upper/Lower Triangular Parts. - 5.9.7 Solving Linear Systems. - 5.9.8 Matrix Row and Column Operations. - 5.9.9 Computing the Rank of a Matrix. - 5.9.10 Symbolic Linear Algebra. - 5.10 Plotting of Scalar and Vector Fields. - 5.10.1 Installation. - 5.10.2 Surface Plots. - 5.10.3 Parameterized Curve. - 5.10.4 Contour Lines. - 5.10.5 The Gradient Vector Field. - 5.11 Matplotlib. - 5.11.1 Surface Plots. - 5.11.2 Contour Plots. - 5.11.3 Vector Field Plots. - 5.12 Mayavi. - 5.12.1 Surface Plots. - 5.12.2 Contour Plots. - 5.12.3 Vector Field Plots. - 5.12.4 A 3D Scalar Field and Its Gradient Field. - 5.12.5 Animations. - 5.13 Summary. - 5.13.1 Chapter Topics. - 5.13.2 Example: Animating a Function. - 5.14 Exercises. - 6 Dictionaries and Strings. - 6.1 Dictionaries. - 6.1.1 Making Dictionaries. - 6.1.2 Dictionary Operations. - 6.1.3 Example: Polynomials as Dictionaries. - 6.1.4 Dictionaries with Default Values and Ordering. - 6.1.5 Example: Storing File Data in Dictionaries. - 6.1.6 Example: Storing File Data in Nested Dictionaries. - 6.1.7 Example: Reading and Plotting Data Recorded at Specific Dates. - 6.2 Strings. - 6.2.1 Common Operations on Strings. - 6.2.2 Example: Reading Pairs of Numbers. - 6.2.3 Example: Reading Coordinates. - 6.3 Reading Data fromWeb Pages. - 6.3.1 About Web Pages. - 6.3.2 How to Access Web Pages
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  • 55
    Monograph available for loan
    Monograph available for loan
    Bremerhaven : Alfred Wegener Institute, Helmholtz-Centre for Polar and Marine Research
    Call number: AWI A4-19-92165
    Type of Medium: Monograph available for loan
    Pages: 86 Seiten , Illustrationen, Diagramme, Karten
    Edition: January 2018
    Series Statement: Im Fokus / Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung
    Language: German
    Note: TABLE OF CONTENTS: EDITORIAL. - Tracking Changes: research at our planet’s hotspots. - FOCUS TOPIC. - Hotspot Arktic - when the ice disappears. - OCEANOGRAPHY. - E-mails from the Filchner Ice Shelf. - SEA-ICE FORECASTING. - Great minds don’t always think alike. - CLIMATE MODELLING. - Always the right scale. - HYDROACOUSTICS. - The Music of the Ocean. - OCEANOGRAPHY. - The Pulse of Heat in the North Atlantic. - OCEANOGRAPHY. - Where is the giant iceberg from the Larsen C Ice Shelf heading?. - ATMOSPHERIC RESEARCH. - Hitchhiking across the arctic. - CLIMATE MODELLING. - The benefits of model. - REMOTE SENSING. - Minding the gaps. - ATMOSPHERIC RESEARCH. - The Ozone Story. - SEA-ICE PHYSICS. - A bird’s eye view of the ice. - RESEARCH NETWORK INITIATIVE. - Understanding the climate change on your own doorstep. - INFOGRAPHIC. - Decoding the Earth ́s climate history. - SEA LEVEL RISE. - Melting ice flooded shores. - MASTHEAD.
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  • 56
    Call number: AWI G8-19-92586
    Description / Table of Contents: Arctic warming has implications for the functioning of terrestrial Arctic ecosystems, global climate and socioeconomic systems of northern communities. A research gap exists in high spatial resolution monitoring and understanding of the seasonality of permafrost degradation, spring snowmelt and vegetation phenology. This thesis explores the diversity and utility of dense TerraSAR-X (TSX) X-Band time series for monitoring ice-rich riverbank erosion, snowmelt, and phenology of Arctic vegetation at long-term study sites in the central Lena Delta, Russia and on Qikiqtaruk (Herschel Island), Canada. In the thesis the following three research questions are addressed: • Is TSX time series capable of monitoring the dynamics of rapid permafrost degradation in ice-rich permafrost on an intra-seasonal scale and can these datasets in combination with climate data identify the climatic drivers of permafrost degradation? • Can multi-pass and multi-polarized TSX time series adequately monitor seasonal snow cover and snowmelt in small Arctic catchments and how does it perform compared to optical satellite data and field-based measurements? • Do TSX time series reflect the phenology of Arctic vegetation and how does the recorded signal compare to in-situ greenness data from RGB time-lapse camera data and vegetation height from field surveys? To answer the research questions three years of TSX backscatter data from 2013 to 2015 for the Lena Delta study site and from 2015 to 2017 for the Qikiqtaruk study site were used in quantitative and qualitative analysis complimentary with optical satellite data and in-situ time-lapse imagery. The dynamics of intra-seasonal ice-rich riverbank erosion in the central Lena Delta, Russia were quantified using TSX backscatter data at 2.4 m spatial resolution in HH polarization and validated with 0.5 m spatial resolution optical satellite data and field-based time-lapse camera data. Cliff top lines were automatically extracted from TSX intensity images using threshold-based segmentation and vectorization and combined in a geoinformation system with manually digitized cliff top lines from the optical satellite data and rates of erosion extracted from time-lapse cameras. The results suggest that the cliff top eroded at a constant rate throughout the entire erosional season. Linear mixed models confirmed that erosion was coupled with air temperature and precipitation at an annual scale, seasonal fluctuations did not influence 22-day erosion rates. The results highlight the potential of HH polarized X-Band backscatter data for high temporal resolution monitoring of rapid permafrost degradation. The distinct signature of wet snow in backscatter intensity images of TSX data was exploited to generate wet snow cover extent (SCE) maps on Qikiqtaruk at high temporal resolution. TSX SCE showed high similarity to Landsat 8-derived SCE when using cross-polarized VH data. Fractional snow cover (FSC) time series were extracted from TSX and optical SCE and compared to FSC estimations from in-situ time-lapse imagery. The TSX products showed strong agreement with the in-situ data and significantly improved the temporal resolution compared to the Landsat 8 time series. The final combined FSC time series revealed two topography-dependent snowmelt patterns that corresponded to in-situ measurements. Additionally TSX was able to detect snow patches longer in the season than Landsat 8, underlining the advantage of TSX for detection of old snow. The TSX-derived snow information provided valuable insights into snowmelt dynamics on Qikiqtaruk previously not available. The sensitivity of TSX to vegetation structure associated with phenological changes was explored on Qikiqtaruk. Backscatter and coherence time series were compared to greenness data extracted from in-situ digital time-lapse cameras and detailed vegetation parameters on 30 areas of interest. Supporting previous results, vegetation height corresponded to backscatter intensity in co-polarized HH/VV at an incidence angle of 31°. The dry, tall shrub dominated ecological class showed increasing backscatter with increasing greenness when using the cross polarized VH/HH channel at 32° incidence angle. This is likely driven by volume scattering of emerging and expanding leaves. Ecological classes with more prostrate vegetation and higher bare ground contributions showed decreasing backscatter trends over the growing season in the co-polarized VV/HH channels likely a result of surface drying instead of a vegetation structure signal. The results from shrub dominated areas are promising and provide a complementary data source for high temporal monitoring of vegetation phenology. Overall this thesis demonstrates that dense time series of TSX with optical remote sensing and in-situ time-lapse data are complementary and can be used to monitor rapid and seasonal processes in Arctic landscapes at high spatial and temporal resolution.
    Type of Medium: Dissertations
    Pages: XIII, 131 Seiten , Illustrationen
    Language: Undetermined
    Note: Dissertation, Universität Potsdam, 2019 , TABLE OF CONTENTS Abstract Zusammenfassung Table of contents List of figures List of tables List of abbreviations 1 Introduction 1.1 Scientific background and motivation 1.1.1 Permafrost degradation 1.1.2 Snow cover 1.1.3 Vegetation phenology 1.2 Remote sensing of rapid changes 1.2.1 SAR remote sensing 1.2.2 TerraSar-X 1.3 Data and methods 1.4 Aims and objectives 1.5 Study areas and data 1.6 Thesis structure and author contributions 1.6.1 Chapter 2 – Monitoring inter-and intra-seasonal dynamics of rapidly degrading ice-rich permafrost riverbanks in the Lena Delta with TerraSAR-X time series 1.6.2 Chapter 3 – TerraSAR-X time series fill a gap in spaceborne snowmelt monitoring of small Arctic catchments 1.6.3 Chapter 4 – Estimation of Arctic tundra vegetation phenology with TerraSAR-X 2 Monitoring inter-and intra-seasonal dynamics of rapidly degrading ice-rich permafrost riverbanks in the Lena Delta with TerraSAR-X time series 2.1 Abstract 2.2 Introduction 2.3 Study area 2.4 Data and methods 2.4.1 SAR data and processing 2.4.2 Automated cliff-top line extraction from SAR data 2.4.3 Quantification of cliff-top erosion with the Digital Shoreline Analysis System 2.4.4 Cliff top mapping from optical satellite data 2.4.5 In-situ observations of cliff top erosion 2.4.6 Climate data 2.4.7 Statistical data analysis 2.5 Results 2.5.1 TSX erosion versus in-situ and optical datasets 2.5.2 Inter-and intra-annual cliff-top erosion and climate data 2.5.3 Backscatter time series 2.6 Discussion 2.6.1 Inter-annual dynamics of cliff-top erosion 2.6.2 Intra-annual dynamics of cliff-top erosion 2.6.3 Backscatter dynamics of tundra and cliff surfaces 2.7 Conclusions 2.8 Acknowledgments 3 TerraSAR-X time series fill a gap in spaceborne snowmelt monitoring of small Arctic catchments 3.1 Abstract 3.2 Introduction 3.3 Study area 3.4 Data and methods 3.4.1 SAR satellite data 3.4.2 Optical satellite data 3.4.3 In-situ time-lapse camera data 3.4.4 Snow Cover Extent from TerraSAR-X 3.4.5 Snow Cover Extent from Landsat 8 3.4.6 Accuracy assessment of TerraSAR-X Snow Cover Extent 3.4.7 Fractional Snow Cover time series analysis 3.5 Results 3.5.1 Evaluation of TSX Snow Cover Extent 3.5.2 Time series of Fractional Snow Cover in all catchments 3.5.3 Time series of Fractional SnowCover in small catchments 3.6 Discussion 3.6.1 Spatiotemporal monitoring of snowmelt dynamics using TSX 3.6.2 Technical considerations for using TSX for wet snow detection 3.7 Conclusions 3.8 Acknowledgements 3.9 Appendix 4 Relationships between X-Band SAR and vegetation phenology in a low Arctic ecosystem 4.1 Abstract 4.2 Introduction 4.3 Study area 4.4 Data and methods 4.4.1 In-situ time-lapse phenological cameras 4.4.2 Time-lapse image analysis 4.4.3 SAR satellite data 4.4.4 Backscatter and coherence time series 4.4.5 In-situ vegetation and climate data 4.5 Results 4.5.1 Phenocams 4.5.2 Backscatter dynamics 4.5.3 Coherence dynamics 4.6 Climate data 4.7 Backscatter and vegetation height 4.8 Discussion 4.9 Conclusion 4.10 Acknowledgments 5 Synthesis 5.1 Rapid permafrost disturbance 5.2 Snowmelt dynamics 5.3 Arctic tundra vegetation phenology 5.4 Seasonality and complementarity of TSX 5.5 Limitations and technical considerations 5.6 Key findings and outlook References Acknowledgements
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  • 57
    Call number: AWI G6-19-92461
    Type of Medium: Dissertations
    Pages: XVI, 203 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2019 , Table of contents Abstract Zusammenfassung Abbreviations 1 Introduction 1.1 Scientific background 1.1.1 Permafrost in the Northern Hemisphere 1.1.2 The permafrost carbon climate feedback 1.1.3 Rapidly changing, deep permafrost environments 1.2 Aims of this dissertation 1.3 Investigated study areas 1.4 Basic method overview 1.4.1 Field work in the Arctic 1.4.2 Laboratory procedure 1.4.3 Analysis ofl andscape-scale carbon and nitrogen stocks 1.5 Thesis organization 1.6 Overview of publications 1.6.1 Publication#1 - Yedoma landscape publication 1.6.2 Publication#2 - Thermokarst lake sequence publication 1.6.3 Publication#3 - North Alaska Arctic river delta publication 1.6.4 Extended Abstract - Western Alaska river delta study 1.6.5 Appendices - Supplementary material and paper in preparation II Carbon and nitrogen pools in thermokarst-affected permafrost landscapes in Arctic Siberia 2.1 Abstract 2.2 Introduction 2.3 Material and methods 2.3.1 Study area 2.3.2 Field Work 2.3.3 Laboratory analysis 2.3.4 Landform classification and upscaling C and N pools 2.4 Results 2.4.1 Sedimentological results 2.4.2 Sampling site SOC and N stocks 2.4.3 Upscaling: Landscape SOC and N stocks 2.4.4 Radiocarbon dates 2.5 Discussion 2.5.1 Site specific soil organic C and N stock characteristics 2.5.2 Upscaling of C and N pools 2.5.3 Sediment and organic C accumulation rates 2.5.4 Characterizing soil organic carbon 2.5.5 The fate of organic carbon in thermokarst-affected yedoma in Siberia 2.6 Conclusions III Impacts of successive thermokarst lake stages on soil organic matter, Arctic Alaska 3.1 Abstract 3.2 Plain language summary 3.3 Introduction 3.4 Study site 3.5 Methods 3.5.1 Core collection 3.5.2 Biogeochemical analyses 3.5.3 Study area OC and N calculation 3.6 Results 3.6.1 Biogeochemistry 3.6.2 Sediment organic carbon and nitrogen stocks 3.6.3 Radiocarbon dates and carbon accumulation rates 3.6.4 Landscape C and N budget 3.7 Discussion 3.7.1 Impact of thermokarst lake dynamics on organic matter storage 3.7.2 High organic C and N stocks on the ACP 3.7.3 Landscape chronology 3.7.4 Organic matter accumulation 3.7.5 Future development 3.8 Conclusions IV Sedimentary and geochemical characteristics of two small permafrost-dominated Arctic river deltas in northern Alaska 4.1 Abstract 4.2 Introduction 4.3 Study area 4.4 Material and Methods 4.4.1 Soil organic carbon and soil nitrogen storage 4.4.2 Radiocarbon dating and organic carbon accumulation rates 4.4.3 Grain size distribution 4.4.4 Scaling carbon and nitrogen contents to landscape level 4.5 Results 4.5.1 Carbon and nitrogen contents 4.5.2 Radiocarbon dates and accumulation rates 4.5.3 Grain size distribution 4.5.4 Arctic river delta carbon and nitrogen storage 4.6. Discussion 4.6.1 Significance of carbon and nitrogen stocks in Arctic river deltas 4.6.2 SOC and SN distribution with depth 4.6.3 Sedimentary characteristics 4.6.3.1 Accumulation rates 4.6.3.2 Sediment distribution 4.6.4 Impacts of future changes 4.6.5 Significance of remotely sensed upscaling results 4.7 Conclusions V Soil carbon and nitrogen stocks in Arctic river deltas - New data for three Western Alaskan deltas 5.1 Abstract 5.2 Introduction 5.3 Study sites 5.4 Methods 5.5 Results and discussion 5.5 Conclusions VI Discussion 6.1 Interregional comparison 6.2 Changing thermokarst landscapes and their global impact 6.3 A growing C and N data base 6.4 Outlook - potential follow-up projects VII Synthesis VIII References Appendix A Synthesis of SOC and N inventories Appendix B Supplementary material to Chapter II Appendix C Supplementary material to Chapter III Appendix D Supplementary material to Chapter IV Appendix E Supplementary material to Chapter V Appendix F Arctic river delta data set - Version 1.0 Acknowledgements - Danksagung
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  • 58
    Monograph available for loan
    Monograph available for loan
    [Roskilde] : DCE - Danish Centre for Environment and Energy, Aarhus University
    Call number: AWI P5-19-92578
    Type of Medium: Monograph available for loan
    Pages: 148 Seiten , Illustrationen
    Edition: First edition
    ISBN: 978-87-93129-13-9
    Language: English
    Note: CONTENTS ABOUT THE AUTHORS PREFACE FROM THE ASSOCIATION OF POLAR EARLY CAREER SCIENTISTS PREFACE FROM THE INTERACT STATION MANAGERS’ FORUM ABOUT INTERACT ABOUT APECS INTERACT STATIONS INTRODUCTION 1. Getting started – Outlining your field project 1.1 Scientific rationale and objectives 1.2 Methods and data requirements 1.3 What scientific equipment will you need? 1.4 Study site(s) 1.5 Risk assessment 1.5.1 Risk identification 1.5.2 Risk assessment 1.5.3 Risk mitigation 1.5.4 Contingency plans 1.6 Time schedules 1.6.1 Logistical organisation 1.6.2 Fieldwork activities 1.7 Project budget 1.8 Data and sample management 1.8.1 Data management plan 1.8.2 Sample labelling 1.8.3 Field instrumentation 1.9 Environmental compliance 1.10 Output Chapter resources 2. Further planning – Practicalities and legal issues 2.1 Applying for access to the station 2.2 Transport to the station and conditions for visiting 2.2.1 Access to the station 2.2.2 Conditions for visiting 2.3 Visas and permits required by national authorities 2.3.1 Visas 2.3.2 Permits 2.4 Working with local communities 2.5 Equipment transport 2.6 Checklists and equipment 2.6.1 Checklists 2.6.2 Personal clothing 2.7 Import and export regulations 2.7.1 Import and export permits 2.7.2 Transporting hazardous goods 2.7.3 Handling cooled and frozen materials 2.8 Insurance 2.9 Check-ups and chronical illness 2.10 Training activities 2.11 Financial and other administrative issues 2.12 Final checks before leaving Chapter resources 3. Safety 3.1 General safety guidelines 3.2 Safety barriers 3.2.1 Knowledge, experience, and skills 3.2.2 Attitude and culture 3.2.3 Judgement and leadership 3.2.4 Trip plan 3.3 Education and training 3.4 Health and first aid 3.4.1 Medicine and chronic illness 3.4.2 First aid 3.5 Transport 3.5.1 Aircraft 3.5.2 Boats 3.5.3 Snowmobiles 3.5.4 Vehicles (Automobiles and ATV’s) 3.6 Risks at the station 3.6.1 Fire 3.6.2 In the kitchen 3.6.3 Electricity 3.6.4 Hygiene 3.6.5 Laboratory work and chemicals 3.6.6 Workshops and equipment use 3.7 Risks in the field and at the camp 3.7.1 Field camps 3.7.2 Cooking and water treatment 3.7.3 Firearms 3.7.4 Extreme activities 3.8 Natural hazards 3.8.1 Weather change 3.8.2 Glacier fieldwork 3.8.3 Snow avalanches and cornice falls 3.8.4 Steep terrain: Rock avalanches, rock falls, and mud slides 3.8.5 Sea-ice or frozen lakes and rivers 3.8.6 River crossings 3.8.7 Wildlife 3.9 Means of communication 3.9.1 Fieldwork plans and sign in/out boards 3.9.2 Routine calls 3.9.3 Non-routine calls 3.9.4 Emergency calls 3.10 Safety equipment 3.10.1 Communication equipment 3.10.2 Navigation equipment 3.10.3 Clothing 3.10.4 Field camp equipment 3.10.5 Specific safety equipment 3.11 Emergency preparedness Chapter resources 4. Arrival at the station and your time in the field 4.1 Getting to know your team 4.2 Arrival at the station 4.3 Working at field sites 4.4 In case something does not go according to plan 4.4.1 Handling delays 4.4.2 Handling conflicts 4.4.3 Harassment and discrimination 4.5 Environmental considerations 4.5.1 Pollution prevention 4.5.2 Waste management 4.5.3 Reducing energy use 4.5.4 Respect protected areas, fauna, and flora 4.6 Working with local communities 4.7 Communication with the outside world 4.8 Leaving the field Chapter resources 5. After fieldwork 5.1 Reporting to the station, funders, and local communities 5.2 Data preservation, backup, and submission APPENDICES Appendix A: Checklists Appendix B: Equipment lists Appendix C: Health risks
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  • 59
    Monograph available for loan
    Monograph available for loan
    Hoboken, NJ : Wiley
    Call number: AWI A14-15-0008
    Description / Table of Contents: The cryosphere, that region of the world where water is temporarily or permanently frozen, plays a crucial role on our planet. Recent developments in remote sensing techniques, and the acquisition of new data sets, have resulted in significant advances in our understanding of all components of the cryosphere and its processes. This book, based on contributions from 40 leading experts, offers a comprehensive and authoritative overview of the methods, techniques and recent advances in applications of remote sensing of the cryosphere. Examples of the topics covered include: snow extent, depth, grain size and impurities; surface and subsurface melting; glaciers; accumulation over the Greenland and Antarctica ice sheets; ice thickness and velocities; gravimetric measurements from space; sea, lake and river ice; frozen ground and permafrost; fieldwork activities; recent and future cryosphere-oriented missions and experiments.
    Type of Medium: Monograph available for loan
    Pages: 408 Seiten , Illustrationen
    Edition: 1. edition
    ISBN: 9781118368855
    Series Statement: The cryosphere science series
    Language: English
    Note: Table of Contents: List of contributors. - Cryosphere Science: Series Preface. - Preface. - Acknowledgments. - About the companion website. - 1 Remote sensing and the cryosphere. - 1.1 Introduction. - 1.2 Remote sensing. - 1.2.1 The electromagnetic spectrum and blackbody radiation. - 1.2.2 Passive systems. - 1.2.3 Active systems. - 1.3 The cryosphere. - References. - 2 Electromagnetic properties of components of the cryosphere. - 2.1 Electromagnetic properties of snow. - 2.1.1 Visible/near-infrared and thermal infrared. - 2.1.2 Microwave region. - 2.2 Electromagnetic properties of sea ice. - 2.2.1 Visible/near-infrared and thermal infrared. - 2.2.2 Microwave region. - 2.3 Electromagnetic properties of freshwater ice. - 2.4 Electromagnetic properties of glaciers and ice sheets. - 2.4.1 Visible/near-infrared and thermal infrared. - 2.4.2 Microwave region. - 2.5 Electromagnetic properties of frozen soil. - 2.5.1 Visible/near-infrared and thermal infrared. - 2.5.2 Microwave region. - References. - Acronyms. - Websites cited. - 3 Remote sensing of snow extent. - 3.1 lntroduction. - 3.2 Visible/near-infrared snow products. - 3.2.1 The normalized difference snow index (NDSI). - 3.3 Passive microwave products. - 3.4 Blended VNIR/PM products. - 3.5 Satellite snow extent as input to hydrological models. - 3.6 Concluding remarks. - Acknowledgments. - References. - Acronyms. - Websites cited. - 4 Remote sensing of snow albedo, grain size, and pollution from space. - 4.1 Introduction. - 4.2 Forward modeling. - 4.3 Local optical properties of a snow layer. - 4.4 Inverse problem. - 4.5 Pitfalls of retrievals. - 4.6 Conclusions. - Acknowledgments. - References. - Acronyms. - Websites cited. - 5 Remote sensing of snow depth and snow water equivalent. - 5.1 Introduction. - 5.2 Photogrammetry. - 5.3 LiDAR. - 5.4 Gamma radiation. - 5.5 Gravity data. - 5.6 Passive microwave data. - 5.7 Active microwave data. - 5.8 Conclusions. - References. - Acronyms. - Websites cited. - 6 Remote sensing of melting snow and ice. - 6.1 Introduction. - 6.2 General considerations on optical/thermal and microwave sensors and techniques for remote sensing of melting. - 6.2.1 Optical and thermal sensors. - 6.2.2 Microwave sensors. - 6.2.3 Electromagnetic properties of dry and wet snow. - 6.3 Remote sensing of melting over land. - 6.4 Remote sensing of melting over Greenland. - 6.4.1 Thermal infrared sensors. - 6.4.2 Microwave sensors. - 6.5 Remote sensing of melting over Antarctica. - 6.6 Conclusions. - References. - Acronyms. - 7 Remote sensing of glaciers. - 7.1 Introduction. - 7.2 Fundamentals. - 7.3 Satellite instruments for glacier research. - 7.4 Methods. - 7.4.1 Image classification for glacier mapping. - 7.4.2 Mapping debris-covered glaciers. - 7.4.3 Glacier mapping with SAR data. - 7.4.4 Assessing glacier changes. - 7.4.5 Area and length changes. - 7.4.6 Volumetrie glacier changes. - 7.4.7 Glacier velocity. - 7.5 Glaciers of the Greenland ice sheet. - 7.5.1 Surface elevation. - 7.5.2 Glacier extent. - 7.5.3 Glacier dynamics. - 7.6 Summary. - References. - Acronyms. - Websites cited. - 8 Remote sensing of accumulation over the Greenland and Antarctic ice sheets. - 8.1 Introduction to accumulation. - 8.2 Spaceborne methods for determining accumulation over ice sheets. - 8.2.1 Microwave remote sensing. - 8.2.2 Other remote sensing techniques and combined methods. - 8.3 Airborne and ground-based measurements of accumulation. - 8.3.1 Ground-based. - 8.3.2 Airborne. - 8.4 Modeling of accumulation. - 8.5 The future for remote sensing of accumulation. - 8.6 Conclusions. - References. - Acronyms. - Website cited. - 9 Remote sensing of ice thickness and surface velocity. - 9.1 Introduction. - 9.1.1 Electrical properties of glacial ice. - 9.2 Radar principles. - 9.2.1 Radar sounder. - 9.2.2 Radar equation. - 9.3 Pulse compression. - 9.4 Antennas. - 9.5 Example results. - 9.6 SAR and array processing. - 9.7 SAR Interferometry. - 9. 7.1 Introduction. - 9.7.2 Basic theory. - 9.7.3 Practical considerations of InSAR systems. - 9.7.4 Application of InSAR to Cryosphere remote sensing. - 9.8 Conclusions. - References. - Acronyms. - 10 Gravimetry measurements from space. - 10.1 Introduction. - 10.2 Observing the Earth's gravity field with inter-satellite ranging. - 10.3 Surface mass variability from GRACE. - 10.4 Results. - 10.5 Conclusions. - References. - Acronyms. - 11 Remote sensing of sea ice. - 11.1 Introduction. - 11.2 Sea ice concentration and extent. - 11.2.1 Passive microwave radiometers. - 11.2.2 Active microwave - scatterometry and radar. - 11.2.3 Visible and infrared. - 11.2.4 Operational sea ice analyses. - 11.3 Sea ice drift. - 11.4 Sea ice thickness and age, and snow depth. - 11.4.1 Altimetric thickness estimates. - 11.4.2 Radiometric thickness estimates. - 11.4.3 Sea ice age estimates as a proxy for ice thickness. - 11.5 Sea ice melt onset and freeze-up, albedo, melt pond fraction and surface temperature. - 11.5.1 Melt onset and freeze-up. - 11.5.2 Sea ice albedo and melt pond fraction. - 11.5.3 Sea ice surface temperature. - 11.6 Summary, challenges and the road ahead. - References. - Acronyms. - Website cited. - 12 Remote sensing of lake and river ice. - 12.1 Introduction. - 12.2 Remote sensing of lake ice. - 12.2.1 Ice concentration, extent and phenology. - 12.2.2 Ice types. - 12.2.3 Ice thickness and snow on ice. - 12.2.4 Snow/ice surface temperature. - 12.2.5 Floating and grounded ice: the special case of shallow Arctic/sub-Arctic lakes. - 12.3 Remote sensing of river ice. - 12.3.1 Ice extent and phenology. - 12.3.2 lce types, ice jams and flooded areas. - 12.3.3 Ice thickness. - 12.3.4 Surface flow velocities. - 12.3.5 Incorporating SAR-derived ice information into a GIS-based system in support of river-flow modeling and flood forecasting. - 12.4 Conclusions and outlook. - Acknowledgments. - References. - Acronyms. - Websites cited. - 13 Remote sensing of permafrost and frozen ground. - 13.1 Permafrost - an essential climate variable of the "Global Climate Observing System". - 13.2 Mountain permafrost. - 13.2.1 Remote sensing of surface features and permafrost landforms. - 13.2.2 Generation of digital elevation models. - 13.2.3 Terrain elevation change and displacement. - 13.3 Lowland permafrost - identification and mapping of surface features. - 13.3.1 Land cover and vegetation. - 13.3.2 Permafrost landforms. - 13.3.3 Landforms and processes indicating permafrost degradation. - 13.4 Lowland permafrost - remote sensing of physical variables related to the thermal permafrost state. - 13.4.1 Land surface temperature through thermal remote sensing. - 13.4.2 Freeze-thaw state of the surface soil through microwave remote sensing. - 13.4.3 Permafrost mapping with airborne electromagnetic surveys. - 13.4.4 Regional surface deformation through radar interferometry. - 13.4.5 A gravimetric signal of permafrost thaw?. - 13.5 Outlook - remote sensing data and permafrost models. - References. - Acronyms. - 14 Field measurements for remote sensing of the cryosphere. - 14.1 Introduction. - 14.2 Physical properties of interest. - 14.2.1 Surface properties. - 14.2.2 Sub-surface properties. - 14.3 Standard techniques for direct measurements of physical properties. - 14.3.1 Topography. - 14.3.2 Snow depth. - 14.3.3 Snow water equivalent and density. - 14.3.4 Temperature. - 14.3.5 Stratigraphy. - 14.3.6 Sea ice depth and ice thickness. - 14.4 New techniques for high spatial resolution measurements. - 14.4.1 Topography. - 14.4.2 Surface properties. - 14.4.3 Sub-surface properties. - 14.5 Simulating airborne and spaceborne observations from the ground. - 14.5.1 Active microwave. - 14.5.2 Passive microwave. - 14.6 Sampling strategies for remote sensing field campaigns: concepts and examples. - 14.6.1 Ice sheet campaigns. - 14.6.2 Seasonal snow campaigns. - 14.6.3 Sea ice campaigns. - 14.7 Conclusions. - References. - Acronyms. - Websites cited. - 15 Remote sensing missions and the cryosphere. - 15.1 In
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  • 60
    Monograph available for loan
    Monograph available for loan
    Dordrecht : Springer
    Call number: AWI A11-15-0048
    Description / Table of Contents: This textbook aims to be a one stop shop for those interested in aerosols and their impact on the climate system. It starts with some fundamentals on atmospheric aerosols, atmospheric radiation and cloud physics, then goes into techniques used for in-situ and remote sensing measurements of aerosols, data assimilation, and discusses aerosol-radiation interactions, aersol-cloud interactions and the multiple impacts of aerosols on the climate system. The book aims to engage those interested in aerosols and their impacts on the climate system: graduate and PhD students, but also post-doctorate fellows who are new to the field or would like to broaden their knowledge. The book includes exercises at the end of most chapters. Atmospheric aerosols are small (microscopic) particles in suspension in the atmosphere, which play multiple roles in the climate system. They interact with the energy budget through scattering and absorption of solar and terrestrial radiation. They also serve as cloud condensation and ice nuclei with impacts on the formation, evolution and properties of clouds. Finally aerosols also interact with some biogeochemical cycles. Anthropogenic emissions of aerosols are responsible for a cooling effect that has masked part of the warming due to the increased greenhouse effect since pre-industrial time. Natural aerosols also respond to climate changes as shown by observations of past climates and modelling of the future climate.
    Type of Medium: Monograph available for loan
    Pages: XVII, 311 Seiten , Illustrationen
    ISBN: 9789401796484
    Uniform Title: Aérosols atmosphériques : propriétés et impacts climatiques
    Language: English
    Note: Contents: 1 General Introduction. - 1.1 The Climate System. - 1.2 The Atmosphere. - 1.3 Energy Budget and Atmospheric Composition. - 1.4 The Water Cycle. - 1.5 Aerosols and Climate Change. - 1.6 Outline of this Textbook. - References. - Further Reading (Textbooks and Articles. - 2 Atmospheric Aerosols. - 2.1 Definitions. - 2.2 Sources of Aerosols and Aerosol Precursors. - 2.2.1 Marine Aerosols. - 2.2.2 Desert Dust. - 2.2.3 Volcanic Aerosols. - 2.2.4 Biogenic Aerosols. - 2.2.5 Biomass Burning Aerosols. - 2.2.6 Aerosols from Fossil Fuel Combustion. - 2.3 Spatial and Temporal Aerosol Distributions. - 2.4 Aerosol-Cloud-Radiation Interactions. - 2.5 Climate Effects of Aerosols. - References. - Further Reading (Textbooks and Articles). - 3 Physical, Chemical and Optical Aerosol Properties. - 3.1 Fine, Accumulation and Coarse Modes. - 3.2 Size Distribution. - 3.3 Chemical Composition. - 3.3.1 Aerosol Mixture. - 3.3.2 Inorganic Aerosols. - 3.3.3 Black Carbon Aerosols. - 3.3.4 Organic Aerosols. - 3.3.5 Geographic Distribution of Aerosol Chemical Composition. - 3.4 Refractive Index. - 3.5 Deliquescence, Efflorescence and Hysteresis. - 3.6 Definition of Aerosol Optical Properties. - 3.6.1 Absorption and Scattering Cross Sections. - 3.6.2 Phase Function. - 3.6.3 Upscatter Fractions. - 3.7 Calculation of Aerosol Optical Properties. - 3.7.1 Mie Theory. - 3. 7.2 Extinction, Scattering and Absorption. - 3.7.3 Optical Depth and Angström Coefficient. - 3.8 Optical Properties of Nonspherical Aerosols. - 3.9 Aerosols and Atmospheric Visibility. - References. - Further Reading (Textbooks and Articles). - 4 Aerosol Modelling. - 4.1 Introduction. - 4.2 Emissions. - 4.2.1 Generalities. - 4.2.2 Fossil Fuels, Biofuels, and Other Anthropogenic Sources. - 4.2.3 Vegetation Fires. - 4.2.4 Sea Spray. - 4.2.5 Desert Dust. - 4.2.6 Dimethylsulphide. - 4.2.7 Biogenic Volatile Organic Compounds. - 4.2.8 Volcanoes. - 4.2.9 Resuspension. - 4.3 Atmospheric Processes. - 4.3.1 Nucleation. - 4.3.2 Condensation of Semi-Volatile Compounds. - 4.3.3 Coagulation. - 4.3.4 In-Cloud Aerosol Production. - 4.3.5 Wet Deposition. - 4.3.6 Dry Deposition. - 4.3.7 Sedimentation. - 4.3.8 Aerosol Transport. - 4.4 Modelling Approaches. - 4.4.1 Bulk Approach. - 4.4.2 Sectional Approach. - 4.4.3 Modal Approach. - 4.5 Example: The Sulphur Budget. - References. - Further Reading (Textbooks and Articles). - 5 Interactions of Radiation with Matter and Atmospheric Radiative Transfer. - 5.1 Introduction. - 5.2 Electromagnetic Radiation. - 5.2.1 Generalities. - 5.2.2 Definitions. - 5.3 Interactions of Radiation with Matter. - 5.3.1 Matter, Energy and Spectral Lines. - 5.3.2 Intensity of Spectral Lines. - 5.3.3 Spectral Line Profiles. - 5.3.4 Processes of lnteractions of Radiation with Matter. - 5.4 Modelling of the Interaction Processes. - 5.4.1 Molecular Absorption Coefficient. - 5.4.2 Scattering Phase Function. - 5.4.3 Molecular Scattering. - 5.4.4 Absorption and Scattering by Aerosols. - 5.4.5 Thermal Emission. - 5.5 Atmospheric Radiative Transfer. - 5.5.1 Equation of Radiative Transfer. - 5.5.2 Extinction Only. - 5.5.3 Scattering Medium. - 5.5.4 Plane-Parallel Atmosphere. - 5.5.5 Resolution of the Equation of Radiative Transfer. - 5.6 Absorption Bands, Energy, and Actinic Fluxes. - 5.6.1 Main Molecular Absorption Bands in the Atmosphere. - 5.6.2 Radiative Flux. - 5.6.3 Two-Flux Method. - 5.6.4 Stefan-Boltzmann Law. - 5.6.5 Radiative Budget. - 5.6.6 Actinic Fluxes. - 5.6.7 Polarization of Radiation. - References. - Further Reading (Textbooks and Articles). - 6 In Situ and Remote Sensing Measurements of Aerosols. - 6.1 Introduction to Aerosol Remote Sensing. - 6.2 Passive Remote Sensing: Measurement of the Extinction. - 6.2.1 General Principles. - 6.2.2 Ground-Based Photometry. - 6.2.3 Spaceborne Occultation Measurements. - 6.2.4 Retrieval of Aerosol Size Distribution. - 6.3 Passive Remote Sensing: Measurement of the Scattering. - 6.3.1 General Principles. - 6.3.2 Ground-Based Measurement of Scattered Radiation. - 6.3.3 Spaceborne Measurements of Scattered Radiation. - 6.4 Measurement of Infrared Radiation. - 6.4.1 General Principles. - 6.4.2 Spaceborne Nadir Measurement of Infrared Radiation. - 6.4.3 Spaceborne Limb Measurement of Infrared Radiation. - 6.5 Active Remote Sensing: Lidar. - 6.5.1 General Principles. - 6.5.2 The Lidar Equation. - 6.5.3 Raman Lidar. - 6.6 In Situ Aerosol Measurements. - 6.6.1 Measurement of Aerosol Concentrations. - 6.6.2 Measurement of Aerosol Chemical Composition. - 6.6.3 Measurement of Aerosol Scattering. - 6.6.4 Measurement of Aerosol Absorption. - 6.7 Conclusions. - References. - Further Reading (Textbooks and Articles). - 7 Aerosol Data Assimilation. - 7.1 Introduction. - 7.2 Basic Principles of Data Assimilation. - 7.3 Applications of Data Assimilation for Aerosols. - References. - Further Reading (Textbooks and Articles). - 8 Aerosol-Radiation Interactions. - 8.1 Introduction. - 8.2 Atmospheric Radiative Effects Due to Aerosols. - 8.2.1 Simplified Equation for Scattering Aerosols. - 8.2.2 Simplified Equation for Absorbing Aerosols. - 8.2.3 Radiative Transfer Calculations. - 8.2.4 Global Estimates and Sources of Uncertainty. - 8.3 Rapid Adjustments to Aerosol-Radiation Interactions. - 8.4 Radiative Impact of Aerosols on Surface Snow and Ice. - References. - Further Reading (Textbooks and Articles). - 9 Aerosol-Cloud lnteractions. - 39.1 Introduction. - 9 .1.1 Cloud Formation. - 9 .1.2 Cloud Distribution. - 9 .1.3 Aerosol-Cloud Interactions. - 9.2 Aerosol Effects on Liquid Clouds. - 9 .2.1 Saturation Pressure of Water Vapour. - 9.2.2 Kelvin Effect. - 9.2.3 Raoult's Law. - . - 9.2.4 Köhler Theory. - 9.2.5 Extensions to the Köhler Theory. - 9.2.6 CCN and Supersaturation in the Cloud. - 9.2.7 Dynamical and Radiative Effects in Clouds. - 9.2.8 Principle of the Cloud Albedo Effect. - 9.2.9 Observations of the Cloud Albedo Effect. - 9.2.10 Adjustments in Liquid Water Clouds. - 9.2.11 Rapid Adjustments Occurring in Liquid Clouds. - 9.3 Aerosols Effects on Mixed-Phased and Ice Clouds. - 9.3.1 Elements of Microphysics of Ice Clouds. - 9.3.2 Impact of Anthropogenic Aerosols on Ice Clouds. - 9.4 Forcing Due to Aerosol-Cloud lnteractions. - 9.5 Aerosols, Contrails and Aviation-Induced Cloudiness. - 9.5.1 Formation of Condensation Trails. - 9.5.2 Estimate of the Climate Impact of Contrails. - References. - Further Reading (Textbooks and Articles). - 10 Climate Response to Aerosol Forcings. - 10.1 Introduction. - 10.2 Radiative Forcing, Feedbacks and Climate Response. - 10.2.1 Radiative Forcing. - 10.2.2 Climate Feedbacks. - 10.2.3 Rapid Adjustments and Effective Radiative Forcing. - 10.2.4 Climate Response and Climate Efficacy. - 10.3 Climate Response to Aerosol Forcings. - 10.3.1 Equilibrium Response. - 10.3.2 Past Emissions. - 10.3.3 Detection and Attribution of Aerosol Impacts. - 10.3.4 Future Emissions Scenarios. - 10.4 Nuclear Winter. - References. - Further Reading (Textbooks and Articles). - 11 Biogeochemical Effects and Climate Feedbacks of Aerosols. - 11 .1 Introduction. - 11.2 Impact of Aerosols on Terrestrial Ecosystems. - 11.2.1 Diffuse Radiation and Primary Productivity. - 11.2.2 Aerosols as a Source of Nutrients. - 11.2.3 Acidification of Precipitation. - 11.3 Impact of Aerosols on Marine Ecosystems. - 11.4 Aerosols-Atmospheric Chemistry Interactions. - 11.4.1 Interactions with Tropospheric Chemistry. - 11.4.2 Impact of Stratospheric Aerosols on the Ozone Layer and Ultravialet Radiation. - 11.5 Climate Feedbacks Involving Marine Aerosols. - 11.5.1 Sulphate Aerosols from DMS Emissions. - 11.5.2 Marine Aerosols. - 11.5.3 Other Aerosols of Maritime Origin. - 11.6 Climate Feedbacks Involving Continental Aerosols. - 11.6.1 Secondary Organic Aerosols. - 11.6.2 Primary Aerosols of Biogenic Origin. - 11.6.3 Aerosols from Vegetation Fires. - 11.6.4 Desert Dust. - 11.7 Climate Feedbacks Involving Stratospheric Aerosols. - References. - Further Reading (Textbooks and Articles). - 12 Strato
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  • 61
    Monograph available for loan
    Monograph available for loan
    Tokyo : National Institute for Polar Research
    Call number: AWI P5-15-0033
    Type of Medium: Monograph available for loan
    Pages: 26 S. : Ill., graph. Darst., Kt.
    Edition: 2014, rev. March 2015
    Language: English
    Note: Contents: 1. Introduction. - (1) The purposes of the long-term plan report. - (2) The background and particulars of this report. - (3) Contents of this report. - 2.Changes in the Arctic environment to date and in the near future. - 3. History of Arctic environmental research. - 4. Abstracts of all themes. - (1) Elucidation of abrupt environmental change in the Arctic associated with the on-going global warming. - Theme 1: Arctic amplification of global warming. - Theme 2: Mechanisms and influence of sea ice decline. - Theme 3: Biogeochemical cycles and ecosystem changes. - Theme 4: Ice sheet, glaciers, permafrost, snowfall, snow cover and hydrological cycle. - Theme 5: Interactions between the Arctic and the entire earth. - Theme 6: Predicting future environmental conditions of the Arctic based on paleoenvironmental records. - Theme 7: Effects of the Arctic environment on human society. - (2) Elucidation of environmental change concerning biodiversity. - Theme 8: Effects on terrestrial ecosystems and biodiversity. - Theme 9: Influence on marine ecosystem and biodiversity. - (3) Broad and important subjects on the Arctic environment. - Theme 10: Geospace environment. - Theme 11: Interaction of surface environment change with solid earth. - Theme 12: Basic understanding on formation and transition process of permafrost. - (4) Development of methods enabling breakthroughs in environmental research. - Theme A: Sustainable seamless monitoring. - Theme B: Earth system-modeling for inter-disciplinary research. - Theme C: Data assimilation to connect monitoring and modeling. - 5. Improvement of research foundation. - Authors and reviewers.
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  • 62
    Call number: AWI P1-15-0045
    Description / Table of Contents: This document presents the Policy-makers Summary of the 2015 AMAP Assessments of Pollution Issues (POPs Trends; Radioactivity in the Arctic; Human Health in the Arctic).
    Type of Medium: Monograph available for loan
    Pages: 10 S. : Ill., graph. Darst.
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  • 63
    Monograph available for loan
    Monograph available for loan
    Cham : Springer
    Call number: AWI G6-15-89028
    Description / Table of Contents: The book offers a modern, comprehensive, and holistic view of natural gas seepage, defined as the visible or invisible flow of gaseous hydrocarbons from subsurface sources to Earth’s surface. Beginning with definitions, classifications for onshore and offshore seepage, and fundamentals on gas migration mechanisms, the book reports the latest findings for the global distribution of gas seepage and describes detection methods. Seepage implications are discussed in relation to petroleum exploration, environmental impacts (hazards, pollution, atmospheric emissions, and past climate change), emerging scientific issues (abiotic gas and methane on Mars), and the role of seeps in ancient cultures. With an updated bibliography and an integrated analysis of available data, the book offers a new fundamental awareness - gas seepage is more widespread than previously thought and influences all of Earth’s external “spheres”, including the hydrosphere, atmosphere, biosphere, and anthroposphere.
    Type of Medium: Monograph available for loan
    Pages: XIII, 199 S. , Ill., graph. Darst.
    ISBN: 978-3-319-14600-3
    Language: English
    Note: Contents: 1 Introduction. - 1.1 Basic Concepts and Definitions. - 1.1.1 What Gas Seepage Is, What It Is Not. - 1.1.2 A Jungle of Names: Seeps, Macroseeps, Microseepage, Microseeps, and Miniseepage. - 1.1.3 Seepage id est Migration. - 1.1.4 Microbial, Thermogenic, and Abiotic Methane. - 1.2 Significance of Seepage and Implications. - 1.2.1 Seepage and Petroleum Exploration. - 1.2.2 Marine Seepage on the Crest of the Wave. - 1.2.3 From Sea to Land. - 1.2.4 A New Vision. - References. - 2 Gas Seepage Classification and Global Distribution. - 2.1 Macro-Seeps. - 2.1.1 Gas Seeps. - 2.1.2 Oil Seeps. - 2.1.3 Gas-Bearing Springs. - 2.1.4 Mud Volcanoes. - 2.1.5 Miniseepage. - 2.1.6 The Global Distribution of Onshore Macro-Seeps. - 2.2 Microseepage. - 2.3 Marine Seepage Manifestations. - References. - 3 Gas Migration Mechanisms. - 3.1 Fundamentals. - 3.1.1 Sources and Pathways. - 3.1.2 Diffusion and Advection. - 3.2 Actual Mechanisms and Migration Forms. - 3.2.1 Bubble and Microbubble Flow. - 3.2.2 Gas Seepage Velocity. - 3.2.3 Matter Transport by Microbubbles. - 3.2.4 The Concept of Carrier Gas and Trace Gas. - References. - 4 Detecting and Measuring Gas Seepage. - 4.1 Gas Detection Methods. - 4.1.1 Above-Ground (Atmospheric) Measurements. - 4.1.2 Ground Measurements. - 4.1.3 Measurements in Aqueous Systems. - 4.2 Indirect Methods. - 4.2.1 Chemical-Mineralogical Alterations of Soils. - 4.2.2 Vegetation Changes (Geobotanical Anomalies). - 4.2.3 Microbiological Analyses of Soils. - 4.2.4 Radiometric Surveys. - 4.2.5 Geophysical Techniques. - References. - 5 Seepage in Field Geology and Petroleum Exploration. - 5.1 Seepage and Faults. - 5.2 Microseepage Applied to Areal Petroleum Exploration. - 5.2.1 Which Gas Can Be Measured?. - 5.2.2 Microseepage Methane Flux Measurements. - 5.3 Seep Geochemistry for Petroleum System Evaluation. - 5.3.1 Recognising Post-genetic Alterations of Gases. - 5.3.2 Assessing Gas Source Type and Maturity. - 5.3.3 The Presence of Undesirable Gases (CO2, H2S, N2). - 5.3.4 Helium in Seeps… for Connoisseurs. - References. - 6 Environmental Impact of Gas Seepage. - 6.1 Geohazards. - 6.1.1 Methane Explosiveness. - 6.1.2 The Toxicity of Hydrogen Sulphide. - 6.1.3 Mud Expulsions and the Degradation of Soil-Sediments. - 6.2 Stray Gas, Natural versus Man-Made. - 6.3 Hypoxia in Aquatic Environments. - 6.4 Gas Emissions to the Atmosphere. - 6.4.1 Methane Fluxes and the Global Atmospheric Budget. - 6.4.2 Ethane and Propane Seepage, a Forgotten Potential Source of Ozone Precursors. - 6.5 Natural Seepage and CO2 Geological Sequestration. - References. - 7 Seepage in Serpentinised Peridotites and on Mars. - 7.1 Seeps and Springs in Active Serpentinisation Systems. - 7.1.1 Where Abiotic Methane Is Seeping. - 7.1.2 How Abiotic Methane in Land-Based Serpentinisation Systems Is Formed. - 7.1.3 How to Distinguish Abiotic and Biotic Methane. - 7.1.4 Seepage to the Surface. - 7.1.5 Is Abiotic Gas Seepage Important for the Atmospheric Methane Budget?. - 7.2 Potential Methane Seepage on Mars. - 7.2.1 Looking for Methane on Mars. - 7.2.2 A Theoretical Martian Seepage. - References. - 8 Gas Seepage and Past Climate Change. - 8.1 Past Seepage Stronger than Today. - 8.2 Potential Proxies of Past Seepage. - 8.3 Methane and Quaternary Climate Change. - 8.3.1 Traditional Models: Wetlands versus Gas Hydrates. - 8.3.2 Adding Submarine Seeps. - 8.3.3 Considering Onshore and Offshore Seepage in Total. - 8.3.4 CH4 Isotope Signatures in Ice Cores. - 8.4 Longer Geological Time Scale Changes. - 8.4.1 The Concept of Sedimentary Organic Carbon Mobilization. - 8.4.2 Paleogene Changes. - References. - 9 Seeps in the Ancient World: Myths, Religions, and Social Development. - 9.1 Seeps in Mythology and Religion. - 9.2 Seeps in Social and Technological Development. - References. - Epilogue. - Index.
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  • 64
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo Politechničeskogo muzeja
    Call number: AWI E1-16-90310
    Type of Medium: Monograph available for loan
    Pages: 172, [1] Seiten , Illustrationen
    ISBN: 978-5-98962-037-1
    Language: Russian
    Note: In kyrill. Schr.
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  • 65
    Monograph available for loan
    Monograph available for loan
    Bremerhaven : Alfred-Wegener-Institut [Eigenverlag]
    Call number: AWI S6-17-90977
    Type of Medium: Monograph available for loan
    Pages: 101 Seiten , zahlreiche farbige Illustrationen , 21 x 15 cm
    Edition: 1. Auflage
    Language: German
    Note: Inhalt: Einleitung. - Meeresforschung in der deutschen Nordsee : über Tradition, Beharrlichkeit und Exzellenz. - Gezeiten : ausgewählte Ereignisse. - Themen & Texte. - Die stille Frühgeschichte der Biologischen Anstalt Helgoland : über ihre Entstehung 1892 und über die Wiederaufnahme ihrer Arbeit 1945 / Christian Salewski. - Wassereimer mit wundersamen Kleinstlebewesen : die Wiege der Meeresforschung auf Helgoland / Karen H. Wiltshire und Peter Lemke. - Lebensgemeinschaften erforschen : Karl August Möbius und die Austernbänke / Christian Buschbaum. - "Da muss man tauchen" : die Erfassung der untermeerischen Algenvegetation / Klaus Lüning. - Forschung im Wandel : von Organismen zu Ökosystemen / Maarten Boersma. - Otto Kinne : Direktor der Biologischen Anstalt Helgoland von 1962-1984 / Karen H. Wiltshire. - Ein persönlicher Rückblick : von einer kleinen Feldstation zum Wissenschaftsbetrieb / Harald Asmus und Ragnhild Asmus. - Gerhard Drebes : Experte für marines Phytoplankton / Kerstin Mölter. - Gastliche Häuser : Gestern und Heute / Gotthilf Hempel. - Die Biologische Anstalt Helgoland und ihr Anschluss an das AWI / Jörn Thiede und Rainer Paulenz. - Jubiläumsgemälde / Lionel Playford. - Zahlen & Daten / Karen H. Wiltshire und Kerstin Mölter. - Von "Alte Post" bis "Bluehouse" : Stationsgebäude im Wandel der Zeit. - Entwicklungsgrade° : eine Zeitreihe. - Prägende Persönlichkeiten. - Forschungsflotte. - Literatur. - Fotonachweise, Impressum.
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  • 66
    Call number: AWI S1-16-89841
    Description / Table of Contents: This book covers the basics of processing and spectral analysis of monovariate discrete-time signals. The approach is practical, the aim being to acquaint the reader with the indications for and drawbacks of the various methods and to highlight possible misuses. The book is rich in original ideas, visualized in new and illuminating ways, and is structured so that parts can be skipped without loss of continuity. Many examples are included, based on synthetic data and real measurements from the fields of physics, biology, medicine, macroeconomics etc., and a complete set of MATLAB exercises requiring no previous experience of programming is provided. Prior advanced mathematical skills are not needed in order to understand the contents: a good command of basic mathematical analysis is sufficient. Where more advanced mathematical tools are necessary, they are included in an Appendix and presented in an easy-to-follow way. With this book, digital signal processing leaves the domain of engineering to address the needs of scientists and scholars in traditionally less quantitative disciplines, now facing increasing amounts of data.
    Type of Medium: Monograph available for loan
    Pages: xxiv, 900 Seiten , Illustrationen
    ISBN: 978-3-319-25466-1
    Series Statement: Signals and Communication Technology
    Language: English
    Note: Contents: 1 Introduction. - 1.1 Chapter Summary. - 1.2 The Meaning of the Book’s Title. - 1.3 Historical Background. - 1.4 How to Read This Book. - 1.5 Further Reading. - References. - PART 1 BASIC THEORETICAL CONCEPTS. - 2 Discrete-Time Signals and Systems. - 2.1 Chapter Summary. - 2.2 Basic Definitions and Concepts. - 2.3 Discrete-Time Signals: Sequences. - 2.3.1 Basic Sequence Operations. - 2.3.2 Basic Sequences. - 2.3.3 Deterministic and Random Signals. - 2.4 Linear Time-Invariant (LTI) Systems. - 2.4.1 Impulse Response of an LTI System and Linear Convolution. - 2.4.2 An Example of Linear Convolution. - 2.4.3 Interconnections of LTI Systems. - 2.4.4 Effects of Stability and Causality Constraints on the Impulse Response of an LTI System. - 2.4.5 Finite (FIR) and Infinite (IIR) Impulse Response Systems. - 2.4.6 Linear Constant-Coefficient Difference Equation (LCCDE). - 2.4.7 Examples of LCCDE. - 2.4.8 The Solutions of an LCCDE. - 2.4.9 From the LCCDE to the Impulse Response: Examples. - 2.4.10 Eigenvalues and Eigenfunctions of LTI Systems. - References. - 3 Transforms of Discrete-Time Signals. - 3.1 Chapter Summary. - 3.2 z-Transform. - 3.2.1 Examples of z-Transforms and Special Cases. - 3.2.2 Rational z-Transforms. - 3.2.3 Inverse z-Transform. - 3.2.4 The z-Transform on the Unit Circle. - 3.2.5 Selected z-Transform Properties. - 3.2.6 Transfer Function of an LTI System. - 3.2.7 Output Sequence of an LTI System. - 3.2.8 Zeros and Poles: Forms for Rational Transfer Functions. - 3.2.9 Inverse System. - 3.3 Discrete-Time Fourier Transform (DTFT). - 3.3.1 An Example of DTFT Converging in the Mean-Square Sense. - 3.3.2 Line Spectra. - 3.3.3 Inverse DTFT. - 3.3.4 Selected DTFT Properties. - 3.3.5 The DTFT of a Finite-Length Causal Sequence. - 3.4 Discrete Fourier Series (DFS). - 3.4.1 Selected DFS Properties. - 3.4.2 Sampling in the Frequency Domain and Aliasing in the Time Domain. - 3.5 Discrete Fourier Transform (DFT). - 3.5.1 The Inverse DFT in Terms of the Direct DFT. - 3.5.2 Zero Padding. - 3.5.3 Selected DFT Properties. - 3.5.4 Circular Convolution Versus Linear Convolution. - 3.6 Fast Fourier Transform (FFT). - 3.7 Discrete Trigonometric Expansion. - 3.8 Appendix: Mathematical Foundations of Signal Representation. - 3.8.1 Vector Spaces. - 3.8.2 Inner Product Spaces. - 3.8.3 Bases in Vector Spaces. - 3.8.4 Signal Representation by Orthogonal Bases. - 3.8.5 Signal Representation by Standard Bases. - 3.8.6 Frames and Biorthogonal Bases. - 3.8.7 Summary and Complements. - References. - 4 Sampling of Continuous-Time Signals. - 4.1 Chapter Summary. - 4.2 Sampling Theorem. - 4.3 Reconstruction of a Continuous-Time Signal from Its Samples. - 4.4 Aliasing in the Frequency Domain and Anti-Aliasing Filter. - 4.5 The Uncertainty Principle for the Analog Fourier Transform. - 4.6 Support of a Continuous-Time Signal in the Time and Frequency Domains. - 4.7 Appendix: Analog and Digital Frequency Variables. - References. - 5 Spectral Analysis of Deterministic Discrete-Time Signals. - 5.1 Chapter Summary. - 5.2 Issues in Practical Spectral Analysis. - 5.2.1 The Effect of Windowing. - 5.2.2 The Effect of Spectral Sampling. - 5.3 Classical Windows. - 5.4 The Kaiser Window. - 5.5 Energy and Power Signals and Their Spectral Representations. - 5.6 Correlation of Deterministic Discrete-Time Signals. - 5.6.1 Correlation of Energy Signals. - 5.6.2 Correlation of Power Signals. - 5.6.3 Effect of an LTI System on Correlation Properties of Input and Output Signals. - 5.7 Wiener-Khinchin Theorem. - 5.7.1 Energy Signals and Energy Spectrum. - 5.7.2 Power Signals and Power Spectrum. - References. - PART 2 DIGITAL FILTERS. - 6 Digital Filter Properties and Filtering Implementation. - 6.1 Chapter Summary. - 6.2 Frequency-Selective Filters. - 6.3 Real-Causal-Stable-Rational (RCSR) Filters. - 6.4 Amplitude Response. - 6.5 Phase Response. - 6.5.1 Phase Discontinuities and Zero-Phase Response. - 6.5.2 Linear Phase (LP). - 6.5.3 Generalized Linear Phase (GLP). - 6.5.4 Constraints on GLP Filters. - 6.6 Digital Filtering Implementation. - 6.6.1 Direct Forms. - 6.6.2 Transposed-Direct Forms. - 6.6.3 FIR Direct and Transposed-Direct Forms. - 6.6.4 Direct and Transposed-Direct Forms for LP FIR Filters. - 6.6.5 Cascade and Parallel Forms. - 6.7 Zero-Phase Filtering. - 6.8 An Incorrect Approach to Filtering. - 6.9 Filtering After Downsampling. - 6.9.1 Theory of Downsampling. - 6.9.2 An Example of Filtering After Downsampling. - References. - 7 FIR Filter Design. - 7.1 Chapter Summary. - 7.2 Design Process. - 7.3 Specifications of Digital Filters. - 7.3.1 Constraints on the Magnitude Response. - 7.3.2 Constraints on the Phase Response. - 7.4 Selection of Filter Type: IIR or FIR?. - 7.5 FIR-Filter Design Methods and Approximation Criteria. - 7.6 Properties of GLP FIR Filters. - 7.6.1 Factorization of the Zero-Phase Response. - 7.6.2 Zeros of the Transfer Function. - 7.6.3 Another Form of the Adjustable Term. - 7.7 Equiripple FIR Filter Approximations: Minimax Design. - 7.8 Predicting the Minimum Filter Order. - 7.9 MPR Algorithm. - 7.10 Properties of Equiripple FIR Filters. - 7.11 The Minimax Method for Bandpass Filters. - References. - 8 IIR Filter Design. - 8.1 Chapter Summary. - 8.2 Design Process. - 8.3 Lowpass Analog Filters. - 8.3.1 Laplace Transform. - 8.3.2 Transfer Function and Design Parameters. - 8.4 Butterworth Filters. - 8.5 Chebyshev Filters. - 8.5.1 Chebyshev-I Filters. - 8.5.2 Chebyshev-II Filters. - 8.6 Elliptic Filters. - 8.7 Normalized and Non-normalized Filters. - 8.8 Comparison Among the Four Analog Filter Types. - 8.9 From the Analog Lowpass Filter to the Digital One. - 8.9.1 Bilinear Transformation. - 8.9.2 Design Procedure. - 8.9.3 Examples. - 8.10 Frequency Transformations. - 8.10.1 From a Lowpass to a Highpass Filter. - 8.10.2 From a Lowpass to a Bandpass Filter. - 8.10.3 From a Lowpass to a Bandstop Filter . - 8.11 Direct Design of IIR Filters. - 8.12 Appendix. - 8.12.1 Trigonometric Functions with Complex Argument. - 8.12.2 Elliptic Integrals. - 8.12.3 Jacobi Elliptic Functions. - 8.12.4 Landen-Gauss Transformation. - 8.12.5 Elliptic Rational Function. - References. - PART 3 SPECTRAL ANALYSIS. - 9 Statistical Approach to Signal Analysis. - 9.1 Chapter Summary. - 9.2 Preliminary Considerations. - 9.3 Random Variables. - 9.4 Ensemble Averages. - 9.5 Stationary Random Processes and Signals. - 9.6 Ergodicity. - 9.7 Wiener-Khinchin Theorem for Random Signals and Power Spectrum. - 9.8 Cross-Power Spectrum of Two Random Signals. - 9.9 Effect of an LTI System on a Random Signal. - 9.10 Estimation of the Averages of Ergodic Stationary Signals. - 9.10.1 General Concepts in Estimation Theory. - 9.10.2 Mean and Variance Estimation. - 9.10.3 Autocovariance Estimation. - 9.10.4 Cross-Covariance Estimation. - 9.11 Appendix: A Road Map to the Analysis of a Data Record. - References. - 10 Non-Parametric Spectral Methods. - 10.1 Chapter Summary. - 10.2 Power Spectrum Estimation. - 10.3 Periodogram. - 10.3.1 Bias. - 10.3.2 Variance. - 10.3.3 Examples. - 10.3.4 Variance Reduction by Band- and Ensemble-Averaging. - 10.4 Bartlett’s Method. - 10.5 Modified Periodogram. - 10.6 Welch’s Method. - 10.7 Blackman-Tukey Method. - 10.8 Statistical Significance of Spectral Peaks. - 10.9 MultiTaper Method. - 10.10 Estimation of the Cross-Power Spectrum of Two Random Signals. - 10.11 Use of the FFT in Power Spectrum Estimation. - 10.12 Power Spectrum Normalization. - References. - 11 Parametric Spectral Methods. - 11.1 Chapter Summary. - 11.2 Signals with Rational Spectra . - 11.3 Stochastic Models and Processes. - 11.3.1 Autoregressive-Moving Average (ARMA) Model. - 11.3.2 Autoregressive (AR) Model. - 11.3.3 Moving Average (MA) Model. - 11.3.4 How the AR and MA Modeling Approaches Are Theoretically Related. - 11.3.5 First-Order AR and MA Models: White, Red and Blue Noise. - 11.3.6 Higher-Order AR Models. - 11.4 The AR Approach to Spectral Estimation. - 11.5 AR Modeling and Linear Prediction. - 11.6
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  • 67
    Monograph available for loan
    Monograph available for loan
    New York, NY : Cambridge University Press
    Call number: AWI A6-17-90616
    Type of Medium: Monograph available for loan
    Pages: xxxiv, 432 Seiten , Illustrationen, graphische Darstellungen
    Edition: First published
    ISBN: 9781107118140
    Language: English
    Note: Contents: Lists of figures. - List of contributors. - Preface. - 1. Challenges for ice age dynamics: a dynamical systems perspective / Michel Crucifix, Guillaume Lenoir and Takahito Mitsui. - 2. Tipping points in the climate system / Peter Ditlevsen. - 3. Atmospheric teleconnection patterns / Steven B. Feldstein and Christian L. E. Franzke. - 4. Atmospheric regimes: the link between weather and the large scale circulation / David M. Straus, Franco Molteni and Susanna Corti. - 5. Low-frequency regime transitions and predictability of regimes in a barotropic model / Balu T. Nadiga and Terence J. O'Kane. - 6. Complex network techniques for climatological data analysis / Reik V. Donner, Marc Wiedermann and Jonathan F. Donges. - 7. On inference and validation of causality relations in climate teleconnections / Illia Horenko, Susanne Gerber, Terence J. O'Kane, James S. Risbey and Didier P. Monselesan. - 8. Stochastic climate theory / Georg A. Gottwald, Daan T. Crommelin and Christian L. E. Franzke. - 9. Stochastic subgrid modelling for geophysical and three-dimensional turbulence / Jorgen S. Frederiksen, Vassili Kitsios, Terence J. O'Kane and Meelis J. Zidikheri. - 10. Model error in data assimilation / John Harlim. - 11. Long-term memory in climate: detection, extreme events, and significance of trends / Armin Bunde and Josef Ludescher. - 12. Fractional stochastic models for heavy tailed, and long-range dependent, fluctuations in physical systems / Nicholas W. Watkins. - 13. Modelling spatial extremes using Max-Stable Processes / Mathieu Ribatet. - 14. Extreme value analysis in dynamical systems: two case studies / Tamás Bódai. - Index.
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  • 68
    Series available for loan
    Series available for loan
    Akureyri : International Arctic Science Committee
    Associated volumes
    Call number: AWI P5-18-91643
    In: IASC ... bulletin, 2018
    Type of Medium: Series available for loan
    Pages: 84 Seiten , Illustrationen, graphische Darstellungen, Karten
    ISBN: 978-9935-24-372-0
    ISSN: 1654-7594
    Series Statement: IASC Bulletin 2018
    Language: English
    Note: CONTENTS: PREFACE. - 1 IASC Internal Development. - IASC Organization. - IASC Council. - IASC Executive Committee. - IASC Secretariat. - ISIRA. - IASC Medal 2018. - 2 IASC Working Groups. - Cross-Cutting Activities. - Atmosphere Working Group (AWG). - Cryosphere Working Group (CWG). - Marine Working Group (MWG). - Social and Human Working Group (SHWG). - Terrestrial Working Group (TWG). - 3 Arctic Science Summit Week 2017. - Upcoming ASSWs. - 4 Data and Observations. - Arctic Data Committee (ADC). - Sustaining Arctic Observing Networks (SAON). - 5 Partnerships. - Arctic Council. - Asian Forum for Polar Sciences (AFoPS). - Association of Polar Early Career Scientists (APECS). - Circumpolar Health Research Network (CirchNet). - European Polar Board (EPB). - Forum of Arctic Research Operators (FARO). - International Arctic Social Sciences Association (IASSA). - International Association of Cryospheric Sciences (IACS). - International Council for the Exploration of the Sea (ICES). - The International Permafrost Association (IPA). - The Pacific Arctic Group (PAG). - The Scientific Committee on Antarctic Research (SCAR). - University of the Arctic (UArctic). - WCRP Climate and Cryosphere (CliC). - 6 Capacity Building. - IASC Fellowship Program. - CAFF-IASC Fellowship. - Fellows’ Voices. - Overview of Supported Early Career Scientists.
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  • 69
    Call number: AWI NBM-17-91184
    Description / Table of Contents: The Atlas content is presented by 8 large sections and 39 subsections which present characteristics of the key glaciological regions; there are also two auxiliary subsections: introductory one and the reference part that is indicator of geographical regions. The whole material is placed on the 590 pages of the Atlas. Themes and subjects of the maps are given in a system of three levels which one with corresponding number of base scales and, respectively, the territorial coverage. In addition to a possibility to look through all digital maps, any user can also see original vector layers in the format of shp. files which are saved in decimal degrees .This makes possible to project the data into any view, to design own project, to transform the data into other GIS-formats, to analyze the information together with own or other data with geographical conjunction .
    Type of Medium: Non-book medium
    Pages: 1 CD-ROM
    Language: Russian , English
    Note: In rus. und engl. Sprache , Teilw. in kyrill. Schr.
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  • 70
    Call number: AWI G3-18-91403
    In: Hamburger Beiträge zur physischen Geographie und Landschaftsökologie, Heft 23
    Type of Medium: Series available for loan
    Pages: xiv, 284 Seiten , Illustrationen, Karten
    Series Statement: Hamburger Beiträge zur physischen Geographie und Landschaftsökologie 23
    Language: German
    Note: Inhaltsverzeichnis Lyngen-Alpen und Bergland von Kåfjord und Storfjord / Karl-Dieter Meier. - Bemerkungen zur glaziären und periglaziären Landschaftsformung in den Lyngen-Alpen (Lyngen Halbinsel) und im Bergland von Kåfjord und Storfjord, Norwegisch Lappland, mit ausgewählten themenbezogenen Wanderexkursionen. - 1. Einführung. - 2. Physiogeographische Charakteristik der Lyngen-Alpen und des Berglandes von Kåfjord und Storfjord. - 2.1. Relief. - 2.2. Geologisch-tektonischer Bau, Festgesteine. - 2.3. Lockersedimente. - 2.4. Klima. - 2.5. Vegetation. - 3. Glaziäre Formung. - 3.1. Vergletscherungsgeschichte bis zur "Kleinen Eiszeit". - 3.2. Neuzeitliche Vergletscherung und aktuelle Gletscherdynamik. - 3.3. Zusammenhänge zwischen Gletscher- und Klimaschwankungen. - 4. Periglaziäre Formung. - 4.1. Permafrosterscheinungen und -indikatoren. - 4.2. Räumliche Verbreitung des Permafrostbodens. - 4.3. Periglaziäre Formen und Ablagerungen (ohne Permafrostboden). - 4.3.1. Blockfelder. - 4.3 .2. Sturzschutthalden und -kegel. - 4.3.3. Gelisolifluktionserscheinungen und -formen. - 4.3.4. Frostmusterböden. - 5. Exkursionsvorschläge zur glaziären und periglaziären Landschaftsformung. - 5.1. Anfahrt und Logistik. - 5.2. Fahrstrecken und Wanderexkursionen. - 5.2.1. Fornesdal - Rypedalsvatn (ca. 20 km). - 5.2.2. Fugldal - Fugldalsvatn (ca. 12 km). - 5.2.3. Goverdal - Sörvestbre- Rundvatn (ca. 17 km). - 5.2.4. Slettmo- Sörellendal (ca. 12 km). - 5.2.5. Steindal- Nallannjunni - Steindalsbre (ca. 15 km). - 5.2.6. Lyngsdal - Dalbotn - Vest- / Midt- / Sydbre (ca. 20 km). - 5.2.7. Koppangsdal - Koppangsbre (ca. 6 km). - 5.2.8. Tyttebaerdal - Brevatn - Stortinddalsbre (ca. 20 km). - 5.2.9. Bensnes - Trollvatn (ca. 10 km). - 5.2.10. Sörlenangsbotn - unteres Strupskarddal - Blåvatn- oberes Strupskarddal - Strupvatn - Strupbre (ca. 24 km). - 5.2.11. Veidal - Olderelvvatn - Veidalsvatn (ca. 12 km). - 5.2.12. Indre Nordmannvika - Nordmannvikdal - Nordmannviktind (See 549 m ü. Mo) - Jovnnacahca- Sannjariehppi - Gauknes - Kippeldal (ca. 23 km). - 5.2.13. Skarvdal - Kopperlia - Bievlajavri - Moldojokkadal - Bievlavarri ( ca. 22 km). - 6. Ergebnisse, Schlussfolgerungen und Ausblick. - 7. Literaturverzeichnis. - 8. Kartenverzeichnis. - 8.1. Quartärgeologische Karten. - 8.2. Karten der Festgesteine. - 8.3. Topographische Karten. - 9. Luftbildverzeichnis. , Inhaltsverzeichnis westliche Finnmarksvidda / Karl-Dieter Meier und Dietbert Thannheiser. - Eine Exkursion zur kaltklimatischen quartären Landschaftsformung auf der westlichen Finnmarksvidda, Norwegisch Lappland. - 1. Einführung. - 2. Physiogeographische Charakteristik. - 2.1. Relief und Gewässernetz. - 2.2. Geologisch-tektonischer Bau und Lockersedimente. - 2.3. Klima und Permafrostboden. - 2.4. Vegetation und Böden. - 3. Exkursion über die Finnmarksvidda-Hochfläche. - 3.1. Wissenschaftlicher Hintergrund. - 3.2. Streckenverlauf und Logistik. - 3.3. Streckenbeschreibung. - 3.3.1. Alta - Skillemo. - 3.3.2. Skillemo - Gargia - Beskades - Solovorni. - 3.3.3. Skillemo - Trangdalen - Avzejavri - Solovorni (Alternativstrecke). - 3.3.4. Solovorni - Masi. - 3.3.5. Masi - Gievdneguoika. - 3.3.6. Gievdneguoika - Kautokeino. - 3.3.7. Kautokeino - Avze - Kivijärvi. - 4. Schlussfolgerungen. - 5. Literatur. - 6. Geologische und geomorphologische Karten. - 7. Topographische Karten.
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  • 71
    Monograph available for loan
    Monograph available for loan
    Boca Raton : CRC Press
    Call number: AWI G7-17-91080
    Type of Medium: Monograph available for loan
    Pages: xliv, 382 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9781482234404
    Language: English
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  • 72
    Monograph available for loan
    Monograph available for loan
    Chichester, UK : John Wiley & Sons
    Call number: AWI A4-18-91479
    Type of Medium: Monograph available for loan
    Pages: xii, 652 Seiten , Illustrationen, graphische Darstellungen, Karten
    Edition: Third edition
    ISBN: 1118778383 (print) , 9781118778388 (print) , 1118778375 (print) , 9781118778371 (print) , 1118778359 (print) , 9781118778357 (print)
    Language: English
    Note: Contents: List of contributors. - Preface. - 1 Overview of sea ice growth and properties / Chris Petrich & Hajo Eicken. - 2 Sea ice thickness distribution / Christian Haas. - 3 Snow in the sea-ice system : friend or foe? / Matthew Sturm & Robert A. Massom. - 4 Sea ice and sunlight / Donald K. Perovich. - 5 The sea ice-ocean boundary layer / Miles G. McPhee. - 6 The atmosphere over sea ice / Ola Persson & Timo Vihma. - 7 Sea ice and arctic ocean oceanography / Finlo Cottier, Mike Steele & Frank Nielsen. - 8 Oceanography and sea ice in the southern ocean / Michael P. Meredith & Mark A. Brandon. - 9 Methods of satellite remote sensing of sea ice / Gunnar Spreen & Stefan Kern. - 10 Gaining (and losing) antarctic sea ice : variability, trends and mechanisms / Sharon Stammerjohn & Ted Maksym. - 11 Losing arctic sea ice : observations of the recent decline and the long-term context / Walt N. Meier. - 12 Sea ice in earth system models / Dirk Notz & Cecilia M. Bitz. - 13 Sea ice as a habitat for bacteria, archaea and viruses / Jody W. Deming & R. Eric Collins. - 14 Sea ice as a habitat for primary producers / Kevin R. Arrigo. - 15 Sea ice as a habitat for micrograzers / David A. Caron, Rebecca J. Gast & Marie-Eve Garneau. - 16 Sea ice as a habitat for macrograzers / Bodil A. Bluhm, Kerrie M. Swadling & Rolf Gradinger. - 17 Nutrients, dissolved organic matter and exopolymers in sea ice / Klaus M. Meiners & Christine Michel. - 18 Gases in sea ice / Jean-Louis Tison, Bruno Delille & Stathys Papadimitriou. - 19 Transport and transformation of contaminants in sea ice / Feiyue Wang, Monika Pucko & Gary Stern. - 20 Numerical models of sea ice biogeochemistry / Martin Vancoppenolla & Letizia Tedesco. - 21 Arctic marine mammals and sea ice / Kristin L. Laidre & Eric V. Regehr. - 22 Antarctic marine mammals and sea ice / Marthán N. Bester, Horst Bornemann & Trevor McIntyre. - 23 A feathered perspective : the influence of sea ice on arctic marine birds / Nina J. Karnovsky & Maria V. Gavrilo. - 24 Birds and antarctic sea ice / David Ainley, Eric J. Woehler & Amelie Lescroel. - 25 Sea ice is our beautiful garden : indigenous perspectives on sea ice of sea ice in the arctic / Henry P. Huntington, Shari Gearheard, Lene Kielsen Holm, George Noongwook, Margaret Opie & Joelie Sanguya. - 26 Advances in palaeo sea-ice estimation / Leanne Armand, Alexander Ferry & Amy Leventer. - 27 Ice in subarctic seas / Hermanni Kaartokallio, Mats A. Granskog, Harri Kuosa & Jouni Vainio. - Index.
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  • 73
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : IASC
    Call number: AWI P5-19-92257
    Type of Medium: Monograph available for loan
    Pages: 6 Seiten , Illustrationen
    Language: English
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  • 74
    Monograph available for loan
    Monograph available for loan
    [Santiago de Compostela] : Grupo de Investigación "Ciencia do Sistema Terra"
    Call number: AWI G3-19-92358
    Type of Medium: Monograph available for loan
    Pages: 117 Seiten , Illustrationen
    ISBN: 978-84-606-9215-7
    Series Statement: Monografías del Grupo de Investigación "Ciencia do Sistema Terra (GI-1553)-USC" 2
    Language: Spanish
    Note: Índice Presentación Observaciones geomorfológicas sobre icings y ampollas de hielo en Reindalen (78°N), Nordenskjold Land, Svalbard Nuevas evidencias de la existencia de permafrost en Tierra del Fuego (Argentina): régimen térmico del glaciar rocoso activo del Cerro Krund Surface NMR survey on Hansbreen glacier, Hornsund, SW Spitzberg (Norway) Permafrost y anomalias geotermicas en isla Decepcion (Antartida). Primeros resultados del área del abanico aluvial del Monte Irizar Glacial, periglacial and eolian landforms in the Cerro Campanario (the Andes, 35°S) , In spanischer und englischer Sprache , Zusammenfassungen in spanischer und englischer Sprache
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  • 75
    Monograph available for loan
    Monograph available for loan
    Bremerhaven : Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research
    Call number: AWI G2-19-92755
    Type of Medium: Monograph available for loan
    Pages: 48 Seiten , Illustrationen
    Language: English
    Note: Contents Preface Introduction Helgoland - Treasure trove of species Sylt - Changing tidal flats in a world heritage site Polar Regions - key areas for climate processes Plankton à la carte Plankton and the "extra portion" Forwards, but backwards into the past North Sea in the fast lane of change Vibrios like it hot Detective work in the microcosm Melting glaciers and turbid waters Thawing permafrost comes alive Arctic coasts in retreat A stroll through the underwater forest Mathematical evaluation of the tidal flat menu Let's dive in! Research scientists pay a visit Marine research goes on TV Meeting public needs: Advice and support
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  • 76
    Call number: AWI Bio-19-92601
    Description / Table of Contents: Taxonomy plays a central role in biological sciences. It provides a communication system for scientists as it aims to enable correct identification of the studied organisms. As a consequence, species descriptions should seek to include as much available information as possible at species level to follow an integrative concept of ‘taxonomics’. Here, we describe the cryptic species Epimeria frankei sp. nov. from the North Sea, and also redescribe its sister species, Epimeria cornigera. The morphological information obtained is substantiated by DNA barcodes and complete nuclear 18S rRNA gene sequences. In addition, we provide, for the first time, full mitochondrial genome data as part of a metazoan species description for a holotype, as well as the neotype. This study represents the first successful implementation of the recently proposed concept of taxonomics, using data from high-throughput technologies for integrative taxonomic studies, allowing the highest level of confidence for both biodiversity and ecological research.
    Type of Medium: Series available for loan
    Pages: 26 Seiten , Illustrationen
    ISSN: 2045-2322
    Series Statement: Scientific Reports / Springer Nature 8, 6893
    Language: English
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  • 77
    Call number: ZSP-168-716
    In: Berichte zur Polar- und Meeresforschung, 716
    Type of Medium: Series available for loan
    Pages: 211 Seiten , Illustrationen
    ISSN: 1866-3192
    Series Statement: Berichte zur Polar- und Meeresforschung 716
    Language: English
    Note: Contents Characterization of soil organic matter of Arctic and Antarctic by 13- C NMR and electron spin resonance spectroscopy / Evgeny Abakumov Development of phosphorus forms in soil chronosequence of the Nordenskioldbreen glacier (Svalbard) / Adel Allaberdina, Václav Tejnecký Vertical snow structures from in-situ and remote sensing measurements / Stefanie Arndt, Nicolas Stoll, Stephan Paul, Christian Haas Phenology of Calanus glacialis – comparison between Arctic and Atlantic domains and its implications for reproductive success of little auks / Kaja Balazy, Emilia Trudnowska, Katarzyna Blachowiak-Samolyk Response of southern tundra ecosystem components on aerial pollution from gas pre-treatment centers in West Siberia / Pavel A. Barsukov Soil-ecological excursions to permafrost-affected areas in West Siberia for European scientists and students / Pavel A. Barsukov, S. Platonova, S. Gizhitskaya, E. Smolentseva, N. Lashchinskiy, A. Babenko, I. Lyubechanskiy, O. Saprykin, O.Rusalimova Christian Siewert Freezing and hungry? Hydrocarbon degrading microbial communities in Barents Sea sediments around Svalbard / Bartholomäus Sven, Nontje Straaten, Daniela Zoch, Martin Krüger Biological soil crust algae in the polar regions – biodiversity, genetic diversity and ecosystem resilience under global change scenarios / Burkhard Becker, Burkhard Büdel and Ulf Karsten UDASH - Unified Database for Arctic and Subarctic Hydrography / Axel Behrendt, Hiroshi Sumata, Benjamin Rabe, Torsten Kanzow and Ursula Schauer Compound-specific radiocarbon constraints on Antarctic sediment chronologies / Sonja Berg, Sandra Jivcov, Janet Rethemeyer Environmental conditions in terrestrial East Antarctica during the last glacial - new evidence from mumiyo deposits / Sonja Berg, Martin Melles, Wolf-Dieter Hermichen, Janet Rethemeyer, Gerhard Kuhn Collection-based diatom research: collection imaging to biogeography and microevolution in the Southern Ocean / Bánk Beszteri, Stefan Pinkernell, Michael Kloster, Ute Postel, Gerhard Kauer, Uwe John, Klaus Valentin, Gernot Glöckner In vivo observations of OWA induced pH changes in the brain of polar cod Boreogadus saida / Christian Bock, Felizitas C. Wermter, Bastian Maus, Hans-O. Pörtner, Wolfgang Dreher A journey into the Triassic polar forests of Antarctica / Benjamin Bomfleur Long-term time-series of Arctic BrO derived from UV-VIS satellite remote sensing / lias Bougoudis, Anne-Marlene Blechschmidt, Andreas Richter, Sora Seo, John P. Burrows The effect of climate change on the carbon balance in microalgae / Deborah Bozzato, Torsten Jakob, Christian Wilhelm Species composition and abundance of the shallow water fish community of Kongsfjorden, Svalbard / Markus Brand, Philipp Fischer Decadal changes in a breeding population of southern giant petrels on King George Island, Antarctic, in response to human activities / Christina Braun, Jan Esefeld, Hans-Ulrich Peter Geodetic GNSS measurements to investigate the recent crustal deformation at the Antarctic Peninsula and in the Amundsen Sea Embayment, West Antarctica / Peter Busch, Mirko Scheinert, Christoph Knöfel, Lutz Eberlein, Martin Horwath, Ludwig Schröder, Andreas Groh Parameterization of snow BRDF measurements in Antarctica / T. Carlsen, G. Birnbaum, A. Ehrlich, M. Schäfer, and M. Wendisch Airborne and in situ ground-based measurements of surface albedo, bidirectional reflectivity, and snow properties on the Antarctic plateau / T. Carlsen, M. Belke Brea, G. Birnbaum, A. Ehrlich, J. Freitag, G. Heygster, L. Istomina, S. Kipfstuhl, A. Orsi, M. Schäfer, and M. Wendisch Retreats of ice sheet and ice shelf driven by warm water incursions in the Ross Sea since the Last Glacial Maximum / Zhihua Chen, Mengshan Ju, Shulan Ge, Zheng Tang, Yuanhui Huang, Renjie Zhao, Ralf Tiedemann, Lester Lembke-Jene Influence of breeze circulation on local wind climatology in Svalbard fjords / Małgorzata Cisek, Przemysław Makuch, Tomasz Petelski, Jacek Piskozub Life strategies on photobiology and metabolite profile of genetic indentical photobionts of two different lichen species / Nadine Determeyer-Wiedmann, Sieglinde Ott Land-Ocean Interactions in the late glacial Bering Sea / B. Diekmann, R. Wang, H. Kühn, R. Gersonde, R. Tiedemann, G. Kuhn Does environmental change affect polar microbial communities? / Daniel R. Dietrich Rapid glacial isostatic uplift in Patagonia: Interplay of enhanced ice mass loss and slab window tectonics / R. Dietrich, A. Richter, E. Ivins, H. Lange, L. Mendoza, L. Schröder, J.L. Hormaechea, G. Casassa, E. Marderwald, M. Fritsche, R. Perdomo, M. Horwath Phylogenomics of the longitarsal Colossendeidae: the evolution of a diverse Antarctic sea spider radiation / Lars Dietz, Jana S. Dömel, Christoph Mayer, Florian Leese Revealing the evolutionary history of Southern Ocean sea spiders using genome-wide SNP data / Jana S. Dömel, Till-Hendrik Macher, Lars Dietz, Christoph Mayer, Roland R. Melzer and Florian Leese Geothermal heat flux derived from airborne magnetic grids and measured temperature gradients in the Amundsen Sea sector of West Antarctica / Ricarda Dziadek, Karsten Gohl, Fausto Ferraccioli, Norbert Kaul, Cornelia Spiegel Sea spray aerosol fluxes in the area of the Spitsbergen Shelf and the Greenland Sea / K. Dziembor, T. Petelski, P. Markuszewski, T. Zieliński, P. Makuch, I. Wróbel More than two decades of geodetic GNSS measurements in Antarctica, Greenland and Patagonia – a technology review / Lutz Eberlein, Mirko Scheinert, Peter Busch, Christoph Knöfel, Andreas Richter Analysing the flow velocity of major outlet glaciers in North Greenland using Landsat data / Benjamin Ebermann, Ralf Rosenau, Mirko Scheinert, Martin Horwath Partitioning growing season net ecosystem exchange of CO2 into photosynthesis, autotrophic and heterotrophic respiration in the Siberian tundra / Tim Eckhardt, Christian Knoblauch, Lars Kutzbach, Gillian Simpson, Eva-Maria Pfeiffer Meteorological collaboration in the Arctic / Johanna Ekman Meteorological aspects of S.A. Andrée’s attempt to reach the North Pole by balloon in 1897 / Dieter Etling Geodetic mass balance on South Georgia glaciers / David Farias-Barahona, Christian Sommer, Thorsten Seehaus, Philipp Malz, Gino Casassa, Matthias H. Braun Frozen-Ground Cartoons: An international collaboration between artists and permafrost scientists / Michael Fritz, Frédéric Bouchard, Bethany Deshpande, Julie Malenfant-Lepage, Alexandre Nieuwendam, Michel Paquette, Ashley Rudy, Matthias Siewert, Audrey Veillette, Stefanie Weege, Jon Harbor, Otto Habeck, Ylva Sjöberg The Akademii Nauk ice core and solar activity / Diedrich Fritzsche, Luisa von Albedyll, Silke Merchel, Thomas Opel, Georg Rugel, Andreas Scharf Walther Bruns, Gründer der „Aeroarctic“ – ein vergessener Pionier der Deutschen Polarforschung / Diedrich Fritzsche Warming and reduction of precipitations affect the microbiome of recently deglaciated soils in the Swiss Alps / Aline Frossard, Johanna Donhauser, Pascal Niklaus, Thomas Rime, Beat Frey The ice-free topography of Svalbard / Johannes J. Fürst, Francisco Navarro, Fabien Gillet-Chaulet, Geir Moholdt, Xavier Fettweis, Charlotte Lang, Thorsten Seehaus, Matthias H. Braun, Douglas I. Benn, Toby J. Benham, Julian A. Dowdeswell, Mariusz Grabiec, Jack Kohler, Katrin Lindbäck, Rickard Pettersson, Heidi Sevestre Scientific Drilling in Antarctica? Coming to a new drilling proposal / Christoph Gaedicke, Gerhard Kuhn, Olaf Eisen, Andreas Läufer, Emma Smith, Nikola Koglin, Boris Biskaborn, Dieter Franke, Ralf Tiedemann German permanent research facilities in Antarctica - a 40 years record / Hartwig Gernandt Pre-glacial and glacial shelf evolution from seismic and seabed drill records of the Amundsen Sea, West Antarctica / Karsten Gohl, Gabriele Uenzelmann-Neben, Robert Larter, Johann Klages, Claus-Dieter Hillenbrand, Torsten Bickert, Steve Bohaty, Ulrich Salzmann, Thomas Frederichs, Catalina Gebhardt, Katharina Hochmuth and Expedition PS104 Science Party The Turnove
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  • 78
    Call number: AWI G3-19-93211 ; AWI G3-19-93211(2. Ex.)
    Type of Medium: Dissertations
    Pages: viii, 220 Seiten , Illustrationen
    Language: English
    Note: Dissertation, Universität Potsdam, 2019 , Table of Contents Abstract Zusammenfassung 1 Introduction 1.1 Scientific background 1.1.1 Permafrost - terrestrial and subsea 1.1.2 Subsea permafrost distribution 1.1.3 Relevance in the context of a changing Arctic 1.1.4 Influences on subsea permafrost 1.2 Hypotheses and objectives 1.3 Thesis organization 2 Detection of subsea permafrost degradation rates 2.1 An overview of geophysical methods and studies in subsea permafrost 2.2 Geophysical objectives 2.3 Passive seismic techniques 2.3.1 H/V passive seismics 2.3.2 Passive seismic interferometry 2.4 Instrument design & marine tests on Sylt 2.5 Arctic feasibility test site around Muostakh Island 2.6 Arctic deployment for wide area detection around Muostakh Island 3 Modelling of subsea permafrost degradation processes 3.1 An overview on subsea permafrost modelling 3.2 Salt distribution- mechanisms beyond diffusional transport 3.3 Open questions in salt transport and permafrost degradation 3.4 Modelling objectives 3.5 Study sites 3.5.1 Primary study site: Cape Mamontov Klyk 3.5.2 Secondary study sites: Buor Khaya & Muostakh Island 3.6 Developing a model for subsea permafrost 3.6.1 Thermal regime of the subsurface: governing equations of conductive heat transfer 3.6.2 Model definitions: concentration and thaw depth 3.6.3 Saline effect on the state of permafrost 3.6.4 Salt transport: governing equation & parameterizations 3.6.5 Modelling approach 3.6.6 Model testing 3. 7 Results: Influence of model parameters on subsea permafrost degradation 3.8 Discussion and implications 3.8.1 Modelled inundation parameters 3.8.2 Further factors affecting subsea permafrost degradation 3.8.3 Implications 4 From local to regional scale: Amending sparsely distributed temperature records 4.1 An overview of borehole temperature reconstruction . 4.2 On the transferability of ground to air temperatures . 4.3 Reconstruction objectives 4.4 Borehole sites and climate 4.5 Borehole temperatures 4.6 Inversion method 4.6.1 Forward model 4.6.2 Optimization 4.6.3 Sensitivity analysis 4.7 Results and discussion of the reconstruction from the permafrost boreholes 4.7.1 Recoverable period 4.7.2 Optimization 4.7.3 Surface temperature reconstructions and fit 4.7.4 Inversion method's impact on character of solution & sensitivity to temperature history parameterization 4.8 Discussion of spatial differences and implications 4.8.1 Comparison to other temperature data 4.8.2 Site differences 4.8.3 Methodological considerations 4.8.4 Implications 5 Conclusion and outlook 5.1 Outlook Appendices A Modelling tests for H/V method configuration Bibliography Acknowledgements
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  • 79
    Call number: AWI E2-20-93574
    In: Geo : die Welt mit anderen Augen sehen, 03/2020
    Type of Medium: Journal available for loan
    Pages: Seite 26-48 , Illustrationen
    ISSN: 0342-8311
    Series Statement: Geo : die Welt mit anderen Augen sehen 03/2020
    Language: German
    Note: TITELTHEMA: Gefangen im Eis Seit Herbst 2019 führt das Forschungsschiff „Polarstern“ die größte Arktisexpedition aller Zeiten an. Hunderte Wissenschaftler erforschen die Umwelt in der Nordpolregion – unter härtesten Bedingungen. Von Marlene Göring und Esther Horvath NEUSEELAND Ein Land auf Rattenjagd Invasive Arten machen der Vogelwelt auf Neuseeland den Garaus. Jetzt rüsten Tierschützer zum Kampf: Millionen Ratten, Wiesel und Possums sollen sterben. Kann der wahnwitzige Plan gelingen? Von Anke Sparmann und David M. Smith PORTRÄT Musikalische Leckerlis Katzen mögen Mozart? Nur weil sie nichts Besseres kennen. Der Cellist David Teie komponiert Musik eigens für Katzen, Hunde und Affen – mit erstaunlichem Erfolg. Von Johannes Böhme und Jared Soares HONGKONG Die Kolonie der Kämpfer Unversöhnlich stehen sich Polizisten und Demonstranten auf Hongkongs Straßen gegenüber; immer gewalttätiger werden die Proteste. Ein GEO-Team hat unter großer Gefahr Aktivisten über Monate begleitet. FOTOGRAFIE Europa in der Nachkriegszeit Bill Perlmutter kam in den 1950er Jahren als Soldat mit dem Auftrag nach Europa, das alltägliche Leben zu dokumentieren. Sein unvoreingenommener Blick zeigt Menschen mit fröhlichem Aufbruchsgeist. ANTIMATERIE Spurensuche in der Schattenwelt In der Fantasie des Kinos treibt sie Raumschiffe an, im wahren Leben stellt sie Physiker vor ein Rätsel: Eigentlich gibt es viel zu wenig Antimaterie auf der Welt. Wo ist der geheimnisvolle Stoff abgeblieben? KOSMOS In Australien rettet die Feuerwehr Dinosaurier-Bäume. Tiefseekorallen vor Hawaii erholen sich verblüffend schnell. Ein Smartphone-Mikroskop soll Menschen helfen. Dazu Geschichten in Bildern aus Louisiana, der Mongolei und Mosambik GEO-TAG DER NATUR Wie vielfältig sind unsere Biotope? Beim GEO-Tag der Natur werden wieder Tausende Naturliebhaber in ganz Deutschland ausschwärmen, um Artenvielfalt zu kartieren 361° Können Krokodile weinen? Brauchen wir personalisierte Medikamente? Warum gibt es in Städten mehr Kriminalität? Antworten auf diese und weitere spannende Fragen WELTBÜRGER Fermin Pablo Cilio aus Peru
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  • 80
    Call number: ZSP-599-150
    In: Rapportserie / Norsk Polarinstitutt, (DE-B103)114733
    Type of Medium: Series available for loan
    Pages: 325 Seiten , Illustrationen, Karten, Diagramme
    ISBN: 9788276664119 , 9788276664126
    Series Statement: Rapportserie / Norsk Polarinstitutt nr. 150
    Language: Norwegian
    Note: In norwegischer Sprache
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  • 81
    Call number: AWI A7-20-93463
    Description / Table of Contents: Die Arktis erwärmt sich schneller als der Rest der Erde. Die Auswirkungen manifestieren sich unter Anderem in einer verstärkten Erwärmung der arktischen Grenzschicht. Diese Arbeit befasst sich mit Wechselwirkungen zwischen synoptischen Zyklonen und der arktischen Atmosphäre auf lokalen bis überregionalen Skalen. Ausgangspunkt dafür sind Messdaten und Modellsimulationen für den Zeitraum der N-ICE2015 Expedition, die von Anfang Januar bis Ende Juni 2015 im arktischen Nordatlantiksektor stattgefunden hat. Anhand von Radiosondenmessungen lassen sich Auswirkungen von synoptischen Zyklonen am deutlichsten im Winter erkennen, da sie durch die Advektion warmer und feuchter Luftmassen in die Arktis den Zustand der Atmosphäre von einem strahlungs-klaren in einen strahlungs-opaken ändern. Obwohl dieser scharfe Kontrast nur im Winter existiert, zeigt die Analyse, dass der integrierte Wasserdampf als Indikator für die Advektion von Luftmassen aus niedrigen Breiten in die Arktis auch im Frühjahr geeignet ist. Neben der Advektion von…
    Type of Medium: Dissertations
    Pages: xiv, 147 Seiten , Illustrationen, Diagramme
    Language: German
    Note: Inhaltsverzeichnis 1 Einleitung 1.1Wissenschaftliche Zielsetzung 2 Grundlagen 2.1 Grundgleichungen 2.2 Potentielle Vorticity 2.3 Planetare Wellen 2.4 Atmosphärische Instabilität 2.5 Grenzschicht 2.6 Kopplung von Tropo- und Stratosphäre 3 Daten und Methoden 3.1 N-ICE2015 3.1.1 Expeditionsbeschreibung 3.1.2 Ziele der Expedition 3.2 Daten 3.2.1 Beobachtungsdaten 3.2.2 ERA-Interim Reanalyse 3.2.3 Das HIRHAM5 Modell 3.3 Analysemethoden 3.3.1 Temperaturinversionen 3.3.2 Vertikale Stabilität 3.3.3 Grenzschichthöhe 3.3.4 Eady Growth Rate 3.3.5 2d-Skalenfilterung und -Pattern-Korrelation 3.3.6 Nudging Experiment 4 Analyse der N-ICE2015 Radiosonden 4.1 Blick auf die Troposphäre 4.2 Fallstudie zum M2-Sturm: A 4.3 Zyklonencharakteristika 4.4 Temperaturinversionen und Stabilität 4.5 Vergleich mit ERA-Interim, SHEBA und Ny-Ålesund 4.6 Résumé der Expeditionsdaten 5 Nudging Studien mit HIRHAM5 5.1 Vergleich mit ERA-Interim 5.2 Vergleich der Simulationen 5.3 Fallstudie zum M2-Sturm: B 5.3.1 Synoptische Aktivität 5.4 Statistischer Vergleich 6 Einfluss der Stratosphäre 6.1 Stratosphäre im Winter 2014/2015 6.2 Fallstudie zum M2-Sturm: C 6.3 PV als Ladung 6.4 Résumé der Beobachtungen 7 Zusammenfassung und Ausblick A Zusätztliche Abbildungen B Literaturverzeichnis
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  • 82
    Call number: AWI G3-20-93465
    Type of Medium: Dissertations
    Pages: xi, 113, xxxvii Seiten , Illustrationen, Diagramme
    Language: English
    Note: Table of Contents Abstract Zusammenfassung List of Figures List of Tables 1. Introduction 1.1 Scientific Background 1.1.1 Arctic Climate Change 1.1.2 Permafrost Degradation 1.1.3 The Arctic Freshwater System and its Biogeochemistry 1.2 Objectives 1.3 Study Region and Methods 1.3.1 Study Area 1.3.2 Field Sampling and Measurements 1.3.3 Geochemical Analyses 1.3.4 Data Processing 1.4 Thesis Structure 1.5 Author Contributions 2. Spatial Variability of Dissolved Organic Carbon, Solutes and Suspended Sediment in Disturbed Low Arctic Coastal Watersheds 2.1 Abstract 2.2 Introduction 2.3 Study Site 2.4 Methods 2.4.1 Stream Monitoring 2.4.2 Mapping of Disturbances 2.4.3 Flux Estimates and Statistics 2.5 Results 2.5.1 Catchment Disturbance 2.5.2 Runoff and Hydrochemistry 2.5.3 Lateral Transport of Stream Water 2.5.4 Hydrochemical Composition and Fluxes in Nearby Streams 2.6 Discussion 2.6.1 Total Runoff and Water Quality 2.6.2 Water Quality Changes from Headwaters to Downstream 2.6.3 Changes in Hydrochemistry and Isotopic Composition over Time 2.6.4 Importance of Disturbances for Hydrochemistry 2.7 Conclusions 2.8 Supplementary Material 3. Terrestrial Colored Dissolved Organic Matter (cDOM) in Arctic Catchments - Characterizing Organic Matter Composition Across the Arctic 3.1 Introduction 3.2 Study Area 3.3 Methods 3.3.1 Field Methods and Hydrochemistry 3.3.2 Statistical Analyses 3.4 Results 3.4.1 Meteorological Conditions and General Hydrochemistry 3.4.2 DOC and cDOM Absorption Characteristics 3.4.3 Downstream Patterns of DOC and cDOM Along Longitudinal Transects 3.4.4 Temporal Trends ofDOC and cDOM with Changing Meteorological Conditions 3.5 Discussion 3.5.1 Limitations of cDOM Measurements from Terrestrial Sources 3.5.2 Catchment Processes and Biogeochemical Cycling 3.5.2.1 Regional Catchment Properties 3.5.2.2 Rainfall Events 3.5.2.3 Downstream Patterns and Impact of Permafrost Disturbance 3.5.3 Nature of cDOM-DOC Across the Terrestrial Arctic 3.6 Conclusion 3.7 Supplementary Material 4. Summer Rainfall DOC, Solute and Sediment Fluxes in a Small Arctic Coastal Catchment on Herschel Island (Yukon Territory, Canada) 4.1 Abstract 4.2 Introduction 4.3 Study Site 4.4 Methodology 4.4.1 Weather data 4.4.2 Hydrology 4.4.3 Suspended Sediment and Hydrochemistry 4.4.4 Flux Estimates and Statistics 4.5 Results 4.5.1 Meteorological Conditions 4.5.2 Streamflow and Electrical Conductivity 4.5.3 Transport of Suspended Sediment and Organic Matter 4.5.4 Solute Transport 4.5.5 Alluvial Fan Sampling 4.6 Discussion 4.6.1 Hydrological Response 4.6.2 Water Quality and Fluxes 4.6.3 Rainfall Response and Flow Pathways 4.7 Conclusions 4.8 Supplementary Material 5. Synthesis 5.1 Impacts of Permafrost Degradation on Stream Biogeochemistry 5.2 Controls on DOM Quality across the Arctic 5.3 Biogeochemical Fluxes from Small Coastal Catchments to the Arctic Ocean 5.4 Challenges 5.5 Outlook Acronyms Bibliography Acknowledgements Eidesstattliche Erklärung
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  • 83
    Call number: AWI G8-20-93468
    Type of Medium: Dissertations
    Pages: XIII, 151, A28 Seiten , Illustrationen, Diagramme, Karten
    Language: English
    Note: Table of contents Abstract Zusammenfassung Abbreviations and Nomenclature 1. Introduction 1.1 Scientific Background 1.1.1 Climate and Permafrost 1.1.2 Remote Sensing 1.1.3 Research Questions 1.2 General Approach 1.3 Thesis Structure 1.4 Author’ s contributions 1.4.1 Chapter 2 1.4.2 Chapter 3 1.4.3 Chapter 4 1.4.4 Chapter 5 1.4.5 Appendix Paper 1 2. Detection of landscape dynamics in the Arctic Lena Delta withtemporally dense Landsat time-series Stacks 2.1 Abstract 2.2 Introduction 2.3 Study Area and Data 2.3.1 Study Area 2.3.2 Data 2.3.3 Methods/processing 2.4 Results 2.4.1 Regional Scale changes 2.4.2 Local scale changes 2.5 Discussion 2.5.1 Regional scale changes 2.5.2 Local scale changes 2.5.3 Data quality 2.5.4 Data usage and outlook 2.6 Conclusion 2.7 Data Archive 2.8 Acknowledgements 2.9 Appendix A. Supplementary Data 3. Landsat-Based Trend Analysis of Lake Dynamics across NorthernPermafrost Regions 3.1 Abstract 3.2 Introduction 3.3 Study Sites 3.3.1 Alaska North Slope (NSL) 3.3.2 Alaska Kobuk-Selawik Lowlands (AKS) 3.3.3 Central Yakutia (CYA) 3.3.4 Kolyma Lowland (KOL) 3.4 Data and Methods 3.4.1 Data and Trend Analysis 3.4.2 Pixel-Based Machine-Leaming Classification 3.4.3 Object-Based Image Analysis 3.4.4 Data Quality and Post-Processing 3.4.5 Calculation of Lake Change Statistics 3.5 Results 3.5.1 NSL (Alaska North Slope) 3.5.2 AKS (Alaska Kobuk-Selawik Lowlands) 3.5.3 CYA (Central Yakutia) 3.5.4 KOL (Kolyma Lowland) 3.6 Discussion 3.6.1 Data Analysis 3.6.2 Comparison of Sites and Prior Studies 3.7 Conclusions 3.8 Supplementary Materials 3.9 Acknowledgements 3.10 Appendix A 4. Remotely sensing recent permafrost region disturbances across Arcticto Subarctic transects 4.1 Abstract 4.2 Introduction 4.3 Results 4.3.1 Lakes 4.3.2 Retrogressive Thaw Slumps 4.3.3 Wildfire 4.4 Discussion 4.5 Methods 4.5.1 Remote Sensing Data Processing 4.5.2 Auxiliary Data Sources 5. Tundra landform and Vegetation productivity trend maps for theArctic Coastal Plain of northern Alaska 5.1 Abstract 5.2 Background & Summary 5.3 Methods 5.3.1 Polygonal tundra geomorphology mapping 5.3.2 Image processing 5.3.3 Image Classification 5.3.4 Decadal scale NDVI trend analysis 5.4 Data Records 5.5 Technical Validation 5.5.1 Tundra Geomorphology Map 5.5.2 NDVI Trend Map 5.6 Data Citation 6. Discussion/Synthesis 6.1 Landsat-based trend analysis 6.1.1 Spatial Scale 6.1.2 Time series analysis 6.1.3 Model complexity 6.2 Mapping of permafrost landscape dynamics 6.2.1 Lake dynamics 6.2.2 Wildfire 6.2.3 Retrogressive Thaw Slumps 6.3 Pan-arctic scale distribution and consequences of changes inpermafrost 6.4 Outlook Bibliography A-1. Appendix: Reduced arctic tundra productivity linked with landform and climate change interactions A-1.1 Abstract A-1.2 Introduction A-1.3 Methods A-1.4 Results A-1.5 Discussion Danksagung/Acknowledgements Eidesstattliche Erklärung
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  • 84
    Monograph available for loan
    Monograph available for loan
    [Aarhus] : Aarhus University, DCE - Danish Centre for Environment and Energy
    Call number: AWI P5-20-93484
    Type of Medium: Monograph available for loan
    Pages: 189 Seiten , Illustrationen
    Edition: third edition
    ISBN: 978-87-93129-15-3
    Language: English
    Note: INTERACT STATIONS SVALBARD, NORWAY 1 AWIPEV Arctic Research base 2 CNR Arctic Station "Dirigibile ltalia" 3 Ny-Ålesund Research Station- Sverdrup 4 UK Arctic Research Station 5 Netherlands' Arctic Station 6 Adam Mickiewicz University Polar Station - Petuniabukta 7 Czech Arctic Research Station of Josef Svoboda 8 Polish Polar Station, Hornsund NORWAY 9 Finse Alpine Research Centre 10 Nibio Svanhovd Research Station SWEDEN 11 Svartberget Research Station 12 Tarfala Research Station 13 Abisko Scientific Research Station FINLAND 14 Kilpisjarvi Biological Station 15 Pallas-Sodankyla Stations 16 Kolari Research Unit 17 Hyytiälä Forest Research Station 18 Kainuu Fisheries Research Station 19 Oulanka Research Station 20 Varrio Subarctic Research Station 21 Kevo Subarctic Research Station SWITZERLAND 22 Alpine Research and Education Station Furka AUSTRIA 23 Station Hintereis 24 Sonnblick Observatory CZECH REPUBLIC 25 Krkonose Mountains National Park POLAND 26 Karkonosze Mountains National Park 27 M&M Klapa Research Station RUSSIA 28 Lammin-Suo Peatland Station 29 Khibiny Educational and Scientific Station 30 The Arctic Research Station 31 Mukhrino Field Station 32 Numto Park Station 33 Khanymey Research Station 34 Beliy Island Research Station 35 Willem Barentsz Biological Station 36 lgarka Geocryology Laboratory 37 Kajbasovo Research Staton 38 Aktru Research Station 39 Evenkian Field Station 40 International Ecological Educational Center "lstomino" 41 Research Station Samoylov Island 42 Spasskaya Pad Scientific Forest Station 43 Elgeeii Scientific Forest station 44 Chokurdakh Scientific Tundra Station 45 Orotuk Field Station 46 AvachinskyVolcano Field Station 47 North-East Science Station 48 Meinypil'gyno Community Based Biological Station KYRGYZ REPUBLIC 49 Adygine Research Station ALASKA 50 Barrow Arctic Research Center/Barrow Environmental Observatory 51 Toolik Field Station CANADA 52 Kluane Lake Research Station 53 Western Arctic Research Centre 54 Canadian High Arctic Research Station 55 M'Clintock Channel Polar Research Cabins 56 Churchill Northern Studies Centre 57 Flashline Mars Arctic Research Station 58 Polar Environment Atmospheric Research Laboratory 59 CEN Ward Hunt Island Research Station 60 CEN Bylot Island Field Station 61 lgloolik Research Center 62 CEN Salluit Research Station 63 CEN Boniface River Field Station 64 CEN Umiujaq Research Station 65 CEN Whapmagoostui-Kuujjuarapik Research Station 66 CEN Radisson Ecological Research Station 67 CEN Clearwater Lake Research Station 68 Nunavut Research Institute 69 CEN Kangiqsualujjuaq Sukuijarvik Research Station 70 Uapishka Research Station 71 Labrador Institute Research Station GREENLAND 72 DMI Geophysical Observatory- Qaanaaq 73 Arctic Station 74 Arctic DTU, ARTEK Research Station 75 Greenland Institute of Natural Resources 76 Sermilik Research Station 77 Summit Station 78 EGRIP Field Station 79 Zackenberg Research Station 80 Villum Research Station ICELAND 81 Sudurnes Science and Learning Center 82 Litla-Skard 83 China-lceland Arctic Observatory 84 Rif Field Station 85 Skálanes Nature and Heritage Center FAROE ISLANDS 86 Faroe Islands Nature Investigation SCOTLAND 87 ECN Cairngorms
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  • 85
    Call number: AWI G3-20-93487
    Description / Table of Contents: This book provides a general survey of Geocryology, which is the study of frozen ground called permafrost. Frozen ground is the product of cold climates as well as a variety of environmental factors. Its major characteristic is the accumulation of large quantities of ice which may exceed 90% by volume. Soil water changing to ice results in ground heaving, while thawing of this ice produces ground subsidence often accompanied by soil flowage. Permafrost is very susceptible to changes in weather and climate as well as to changes in the microenvironment. Cold weather produces contraction of the ground, resulting in cracking of the soil as well as breakup of concrete, rock, etc. Thus permafrost regions have unique landforms and processes not found in warmer lands. The book is divided into three parts. Part 1 provides an introduction to the characteristics of permafrost. Four chapters deal with its definition and characteristics, the unique processes operating there, the factors affecting it, and its general distribution. Part 2 consists of seven chapters describing the characteristic landforms unique to these areas and the processes involved in their formation. Part 3 discusses the special problems encountered by engineers in construction projects including settlements, roads and railways, the oil and gas industry, mining, and the agricultural and forest industries. The three authors represent three countries and three language groups, and together have over 120 years of experience of working in permafrost areas throughout the world. The book contains over 300 illustrations and photographs, and includes an extensive bibliography in order to introduce the interested reader to the large current literature.
    Type of Medium: Monograph available for loan
    Pages: xliii, 765 Seiten , Illustrationen, Karten, Diagramme
    Edition: First edition
    ISBN: 9781138054165 , 9781315166988 (electronic)
    Language: English
    Note: Table of contents Preface About the authors Acknowledgements Dedication List of figures List of tables List of symbols Part I Introduction and characteristics of permafrost I Definition and description 1.1 Introduction 1.2 Additional terms originating in Russia 1.3 History of permafrost research 1.4 Measurement of ground temperature 1.5 Conduction, convection and advection 1.6 Therm al regimes in regions based on heat conduction 1.7 Continentality index 1.8 Moisture movement in the active layer during freezing and thawing 1.9 Moisture conditions in permafrost ground 1.10 Results of freezing moisture 1.11 Strength of ice 1.12 Cryosols, gelisols, and leptosols 1.13 Fragipans 1.14 Salinity in permafrost regions 1.15 Organic matter 1.16 Micro-organisms in permafrost 1.16.1 Antarctic permafrost 1.16.2 High-latitude permafrost 1.16.3 High altitude permafrost in China 1.16.4 Phenotypic traits 1.16.5 Relation to climate change on the Tibetan plateau 1.17 Gas and gas hydrates 1.18 Thermokarst areas 1.19 Offshore permafrost 2 Cryogenic processes where temperatures dip below 0°C 2.1 Introduction 2.2 The nature of ice and water 2.3 Effects of oil pollution on freezing 2.4 Freezing and thawing of the active layer in permafrost in equilibrium with a stable climate 2.5 Relation of clay mineralogy to the average position of the permafrost table 2.6 Ground temperature envelopes in profiles affected by changes in mean annual ground surface temperature (MASGT) 2.7 Needle ice 2.8 Frost heaving 2.9 Densification and thaw settlement 2.10 Cryostratigraphy, cryostructures, cryotextures and cryofacies 2.11 Ground cracking 2.12 Dilation cracking 2.13 Frost susceptibility 2.14 Cryoturbation, gravity processes and injection structures 2.14.1 Cryoturbation 2.14.2 Upward injection of sediments from below 2.14.3 Load-casting 2.15 Upheaving of objects 2.16 Upturning of objects 2.17 Sorting 2.18 Weathering and frost comminution 2.19 Karst in areas with permafrost 2.20 Seawater density and salinity 3 Factors affecting permafrost distribution 3.1 Introduction 3.2 Climatic factors 3.2.1 Heat balance on the surface of the Earth and its effect on the climate 3.2.2 Relationship between air and ground temperatures 3.2.3 Thermal offset 3.2.4 Relation to air masses 3.2.5 Precipitation 3.2.6 Latitude and longitude 3.2.7 Topography and altitude 3.2.8 Cold air drainage 3.2.9 Buffering of temperatures against change in mountain ranges 3.3 Terrain factors 3.3.1 Vegetation 3.3.2 Hydrology 3.3.3 Lakes and water bodies 3.3.4 Nature of the soil and rock 3.3.5 Fire 3.3.6 Glaciers 3.3.7 The effects of Man 4 Permafrost distribution 4.1 Introduction 4.2 Zonation of permafrost 4.3 Permafrost mapping 4.4 Examples of mapping units used 4.5 Modeling permafrost distribution 4.6 Advances in geophysical methods 4.7 Causes of variability reducing the reliability of small-scale maps 4.8 Maps of permafrost-related properties based on field observations 4.8.1 Permafrost thickness 4.8.2 Maps of ice content 4.8.3 Water resources locked up in perennially frozen ground 4.8.4 Total carbon content 4.9 Use of remote sensing and airborne platforms in monitoring environmental conditions and disturbances 4.10 Sensitivity to climate change: Hazard zonation 4.11 Classification of permafrost stability based on mean annual ground temperature Part II Permafrost landforms II. 1 Introduction 5 Frost cracking, ice-wedges, sand, loess and rock tessellons 5.1 Introduction 5.2 Primary and secondary wedges 5.2.1 Primary wedges 5.2.1.1 Ice-wedges 5.2.1.2 Sand tessellons 5.2.1.3 Loess tessellons 5.2.1.4 Rock tessellons 5.2.2 Secondary wedges 5.2.2.1 Ice-wedge casts 5.2.2.2 Soil wedges 6 Massive ground ice in lowlands 6.1 Introduction 6.2 Distribution of massive icy beds in surface sediments 6.3 Sources of the sediments 6.4 Deglaciation of the Laurentide ice sheet 6.5 Methods used to determine the origin of the massive icy beds 6.6 Massive icy beds interpreted as being formed by cryosuction 6.7 Massive icy beds that may represent stagnant glacial ice 6.8 Other origins of massive icy beds 6.9 Ice complexes including yedoma deposits 6.10 Conditions for growth of thick ice-wedges 6.11 The mechanical condition of the growth of ice-wedges and its connection to the properties of the surrounding sediments 6.12 Buoyancy of ice-wedges 6.13 Summary of the ideas explaining yedoma evolution 6.14 Aufeis 6.15 Perennial ice caves 6.16 Types of ice found in perennial ice caves 6.17 Processes involved in the formation of perennial ice caves 6.18 Cycles of perennial cave evolution 6.18.1 Perennial ice caves in deep hollows 6.18.2 Sloping caves with two entrances 6.18.3 Perennial ice caves with only one main entrance but air entering through cracks and joints in the bedrock walls 6.18.4 Perennial ice caves with only one main entrance and no other sources of cooling 6.19 Ice caves in subtropical climates 6.20 Massive blocks of ice in bedrock or soil 7 Permafrost mounds 7.1 Introduction 7.2 Mounds over 2.5 m diameter 7.2.1 Mounds formed predominantly of injection ice 7.2.1.1 Pingo mounds 7.2.1.2 Hydrostatic or closed system pingos 7.2.1.3 Hydraulic or open system pingos 7.2.1.4 Pingo plateaus 7.2.1.5 Seasonal frost mounds 7.2.1.6 Icing blisters 7.2.1.7 Perennial mounds of uncertain origin 7.2.1.8 Similar mounds that can be confused with injection phenomena 7.2.2 Mounds formed dominantly by cryosuction 7.2.2.1 Paisas 7.2.2.1.1 Paisas in maritime climates 7.2.2.1.2 Paisas in cold, continental climates 7.2.2.1.3 Lithalsas 7.2.2.1.4 Palsa/Lithalsa look-alikes 7.2.3 Mounds formed by the accumulation of ice in the thawing fringe: Peat plateaus 7.3 Cryogenic mounds less than 2.5 m in diameter 7.3.1 Oscillating hummocks 7.3.2 Thufurs 7.3.3 Silt-cycling hummocks 7.3.4 Niveo-aeolian hummocks 7.3.5 Similar-looking mounds of uncertain origin 7.3.6 String bogs 7.3.7 Pounus 8 Mass wasting of fine-grained materials in cold climates 8.1 Introduction 8.2 Classification of mass wasting 8.3 Slow flows 8.3.1 Cryogenic creep 8.3.1.1 Needle ice creep 8.3.1.2 Frost heave and frost creep 8.3.1.3 Gelifluction 8.3.1.4 Other creep-type contributions to downslope movement of soil 8.3.2 Landforms produced by cryogenic slow flows in humid areas 8.3.3 Landforms developed by cryogenic flows in more arid regions 8.4 Cryogenic fast flows 8.4.1 Cryogenic debris flows 8.4.2 Cryogenic slides and slumps 8.4.3 Cryogenic composite slope failures 8.4.3.1 Active-layer detachment slides 8.4.3.2 Retrogressive thaw failures 8.4.3.3 Snow avalanches and slushflows 8.4.3.3.1 Snow avalanches 8.4.3.3.2 Slush avalanches 8.5 Relative effect in moving debris downslope in the mountains 9 Landforms consisting of blocky materials in cold climates 9.1 Introduction 9.2 Source of the blocks 9.3 Influence of rock type 9.4 Weathering products 9.5 Biogenic weathering 9.6 Fate of the soluble salts produced by chemical and biogenic weathering 9.7 Rate of cliff retreat 9.8 Landforms resulting from the accumulation of predominantly blocky materials in cryogenic climates 9.8.1 Cryogenic block fields 9.8.1.1 Measurement of rates of release of blocks on slopes 9.8.2 Cryogenic block slopes and fans 9.8.3 Classification of cryogenic talus slopes 9.8.3.1 Coarse blocky talus slopes 9.8.4 Protection of infrastructure from falling rock 9.9 Talus containing significant amounts of finer material 9.9.1 Rock glaciers 9.9.1.1 Sedimentary composition and structure of active rock glaciers 9.9.1.2 Origin of the ice in active rock glaciers 9.9.1.3 Relationship to vegetation 9.9.2 Movement of active rock glaciers 9.9.2.1 Horizontal movement 9.9.2.2 Movement of the front 9.9.3 Distribution of active rock glaciers 9.9.4 Inactive and fossil rock glaciers 9.9.5 Streams flowing from under rock glaciers 9.10 Cryogenic block streams 9.10.1 Characteristics 9.10.2 Classification 9.10.2.1
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  • 86
    Call number: AWI A8-20-93986
    Type of Medium: Dissertations
    Pages: VI, 129 Seiten , Diagramme
    Language: German
    Note: Inhaltsverzeichnis Kurzfassung Abstract 1 EINFÜHRUNG 2 GRUNDLAGEN 2.1 Allgemeine Zirkulation 2.2 Barokline Instabiltät 2.3 Horizontale und vertikale Wellenausbreitung 2.4 Die Rolle der Arktis im Klimasystem 2.5 Einfluss des klimatischen Wandels in der Arktis auf die mittleren Breiten 2.6 Atmosphärisches Energiespektrum und Skalenwechselwirkung 3 DATEN UND METHODEN 3.1 Verwendete Reanalyse- und Modelldaten 3.1.1 ERA-Interim 3.1.2 AFES 3.1.3 Aufteilung der verwendeten Daten in Zeiträume mit hoher und niedriger Meereisbedeckung 3.2 Methoden 3.2.1 Instabilitätsanalyse für einen zonalgemittelten Grundzustand 3.2.2 Identifikation bevorzugter großskaliger Zirkulationsmuster 3.2.3 Energie- und Enstrophiespektren 3.2.4 Statistische Testverfahren 4 ERGEBNISSE 4.1 Instabilitätsanalyse für einen zonalgemittelten Grundzustand . 4.1.1 Klimatologie ERA-Interim und AFES 4.1.2 Sensititvitätsstudie 4.2 Identifikation bevorzugter großskaliger Zirkulationsmuster 4.2.1 September 4.2.2 Oktober 4.2.3 November 4.2.4 Dezember 4.2.5 Januar 4.2.6 Februar 4.2.7 Zugehörige synoptisch-skalige Aktivität und 2m-Temperatur 4.3 Kinetische Energiespektren und nichtlineare Wechselwirkungen 4.3.1 Kinetische Energiespektren 4.3.2 Enstrophiespektren 4.3.3 Nichtlineare Energiewechselwirkungen, Energieflüsse und Enstrophieflüsse 5 ZUSAMMENFASSUNG UND AUSBLICK Tabellenverzeichnis Abbildungsverzeichnis Variablen und Symbole Literaturverzeichnis Danksagung Anhang A.1 Hough-Funktionen und vertikale Strukturfunktionen A.2 Zugeordnete Legendre-Polynome und Kugelflächenfunktionen Eidesstattliche Erklärung
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  • 87
    Call number: AWI G5-20-93987
    Type of Medium: Dissertations
    Pages: XVI, 91 Seiten , Illustrationen
    Language: English
    Note: Dissertation, Universität Potsdam, 2015 , Table of Contents Acknowledgements Abstract Zusammenfassung List of figures and tables List of Abbreviations 1. Introduction 1.1. Preface and thesis organization 1.2. Research motivation and relevance 1.3. Background knowledge 1.3.1. Terrigenous sediments 1.3.2. Hala Lake 1.3.3. The North Pacific 1.3.4. The Bering Sea 1.4. Aims and objectives 1.5. Methodological overview 1.5.1. Fieldwork 1.5.2. Age-depth modeling 1.5.3. Key proxies: grain size and clay minerals 1.5.4. Supplementary methodology: remote sensing, seismic sub-bottom profiling and geochemistry 1.6. Overview and status of the manuscripts 2 Manuscript 1 : Linkages between Quaternary climate change and sedimentary processes in Hala Lake, northern Tibetan Plateau, China Abstract 2.1. Introduction 2.2. Regional setting 2.3. Materials and methods 2.3.1. Remote sensing of the study area 2.3.2. Fieldwork 2.3.3. Radiocarbon dating of recovered sediment cores 2.3.4. Laboratory work 2.3.5. Statistical data treatment 2.4. Results and interpretation 2.4.1. Remote sensing on the spatial heterogeneity of lake ice and length of lake ice-free days 2.4.2. Seismic sub-bottom profiling 2.4.3. Age and sedimentary characteristics of the sediment core record 2.4.4. Grain-size modeling results 2.5. Discussion 2.5.1. Last Glacial Maximum (~24-17 cal. ka BP) 2.5.2. Time-equivalent of Heinrich Event 1 (~17-15.4 cal. ka BP) 2.5.3. Time-equivalent of Bolling-Allerod (~15.4-13 cal. ka BP) 2.5.4. Time-equivalent of Younger Dryas (~12.9-11.6 cal. ka BP) 2.5.5. Holocene (~11.6 cal. ka BP to present) 2.6. Conclusions Acknowledgments 3 Manuscript 2: Modern modes of provenance and dispersal of terrigenous sediments in the North Pacific and the Bering Sea: Implications and perspectives for palaeoenvironmental reconstructions Abstract 3.1. Introduction 3.2. Study area and regional setting 3.3. Material and methods 3.4. Results 3.4.1. Grain size distribution 3.4.2 Bulk mineralogy 3.4.3. Mineralogy of the clay fraction 3.5. Discussion 3.5.1. Sedimentary processes 3.5.2. Sediment provenance 3.5.3 Implications for palaeoenvironmental studies 3.6. Conclusions Acknowledgements 4 Manuscript 3: Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages Abstract 4.1. Introduction 4.2. Regional setting 4.3. Material and methods 4.4. Results and interpretation 4.4.1. Lithology and stratigraphy 4.4.2. Grain size distribution 4.4.3. Clay mineralogy 4.5. Discussion 4.5.1. Processes of terrigenous sediment supply 4.5.2. Detrital sediment sources 4.5.3. Detrital sediment supply and its relation to regionalpalaeoenvironmental changes 4.5.3.1. Time interval 32-15.7 ka BP: Background sedimentation at low sea level 4.5.3.2. Time interval 15.7-14.5 ka BP: Regional Meltwater Pulse 4.5.3.3. Time interval 14.5-12.9 ka BP: First biological bloom event 4.5.3.4. Time interval 12.9-6 ka BP: Cooling episode, rejuvenation of biological productivity and onset ofmodern conditions 4.5.4. Palaeoenvironmental implications 4.6. Conclusions Acknowledgements 5 Synthesis 5.1. The North Hemisphere synchronization of millennial climate oscillations during the last Glacial: teleconnections from Westerlies and thermohaline Circulation 5.2. The regional asynchronization of millennial climate oscillations during the last Glacial: discrepancy and "recording capacity" 5.3. Secondary connections between global climate transmissions: winter cyclone in the North Pacific 5.4. Future perspectives 6 References 7 Appendix Extended results: Core SO202-39-3 from the mid-latitude North Pacific 7.1. Material 7.2. Results 7.3. Oscillation of eolian sediment transport 7.4. Conclusions
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  • 88
    Call number: AWI Bio-20-93988
    Type of Medium: Dissertations
    Pages: x, 181 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2017 , Contents Abstract Kurzfassung Contents 1. List of figures 2. List of tables Chapter 1. General introduction 1. Motivation 2. Scientific background 3. Objectives of the thesis 4. Thesis outline Chapter 2. Manuscript 1: Treeline dynamics in Siberia under changing climates as inferred from an individual-based model for Larix 1. Abstract 2. Introduction 3. Material and Methods 4. Results 5. Discussion 6. Acknowledgements Chapter 3. Manuscript 2: Field and simulation data reveal dissimilar responses of Larix gmelinii stands to increasing temperature across the Siberian treeline ecotone 1. Abstract 2. Introduction 3. Methods 4. Results 5. Discussion 6. Acknowledgements Chapter 4. Manuscript 3: High gene flow and complex treeline dynamics on the Taymyr Peninsula (north-central Siberia), revealed by nuclear microsatellites of Larix 1. Abstract 2. Introduction 3. Materials and methods 4. Results 5. Discussion 6. Acknowledgements Chapter 5. Manuscript 4: Dispersal distances at treeline in Siberia - genetic guided model improvement 1. Abstract 2. Introduction 3. Methods 4. Results 5. Discussion 6. Acknowledgements Chapter 6. Synopsis 1. Towards a better understanding of Siberian treeline dynamics 2. Methodological challenges to reconstruct and predict the treeline advance 3. Conclusions 4. Outlook Appendix 1. Supplementary information for manuscript 1 (Chapter 2) 2. Supplementary information for manuscript 2 (Chapter 3) 3. Supplementary information for manuscript 3 (Chapter 4) 4. Supplementary information for manuscript 4 (Chapter 5) Bibliography Acknowledgements - Danksagung Declaration
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  • 89
    Call number: AWI G3-20-93985
    Description / Table of Contents: Der zentralasiatische Naturraum, wie er sich uns heute präsentiert, ist das Ergebnis eines Zusammenwirkens vieler verschiedener Faktoren über Jahrmillionen hinweg. Im aktuellen Kontext des Klimawandels zeigt sich jedoch, wie stark sich Stoffflüsse auch kurzfristig ändern und dabei das Gesicht der Landschaft verwandeln können. Die Gobi-Wüste in der Inneren Mongolei (China), als Teil der gleichnamigen Trockenregionen Nordwestchinas, ist aufgrund der Ausgestaltung ihrer landschaftsprägenden Elemente sowie ihrer Landschaftsdynamik, im Zusammenhang mit der Lage zum Tibet-Plateau, in den Fokus der klimageschichtlichen Grundlagenforschung gerückt. Als großes Langzeitarchiv unterschiedlichster fluvialer, lakustriner und äolischer Sedimente stellt sie eine bedeutende Lokalität zur Rekonstruktion von lokalen und regionalen Stoffflüssen dar.. Andererseits ist die Gobi-Wüste zugleich auch eine bedeutende Quelle für den überregionalen Staubtransport, da sie aufgrund der klimatischen Bedingungen insbesondere der Erosion durch Ausblasung preisgegeben wird. Vor diesem Hintergrund erfolgten zwischen 2011 und 2014, im Rahmen des BMBF-Verbundprogramms WTZ Zentralasien – Monsundynamik & Geoökosysteme (Förderkennzeichen 03G0814), mehrere deutsch-chinesische Expeditionen in das Ejina-Becken (Innere Mongolei) und das Qilian Shan-Vorland. Im Zuge dieser Expeditionen wurden für eine Bestimmung potenzieller Sedimentquellen erstmals zahlreiche Oberflächenproben aus dem gesamten Einzugsgebiet des Heihe (schwarzer Fluss) gesammelt. Zudem wurden mit zwei Bohrungen im inneren des Ejina-Beckens, ergänzende Sedimentbohrkerne zum bestehenden Bohrkern D100 (siehe Wünnemann (2005)) abgeteuft, um weit reichende, ergänzende Informationen zur Landschaftsgeschichte und zum überregionalen Sedimenttransfer zu erhalten. Gegenstand und Ziel der vorliegenden Doktorarbeit ist die sedimentologisch-mineralogische Charakterisierung des Untersuchungsgebietes in Bezug auf potenzielle Sedimentquellen und Stoffflüsse des Ejina-Beckens sowie die Rekonstruktion der Ablagerungsgeschichte eines dort erbohrten, 19m langen Sedimentbohrkerns (GN100). Schwerpunkt ist hierbei die Klärung der Sedimentherkunft innerhalb des Bohrkerns sowie die Ausweisung von Herkunftssignalen und möglichen Sedimentquellen bzw. Sedimenttransportpfaden. Die methodische Herangehensweise basiert auf einem Multi-Proxy-Ansatz zur Charakterisierung der klastischen Sedimentfazies anhand von Geländebeobachtungen, lithologisch-granulometrischen und mineralogisch-geochemischen Analysen sowie statistischen Verfahren. Für die mineralogischen Untersuchungen der Sedimente wurde eine neue, rasterelektronenmikroskopische Methode zur automatisierten Partikelanalyse genutzt und den traditionellen Methoden gegenübergestellt. Die synoptische Betrachtung der granulometrischen, geochemischen und mineralogischen Befunde der Oberflächensedimente ergibt für das Untersuchungsgebiet ein logisches Kaskadenmodell mit immer wiederkehrenden Prozessbereichen und ähnlichen Prozesssignalen. Die umfangreichen granulometrischen Analysen deuten dabei auf abnehmende Korngrößen mit zunehmender Entfernung vom Qilian Shan hin und ermöglichen die Identifizierung von vier texturellen Signalen: den fluvialen Sanden, den Dünensanden, den Stillwassersedimenten und Stäuben. Diese Ergebnisse können als Interpretationsgrundlage für die Korngrößenanalysen des Bohrkerns genutzt werden. Somit ist es möglich, die Ablagerungsgeschichte der Bohrkernsedimente zu rekonstruieren und in Verbindung mit eigenen und literaturbasierten Datierungen in einen Gesamtkontext einzuhängen. Für das Untersuchungsgebiet werden somit vier Ablagerungsphasen ausgewiesen, die bis in die Zeit des letzten glazialen Maximums (LGM) zurückreichen. Während dieser Ablagerungsphasen kam es im Zuge unterschiedlicher Aktivitäts- und Stabilitätsphasen zu einer kontinuierlichen Progradation und Überprägung des Schwemmfächers. Eine besonders aktive Phase kann zwischen 8 ka und 4 ka BP festgestellt werden, während der es aufgrund zunehmender fluvialer Aktivitäten zu einer deutlich verstärkten Schwemmfächerdynamik gekommen zu sein scheint. In den Abschnitten davor und danach waren es vor allem äolische Prozesse, die zu einer Überprägung des Schwemmfächers geführt haben. Hinsichtlich der mineralogischen Herkunftssignale gibt es eine große Variabilität. Dies spiegelt die enorme Heterogenität der Geologie des Untersuchungsgebietes wider, wodurch die räumlichen Signale nicht sehr stark ausgeprägt sind. Dennoch, können für das Einzugsgebiet drei größere Bereiche deklariert werden, die als Herkunftsgebiet in Frage kommen. Das östliche Qilian Shan Vorland zeichnet sich dabei durch deutlich höhere Chloritgehalte als primäre Quelle für die Sedimente im Ejina-Becken aus. Sie unterscheiden sich insbesondere durch stark divergierende Chloritgehalte in der Tonmineral- und Gesamtmineralfraktion, was das östliche Qilian Shan Vorland als primäre Quelle für die Sedimente im Ejina-Becken auszeichnet. Dies steht in Zusammenhang mit den Grünschiefern, Ophioliten und Serpentiniten in diesem Bereich. Geochemisch deutet vor allem das Cr/Rb-Verhältnis eine große Variabilität innerhalb des Einzugsgebietes an. Auch hier ist es das östliche Vorland, welches aufgrund seines hohen Anteils an mafischen Gesteinen reich an Chromiten und Spinellen ist und sich somit vom restlichen Untersuchungsgebiet abhebt. Die zeitliche aber auch die generelle Variabilität der Sedimentherkunft lässt sich in den Bohrkernsedimenten nicht so deutlich nachzeichnen. Die mineralogisch-sedimentologischen Eigenschaften der erbohrten klastischen Sedimente zeugen zwar von zwischenzeitlichen Änderungen bei der Sedimentherkunft, diese sind jedoch nicht so deutlich ausgeprägt, wie es die Quellsignale in den Oberflächensedimenten vermuten lassen. Ein Grund dafür scheint die starke Vermischung unterschiedlichster Sedimente während des Transportes zu sein. Die Kombination der Korngrößenergebnisse mit den Befunden der Gesamt- und Schwermineralogie deuten darauf hin, dass es zwischenzeitlich eine Phase mit überwiegend äolischen Prozessen gegeben hat, die mit einem Sedimenteintrag aus dem westlichen Bei Shan in Verbindung stehen. Neben der Zunahme ultrastabiler Schwerminerale wie Zirkon und Granat und der Abnahme opaker Schwerminerale, weisen vor allem die heutigen Verhältnisse darauf hin. Der Vergleich der traditionellen Schwermineralanalyse mit der Computer-Controlled-Scanning-Electron-Microscopy (kurz: CCSEM), die eine automatisierte Partikelauswertung der Proben ermöglicht, zeigt den deutlichen Vorteil der modernen Analysemethode. Neben einem zeitlichen Vorteil, den man durch die automatisierte Abarbeitung der vorbereiteten Proben erlangen kann, steht vor allem die deutlich größere statistische Signifikanz des Ergebnisses im Vordergrund. Zudem können mit dieser Methode auch chemische Varietäten einiger Schwerminerale bestimmt werden, die eine noch feinere Klassifizierung und sicherere Aussagen zu einer möglichen Sedimentherkunft ermöglichen. Damit ergeben sich außerdem verbesserte Aussagen zu Zusammensetzungen und Entstehungsprozessen der abgelagerten Sedimente. Die Studie verdeutlicht, dass die Sedimentherkunft innerhalb des Untersuchungsgebietes sowie die ablaufenden Prozesse zum Teil stark von lokalen Gegebenheiten abhängen. Die Heterogenität der Geologie und die Größe des Einzugsgebietes sowie die daraus resultierende Komplexität der Sedimentgenese, machen exakte Zuordnungen zu klar definierten Sedimentquellen sehr schwer. Dennoch zeigen die Ergebnisse, dass die Sedimentzufuhr in das Ejina-Becken in erster Linie durch fluviale klastische Sedimente des Heihe aus dem Qilian Shan erfolgt sein muss. Die Untersuchungsergebnisse zeigen jedoch ebenso die Notwendigkeit einer ergänzenden Bearbeitung angrenzender Untersuchungsgebiete, wie beispielsweise den Gobi-Altai im Norden oder den Beishan im Westen, sowie die Verdichtung der Oberflächenbeprobung zur feineren Auflösung von lokalen Sedimentquellen.
    Type of Medium: Dissertations
    Pages: xi, 186 Seiten , Illustrationen, Diagramme, Karten
    Language: German
    Note: Dissertation, Universität Potsdam, 2020 , INHALTSVERZEICHNIS Zusammenfassung Inhaltsverzeichnis Abbildungsverzeichnis Tabellenverzeichnis Abkürzungsverzeichnis 1 Einleitung 1.1 Einleitung 1.2 Wissenschaftliches Ziel 2 Stand der Forschung 3 Einführung in das Untersuchungsgebiet 3.1 Lage und Physiogeographie 3.2 Geologie 3.3 Geomorphologie 3.3.1 Ejina-Becken 3.3.2 Hexi-Korridor & Qilian Shan 3.4 Klima 4 Methoden 4.1 Probennahme - Strategie und Bohrung 4.2 Probenpräparation 4.3 Tonmineralanalyse 4.4 Schwermineralanalyse 4.4.1 Probenpräparation 4.4.2 Polarisationsmikroskopie 4.4.3 Röntgendiffraktometrie (XRD) 4.4.4 Computer Controlled Scanning Electron Microscopy (CCSEM) 4.5 Gesamtmineralogie (XRD) 4.6 Gesamtgeochemie (XRF) 4.6.1 Röntgenfluoreszenz (Einzelproben Analyse) 4.6.2 Röntgenfluoreszenz (Kernscan) 4.7 Korngrößenanalyse 4.8 Geochronologie 4.9 Räumliche Datenanalyse 5 Ergebnisse 5.1 Oberflächensedimente 5.1.1 Probensätze 5.1.2 Korngrößenanalyse 5.1.3 Gesamtmineralogie (XRD) 5.1.4 Gesamtgeochemie (XRF) 5.1.5 Tonmineralogie 5.1.6 Schwermineralogie 5.2 Bohrkern GN100 5.2.1 Lithostratigraphie 5.2.2 Korngrößenanalyse 5.2.3 Gesamtmineralogie (XRD) 5.2.4 Gesamtgeochemie (XRF) 5.2.5 Tonmineralogie 5.2.6 Schwermineralogie 5.2.7 Datierungen 6 Diskussion 6.1 Korngrößenvariationen und texturelle Signale der Oberflächensedimente 6.2 Mineralogische und geochemische Herkunftssignale der Oberflächensedimente 6.2.1 Gesamtmineralogie (XRD) 6.2.2 Gesamtgeochemie (XRF) 6.2.3 Tonmineralogie 6.2.4 Schwermineralogie 6.3 Heutige Sedimenttransportpfade - Synoptische Betrachtung der aktuellen Oberflächensignale 6.4 Korngrößenvariationen und texturelle Signale der Bohrkernsedimente (GN100) 6.5 Mineralogische und geochemische Herkunftssignale der Bohrkernsedimente (GN100) 6.6 Zeitliche Dimension des Sedimenteintrags - Ablagerungsgeschichte des Bohrkerns GN100 6.6.1 Darstellung der Sedimentherkunft und Ablagerungsgeschichte im Untersuchungsgebiet Schlussfolgerungen Literaturverzeichnis Anhang
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  • 90
    Call number: AWI G5-20-93989
    Type of Medium: Dissertations
    Pages: viii, 139 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2018 , Table of Content I. Abstract II. Deutsche Zusammenfassung 0 Preface 1 Scientific Background 1.1 Paleoenvironmental changes since the gLGM in arid Central Asia and north-western High Asia 1.1.1 Paleoclimatic changes 1.1.2 Lake level fluctuations following climatic changes 1.1.3 Inferred terrestrial vegetation responses to environmental changes and possible human impact 1.2 The role of proxy records in tracing environmental changes 1.2.1 Archives and Proxies investigated in environmental studies in Central Asia 1.2.2 Limnological systems as environmental archives 1.2.3 The multiproxy approach as a tool to decipher environmental change 1.3 Study area 1.4 Material and Method Overview 1.4.1 Field based sampling 1.4.2 Outline of material and methods 1.5 Aim and objectives ofthis thesis 1.6 Thesis outline 1.7 Contribution of the authors 1.7.1 Manuscript I - published 1.7.2 Manuscript II - published 1.7.3 Manuscript III - published 1.7.4 Manuscript IV - in preparation 2 Manuscript I Climatic and limnological changes at Lake Karakul (Tajikistan) during the last ~29 cal ka 2.1 Abstract 2.2 Introduction 2.3 Study Area 2.4 Material and methods 2.4.1 Fieldwork 2.4.2 Laboratory analysis 2.5 Results 2.5.1 Age-depth relationship in core KK12-1 2.5.2 TIC, TOC, TOC/TN, δ18Ocarb and δ13CCarb 2.5.3 Grain-size distribution and results ofend-member modelling 2.5.4 XRF data 2.5.5 Ordination results of sediment parameters 2.6 Discussion 2.6.1 Paleoenvironmental indicators from sediment variables 2.6.2 Implications ofthe Lake Karakul sediment record 2.6.3 Linking lake internal development to climate change 2.7 Conclusions 2.8 Acknowledgements 2.9 Data availability 3 Manuscript II Aquatic macrophyte dynamics in Lake Karakul (Eastern Pamir) over the last 29 cal ka revealed by sedimentary ancient DNA and geochemical analyses of macrofossil remains 3.1 Abstract 3.2 Introduction 3.3 Material and Methods 3.3.1 Sample acquisition and treatment 3.3.2 Genetic approach 3.3.3 Elemental isotopic analyses ofaquatic macrophyte remains 3.4 Results 3.4.1 Macrophyte records along lake depth transects in Lake Karakul 3.4.2 Submerged plant content 3.4.3 Ancient DNA analyses 3.4.4 C, N, δ13C and δ15N of Stuckenia cf. pamirica remains 3.5 Discussion 3.5.1 Assessment of aDNA and chemical aquatic macrophyte data as proxies for the macrophyte composition and the paleo-productivity 3.5.2 Changes of past submerged plant composition and productivity and potential drivers 3.6 Conclusions 3.7 Acknowledgements 3.8 Data Availability 4 Manuscript III Radiocarbon and optical stimulated luminescence dating of sediments from Lake Karakul, Tajikistan 4.1 Abstract 4.2 Introduction 4.3 Regional setting 4.4 Methods 4.4.1 Collection and correlation of cores 4.4.2 Radiocarbon dating 4.4.3 Optically stimulated luminescence (OSL) dating 4.4.4 Establishment ofage-depth model 4.4.5 Investigation of exposed lake sediments 4.5 Results 4.6 Discussion 4.6.1 Recovered sediments and correlation ofcores from Lake Karakul 4.6.2 Age-depth model, and assessment of radiocarbon and OSL age data 4.6.3 Significance ofexposed sediments at section KK13-S1 4.6.4 Implications ofthe chronological data 4.7 Conclusion 4.8 Acknowledgements 5 Manuscript IV Vegetation change in the Eastern Pamir Mountains inferred from Lake Karakul pollen spectra of the last 28 ka 5.1 Abstract 5.2 Introduction 5.3 Study site 5.4 Material and Methods 5.4.1 Sediment cores and chronology 5.4.2 Pollen sample preparation and pollen analyses 5.4.3 Pollen data treatment 5.5 Results 5.5.1 Composite core (KK12-1/2; 27.6 cal ka BP to present) 5.5.2 Short core TAJ-Kar-08-lB 5.6 Discussion 5.6.1 Interpretation of pollen data 5.6.2 Terrestrial vegetation change in the Eastern Pamir Mountains in response to past climate change 5.7 Conclusions 5.8 Acknowledgements 5.9 Data Availability 6 Synthesis 6.1 Proxy evaluation 6.1.1 Age-depth relationship 6.1.2 Limnological proxies 6.1.3 Terrestrial proxies 6.2 The potential of Lake Karakul as archive for long term environmental change in the Eastern Pamir 6.3 Climate and moisture availability changes over time - inferred from sedimentary proxies 6.4 Assessment ofthe aquatic macrophyte composition and paleoproductivity within Lake Karakul 6.5 Inferred terrestrial vegetation changes as responds to climatic changes over the last 28 cal ka 6.6 Comparison inferred regional vegetation, lake internal and lake external variations and changes in climate reconstructed in other studies 6.6.1 Pre- gLGM and global Last Glacial Maximum (27.6 to 19 cal ka BP) 6.6.2 Late glacial 6.6.3 Early to middle Holocene 6.6.4 Middle to late Holocene 6.7 Outlook 7 Appendix 7.1 Supplementary information for Manuscript I 7.2 Supplementary information for Manuscript II 7.3 Supplementary information for Manuscript III 8 References Danksagung Eldesstattliche Erklärung
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  • 91
    Call number: AWI A4-20-93991
    Description / Table of Contents: Over the last decades, the Arctic regions of the earth have warmed at a rate 2–3 times faster than the global average– a phenomenon called Arctic Amplification. A complex, non-linear interplay of physical processes and unique pecularities in the Arctic climate system is responsible for this, but the relative role of individual processes remains to be debated. This thesis focuses on the climate change and related processes on Svalbard, an archipelago in the North Atlantic sector of the Arctic, which is shown to be a "hotspot" for the amplified recent warming during winter. In this highly dynamical region, both oceanic and atmospheric large-scale transports of heat and moisture interfere with spatially inhomogenous surface conditions, and the corresponding energy exchange strongly shapes the atmospheric boundary layer. In the first part, Pan-Svalbard gradients in the surface air temperature (SAT) and sea ice extent (SIE) in the fjords are quantified and characterized. This analysis is based on observational data from meteorological stations, operational sea ice charts, and hydrographic observations from the adjacent ocean, which cover the 1980–2016 period. [...]
    Type of Medium: Dissertations
    Pages: xv, 123 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2020 , CONTENTS 1 Introduction 1.1 Context: A rapidly changing Arctic 1.1.1 Documentation of recent changes in the Arctic 1.1.2 Research relevance 1.1.3 Objective: Svalbard as a hotspot for climate change 1.2 Physical Background 1.2.1 Radiation and surface energy balance 1.2.2 Peculiarities of the Arctic climate system 1.2.3 Role of atmospheric circulation 1.3 The regional setup on Svalbard 2 data and methods 2.1 Data description 2.1.1 Era-Interim atmospheric reanalysis 2.1.2 Svalbard Station Meteorology 2.1.3 Sea Ice Extent 2.1.4 Ocean data products 2.1.5 FLEXTRA Trajectories 2.2 Statistical Methods 2.2.1 Trend estimation 2.2.2 Correlation 2.2.3 Coefficient of Determination 3 state of surface climate parameters: pan-svalbard differences 3.1 Motivation 3.2 Surface air temperature 3.2.1 Annual cycle 3.2.2 Annual temperature range 3.2.3 Long-term trends 3.3 Fjord Sea Ice coverage 3.3.1 Climatology 3.3.2 Sea ice cover trends 3.3.3 Regional classification across Svalbard 3.3.4 Drivers of regional differences 3.4 Discussion and Conclusion 3.5 Current state of climate projections for the Svalbard region 4 Air mass back trajectories 4.1 Methodology 4.2 Winter 4.2.1 Source Regions of Ny-Ålesund Air 4.2.2 Circulation changes 4.2.3 Quantification of Advective Warming 4.3 Summer 4.3.1 Source Regions of Ny-Ålesund Air 4.3.2 Circulation changes 4.3.3 Quantification of advective cooling 4.3.4 Observational Case Study: May/June 2017 4.4 Discussion and Conclusion 5 Changing drivers of the arctic near surface temperature budget 5.1 Winter 5.2 Summer 5.3 Summary 6 Summary and conclusion A Details on calculations A.1 SLP composite Index A.2 Derivation of coefficient of determination A.3 Temperature effect of changing source regions over time B Supplementary figures Bibliography
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  • 92
    Monograph available for loan
    Monograph available for loan
    Toronto : University of Toronto Press
    Call number: AWI G3-21-94408
    Description / Table of Contents: In the Anthropocene, the thawing of frozen earth due to global warming has drawn worldwide attention to permafrost. Contemporary scientists define permafrost as ground that maintains a negative temperature for at least two years. But where did this particular conception of permafrost originate, and what alternatives existed? The Life of Permafrost provides an intellectual history of permafrost, placing the phenomenon squarely in the political, social, and material context of Russian and Soviet science. Pey-Yi Chu shows that understandings of frozen earth were shaped by two key experiences in the Russian Empire and the Soviet Union. On one hand, the colonization and industrialization of Siberia nourished an engineering perspective on frozen earth that viewed the phenomenon as an aggregate physical structure: ground. On the other, a Russian and Soviet tradition of systems thinking encouraged approaching frozen earth as a process, condition, and space tied to planetary exchanges of energy and matter. Aided by the US militarization of the Arctic during the Cold War, the engineering view of frozen earth as an obstacle to construction became dominant. The Life of Permafrost tells the fascinating story of how permafrost came to acquire life as Russian and Soviet scientists studied, named, and defined it.
    Type of Medium: Monograph available for loan
    Pages: viii, 288 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 978-1-4875-0193-8
    Language: English
    Note: CONTENTS Introduction: Historicizing Permafrost Permafrost as a historical object Permafrost in Russian and Soviet history Politics, science, and the environment The life cycle of permafrost Choosing words carefully 1 Mapping The cold of eastern Siberia Birth of a scientific object From Boden-Eis to Eisboden Conclusion 2 Building Colonization and construction Building on frozen earth The soil science of roads The ambiguity of merzlota Conclusion 3 Defining Merzlota as aggregate structure Merzlota as process Personal and institutional politics Vechnaia merzlota in Bolshevik culture Conclusion 4 Adapting From commission to institute Rhetoric of transforming nature Adapting to frozen earth Survival of the systems approach Conclusion 5 Translating Birth of permafrost Criticism and self-criticism From merzlotovedenie to geocryology The dialectic persists Conclusion Epilogue: Resurrecting Acknowledgments Glossary Notes Bibliography Index
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  • 93
    Call number: AWI E2-21-94410
    Description / Table of Contents: Die MOSAiC-Expedition verschiebt die Grenzen des Machbaren und markiert einen historischen Meilenstein der Polarforschung. In den Fußstapfen von Fridtjof Nansens bahnrechender Pionierleistung in den Jahren 1893 bis 1896 mit seinem hölzernen Segelschiff »Fram« bringt sie erstmals einen modernen Forschungseisbrecher im Winter in die direkte Umgebung des Nordpols. 20 Nationen haben sich zusammengetan, um die Geheimnisse des dramatischen Klimawandels der Arktis zu entschlüsseln. Untertützt wird das Flaggschiff der Expedition, der deutsche Forschungseisbrecher »Polarstern«, von sechs weiteren Schiffen und Eisbrechern, Flugzeugen und Helikoptern. Insgesamt fünfhundert Menschen nehmen an den verschiedenen Phasen der Expedition teil. Markus Rex, Kopf des Vorhabens und Expeditionsleiter, berichtet anschaulich vom oft genug dramatischen Verlauf dieser Expedition, aber auch von überwältigend faszinierenden Eindrücken aus der Arktis während der langen winterlichen Polarnacht und während des sommerlichen Polartags. Und er beschreibt die unvorstellbaren Herausforderungen, denen sich die Expeditionsteilnehmer eingefroren im polaren Eis gestellt haben - immer geleitet von dem Ziel, Licht in die Prozesse des globalen Klimawandels zu bringen, der nirgends so auseprägt ist wie in der Arktis.
    Type of Medium: Monograph available for loan
    Pages: 319 Seiten , Illustrationen, Diagramme, Karten
    Edition: 1. Auflage
    ISBN: 9783570104149 , 3570104141
    Language: German
    Note: Inhalt Prolog Teil I: Herbst Kapitel 1: Es beginnt Kapitel 2: Auf dünnem Eis Kapitel 3: Ein neues Zuhause Teil II: Winter Kapitel 4: Allein am Ende der Welt Kapitel 5: Sturm in der Polarnacht Kapitel 6: Weihnachten im Eis Teil III: An Land Kapitel 7: Auf Messers Schneide Teil IV: Frühling Kapitel 8: Wieder im Eis Kapitel 9: Das große Schmelzen Teil V: Sommer Kapitel 10: Hochsommer auf dem Eis Kapitel 11: Der Nordpol - und eine neue Scholle Kapitel 12: Es geht nach Hause Epilog Dank Register Bildnachweis
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  • 94
    Call number: AWI E2-21-94415
    Description / Table of Contents: Noch nie haben Forschende das Meereis der Arktis so umfassend untersuchen können, wie auf der internationalen MOSAiC-Expedition des Forschungseisbrechers Polarstern. Ein Jahr lang ist das Schiff mit dem Eis durch die zentrale Arktis getrieben; ein Jahr lang haben die Männer und Frauen das Eis mithilfe modernster Technik unter die Lupe genommen. Welche Herausforderungen es dabei zu meistern galt und was sie herausgefunden haben im polaren Hotspot des Klimawandels, erzählen sie in zehn DriftStories, die dieser Band vereint. Faszinierende Arktisforschung zum Anfassen – präsentiert von meereisportal.de.
    Type of Medium: Monograph available for loan
    Pages: 106 Seiten , Illustrationen
    ISBN: 978-3-9822680-0-2
    Language: German
    Note: Inhaltsverzeichnis Ausgangspunkt einer Jahrhundertreise Ermittlungen auf viel zu dünnem Eis Für einen schärferen Blick aus dem All Beben und Barrikaden Glitzernde Wolken unter dem Eis Ein heißer Streifen Eis Schnee, die unbekannte Größe Das Omen des ersten Schneeballs Die vielen Gesichter der Kälte Algen in der Arktis: Nichts scheint unmöglich Wiedersehen am Ausgangstor der Arktis Technik-Container Impressum/Bildnachwei
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  • 95
    Call number: AWI A6-21-94541
    Description / Table of Contents: Stratospheric variability is one of the main potential sources for sub-seasonal to seasonal predictability in mid-latitudes in winter. Stratospheric pathways play an important role for long-range teleconnections between tropical phenomena, such as the quasi-biennial oscillation (QBO) and El Niño-Southern Oscillation (ENSO), and the mid-latitudes on the one hand, and linkages between Arctic climate change and the mid-latitudes on the other hand. In order to move forward in the field of extratropical seasonal predictions, it is essential that an atmospheric model is able to realistically simulate the stratospheric circulation and variability. The numerical weather prediction (NWP) configuration of the ICOsahedral Non-hydrostatic atmosphere model ICON is currently being used by the German Meteorological Service for the regular weather forecast, and is intended to produce seasonal predictions in future. This thesis represents the first extensive evaluation of Northern Hemisphere stratospheric winter circulation in ICON-NWP by analysing a ...
    Type of Medium: Dissertations
    Pages: viii, 119 Seiten , Illustrationen, Diagramme, Karten
    Language: English
    Note: Dissertation, Universität Potsdam, 2020 , Contents1 Introduction 1.1 Motivation: Seasonal prediction 1.2 The new atmosphere model ICON 1.3 Research questions 2 Theoretical background 2.1 Fundamentals of atmospheric circulation 2.1.1 Primitive equations 2.1.2 The global energy budget 2.1.3 Baroclinic instability 2.1.4 Vertical structure of the atmosphere 2.2 Stratospheric dynamics 2.2.1 Circulation patterns 2.2.2 Atmospheric waves 2.2.3 Sudden stratospheric warmings 2.2.4 Quasi-biennial oscillation 2.3 Atmospheric Teleconnections 2.3.1 NAM, NAO and PNA 2.3.2 El Niño-Southern Oscillation 2.3.3 Arctic-midlatitude linkages 3 Atmospheric model and methods of analysis 3.1 Atmospheric model ICON-NWP 3.1.1 Model description 3.1.2 Experimental setup 3.2 Reanalysis data ERA-Interim 3.3 Methods of analysis 3.3.1 NAM index for stratosphere–troposphere coupling 3.3.2 Stratospheric warmings 3.3.3 ENSO index and composites 3.3.4 Bias and error estimation 3.3.5 Statistical significance 4 Results 4.1 Evaluation of seasonal experiments with ICON-NWP 4.1.1 Tropospheric circulation 4.1.2 Stratospheric circulation 4.2 Effect of gravity wave drag parameterisations 4.2.1 Stratospheric effects 4.2.2 Effects on stratosphere-troposphere coupling 4.2.3 Tropospheric effects 4.3 Low latitudinal influence on the stratospheric polar vortex 4.3.1 Quasi-biennial oscillation 4.3.2 El Niño-Southern Oscillation 4.4 Arctic-midlatitude linkages 4.4.1 Tropospheric processes 4.4.2 Stratospheric pathway 4.4.3 Sea ice sensitivity experiment 5 Discussion and outlook Bibliography Appendix
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  • 96
    Call number: AWI A3-20-93434-2
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 2
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,2
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 97
    Series available for loan
    Series available for loan
    Offenbach/M : Deutscher Wetterdienst, Fachinformationsstelle und Deutsche Meteorologische Bibliothek
    Associated volumes
    Call number: ZSP-652-103
    In: Promet, Heft 103
    Type of Medium: Series available for loan
    Pages: 115 Seiten , Illustrationen, Diagramme, Karten , 30 cm
    Edition: Redaktionsschluss: 29.09.2020
    ISBN: 9783881485227
    ISSN: 0340-4552 , 2194-5950
    Series Statement: Promet Heft 103
    Language: German
    Note: Inhalt Beitrag Vorwort „Zu diesem Heft“ / M. SPRENGER Zyklonen als Stürme von großer sozioökonomischer Relevanz 1 Vorhersage von Zyklonen / F. PANTILLON 2 Clustering von Zyklonen / M. KARREMANN, J. PINTO Struktur und Entwicklung einzelner Zyklonen 3 Die Vermessung von Zyklonen / A. SCHÄFLER, F. EWALD, M. RAUTENHAUS 4 Zyklonen und Fronten / S. SCHEMM, M. SPRENGER 5 Zyklonen als Dauerbrenner in der Geschichte der Meteorologie / H. DAVIES 6 Die PV-Struktur außertropischer Zyklonen / M. BOETTCHER, H. WERNLI 7 Warm Conveyor Belts / H. BINDER, E. MADONNA 8 Von der tropischen zur außertropischen Zyklone / M. RIEMER, C. GRAMS, J. KELLER Zyklonen früher und in Zukunft 9 Zyklonen und Paläoklima / C. RAIBLE, P. LUDWIG, M. MESSMER 10 Zyklonen in einem sich ändernden Klima / U. ULBRICH, G. LECKEBUSCH Buchbesprechung Examina im Jahr 2019 Examina im Jahr 2018
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  • 98
    Call number: AWI G5-22-94780
    Type of Medium: Dissertations
    Pages: xxi, 201 Seiten , Illustrationen, Diagramme
    Language: English
    Note: Dissertation, Universität Potsdam, 2021 , Contents List of Figures List of Tables I Preamble 1 Introduction 1.1.1 The Journey from Weather to Climate 1.1.2 The Climate Background 1.1.3 Pollen as Quantitative Indicators of Past Changes 1.2 Overview and Aims of Manuscripts 1.2.1 List of Manuscripts 1.2.2 Short Summaries of the Manuscripts 1.3 Author Contributions to the Manuscripts II Manuscripts 2 Comparing estimation of techniques for temporal Scaling 2.1 Introduction 2.2 Data and Methods 2.2.1 Scaling estimation methods 2.2.2 Evaluation of the estimators 2.2.3 Data 2.3 Results 2.3.1 Effect of Regular and Irregular Sampling 2.3.2 Effect of Time series length 2.3.3 Application to database 2.4 Discussion 2.5 Conclusions 3 Land temperature variability driven by oceans at millennial timescales 4 Variability of surface climate in simulations of past and future 4.1 Introduction 4.2 Data and Method 4.2.1 Model simulations 4.2.2 The Last Glacial Maximum experiment 4.2.3 The mid Holocene experiment (midHolocene) 4.2.4 The warming experiments 1pctCO2 and abrupt4xCO2 4.2.5 Preprocessing of model simulations 4.2.6 Comparisons across the ensemble 4.2.7 Diagnosing variability changes 4.2.8 Changes in precipitation extremes 4.2.9 Timescale-dependence of the variability changes 4.3 Results 4.3.1 Hydrological sensitivity across the ensemble 4.3.2 Changes in local interannual variability 4.3.3 Changes in modes of variability 4.3.4 Circulation patterns underlying extratropical precipitation extremes 4.3.5 Changes in. the spectrum of variability 4.4 Discussion 4.4.1 Changes in climate variability with global mean temperature 4.4.2 Temperature vs. precipitation scaling 4.4.3 Comparison to climate reconstructions and observations 4.4.4 Limitations 4.5 Conclusions 5 Holocene vegetation variability in the Northern Hemisphere 5.1 Introduction 5.2 Data and Methods 5.2.1 Pollen Database 5.2.2 Principal Component Analysis 5.2.3 Timescale-dependent Estimates of Variability 5.2.4 Biome Classification 5.3 Results 5.3.1 General Vegetation Variability Analysis 5.3.2 Comparison of Forested and Open Land Vegetations 5.3.3 Comparison of Broadleaf and Needleleaf Fore ts 5.3.4 Comparison of Temperate and Boreal Coniferous Forests 5.3.5 Comparison of Evergreen and Deciduous Boreal Forests 5.4 Discussion 5.5 Conclusion III Postamble 6 General discussion and conclusion 6.1 Overview 6.2 Timescale-Dependent Estimates of Variability 6.3 Climate and Vegetation Variabilities in the Holocene 6.4 Implications for the 21th Century 6.5 Outlook IV Appendix A Supplementary figures from "Comparing estimation techniques for temporal scaling in paleo-climate timeseries" A.1 Block Average Results A.2 First-Order Correction for the Effect of Interpolation A.3 Change in Bias and Standard Deviation B Methods and supplementary information from "Land temperature variability driven by oceans at millennial timescales" B.1 Methods B.1.1 Reconstructions B.1.2 Significance Testing B.1.3 Testing for Anthropogenic Impacts B.1.4 Instrumental Data B.1.5 Model Data B.1.6 Spectral Estimates B.1.7 Variance Ratios B.1.8 Sub-Decadal Variability Binning B.1.9 Correlation B.1.10 Moran's I B.2 Supplementary Information B.2.1 Tree Ring Data Analysis B.2.2 Energy-Balance Equations B.3 Extended Data Figures C Supplementary figures from "Variability of surface climate in simulations of past and future" D Supplementary figures from "Characterization of holocene vegetation variability in the Northern Hemisphere" Bibliography
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  • 99
    Monograph available for loan
    Monograph available for loan
    Sosnowiec : Wydział Nauk o Ziemi Uniwersytet Śląski | Warszawa : Instytut Geofizyki Polskiej Akademii Nauk | Sopot : Instytut Oceanologii Polskiej Akademii Nauk
    Call number: AWI S6-22-94809
    Type of Medium: Monograph available for loan
    Pages: 101, [3] Seiten , Illustrationen , 22x22 cm
    Language: English
    Note: Table of Contents INTRODUCTION 1. The Centre for Polar Studies 2. The Centre in the context of Polish and international polar research 3. Development and achievements of the Centre for Polar Studies Underwater acoustic signatures od glacier calving Svalbard reveals a new island Freshwater in a salty fjord Between genetics and palaeontology: ancient DNA in palaeoceanographical research Influence of glacial disturbance and food availability on organisms size in Kongsfjorden and Hornsund fjords Message in a stainless steel bottle thrown into deep geological time 4. Technical facilities and infrastructure for polar research 5. Interdisciplinary Polar Studies Foundations of ISP Profiles of doctoral thesis 6. Exploration of Polar and Mountain Regions - a new speciality of MSc studies at the Faculty of Earth Sciences, University of Silesia 7. Science communication and dissemination 8. Towards the future
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  • 100
    Call number: AWI G3-20-94096
    In: Hamburger Beiträge zur physischen Geographie und Landschaftsökologie, Heft 24
    Type of Medium: Series available for loan
    Pages: xiii, 336 Seiten , Illustrationen, Karten
    ISSN: 1866-170X
    Series Statement: Hamburger Beiträge zur physischen Geographie und Landschaftsökologie Heft 24
    Language: German
    Note: Inhaltsverzeichnis 1. Einführung 2. Wissenschaftlicher Hintergrund 3. Physiogeographische Ausstattung des Varanger-Gebietes (Varanger-Halbinsel und Küstenregion Südvarangers) 3.1. Relief 3.2. Geologisch-tektonische Entwicklung bis zum Quartär 3.3. Festgesteine 3.3.1. Varanger-Halbinsel 3.3.1.1. Tanafjord-Varangerfjord-Region 3.3.1.2. Barentssee-Region 3.3.1.3. Schichtdeformationen und Faltenbildungen 3.3.1.4. Ganggesteine (Intrusivgesteine) 3.3.2. Südvaranger 3.4. Quartärgeologische Entwicklung 3.4.1. Pleistozän 3.4.1.1. Glaziation 3.4.1.2. Deglaziation 3.4.2. Holozän 3.5. Pleistozäne und holozäne Lockersedimente 3.6. Klima 3.7. Permafrostboden 3.8. Vegetation 3.9. Böden 4. Periglaziäre Formen, Ablagerungen und Prozesse 4.1. Blockfelder 4.1.1. Verbreitung 4.1.2. Merkmale 4.1.3. Genese 4.1.4. Altersstellung 4.2. Sturzschutthalden 4.3. Kleinformen der Gesteinsverwitterung und Detritusverlagerung 4.4. Formen des Bodenfließens 4.4.1. Fließerde- und Wanderschuttdecken 4.4.2. Rasenloben und -stufen 4.4.3. Schuttloben und -stufen 4.4.4. Wander- und Bremsblöcke 4.5. Formen der Bodenmusterung 4.5.1. Palsas 4.5.2. Lithalsas 4.5.3. Pounus 4.5.4. Thufur 4.5.5. Mudpits 4.5.6. Fossile Eiskeilpolygone 4.5.7. Strukturböden 4.6. Formen der Nivation und Kryoplanation 4.6.1. Nivationswannen und -nischen 4.6.2. Kryoplanationsterrassen und Kryopedimente 4.7. Formen der Windwirkung 4.7.1. Windschliffe und Polituren 4.7.2. Steinpanzer 4.7.3. Flugsanddecken und Dünen 4.7.4. Rasenkanten und -kliffs 5. Exkursionsvorschläge zur glaziären und periglaziären Landschaftsentwicklung 5.1. Anfahrt und Logistik 5.2. Fahrstrecken und Wanderexkursionen (W) 5.2.1. Route 1: Tana Bru – Skiipagurra – Varangerbotn – Nesseby –Vestre Jakobselv – Vadsö (W1: Nattfjelltal) – Skallelv – Komagvaer – Kiberg – Svartnes (W2: Oksevatn-See) – Persfjord – Sandfjord – Hamningberg – Sandfjordtal (W3: Sylteviktal) 5.2.2. Route 2: Tana Bru – Birkestrand (W4: Raudberg) – Höyholmen (W5: Stangenestind) – Leirpollen – Faccabaelcåkka (W6: Hanglefjell) – Gednje – Kongsfjordtal (W7: Bryggarital) – Kongsfjord – Sandfjord (W8: Sandfjordfjell) – Berlevåg – Store Molvik 5.2.3. Route 3: Gednje – Oarduskaidi (W9: Basecaerro-Storklöftfjell) – Raudsandvatna-Seen (W10: Buktkjöl-Höhenzug) – Båtsfjord – Syltefjord 5.2.4. Route 4: Tana Bru – Skiipagurra – Varangerbotn – Karlebotn (W11: Bigganjarga) – Grasbakken (W12: Juovlagurguolba) – Gandvik – Brannsletta – Bugöyfjord – Neiden – Näätämö 5.2.5. Route 5: Tana Bru – Skiipagurra – Varangerbotn – Karlebotn (W13: Roetkaguolba-Vesterelvvatn-See) 6. Zusammenfassung 7. Schlussfolgerungen und Ausblick 8. Literaturverzeichnis 9. Kartenverzeichnis 9.1. Geologische Karten 9.2. Vegetationsgeographische Karte 9.3. Topographische Karten 10. Luftbildverzeichnis
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