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  • Books  (102)
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  • Books  (102)
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  • Printed Books(GFZ-OPAC)  (102)
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  • 1
    Call number: 1.2/N 07.0275
    Type of Medium: Monograph available for loan
    Pages: XX, 1068 S.
    Edition: 2., korr. Nachdruck
    ISBN: 3540679081
    Classification:
    Geography and Geomorphology
    Location: Reading room
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  • 2
    Monograph available for loan
    Monograph available for loan
    Middlesex : Penguin Books
    Call number: M 97.0180
    Type of Medium: Monograph available for loan
    Pages: xii, 237 S.
    Edition: Revised ed.
    Classification:
    Geography and Geomorphology
    Language: English
    Location: Upper compact magazine
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  • 3
    Monograph available for loan
    Monograph available for loan
    London : Arnold
    Call number: M 97.0181
    Type of Medium: Monograph available for loan
    Pages: ix, 342 S.
    Classification:
    Geography and Geomorphology
    Language: English
    Location: Upper compact magazine
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  • 4
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: M 09.0160
    In: Developments in soil science
    Description / Table of Contents: A guide to preparing Digital Elevation Models (DEM) for analysis and extracting land-surface parameters and objects from DEMs through a variety of software. It offers instructions on applying parameters and objects in soil, agricultural, environmental and earth sciences.Geomorphometry is the science of quantitative land-surface analysis. It draws upon mathematical, statistical, and image-processing techniques to quantify the shape of earth's topography at various spatial scales. The focus of geomorphometry is the calculation of surface-form measures (land-surface parameters) and features (objects), which may be used to improve the mapping and modelling of landforms to assist in the evaluation of soils, vegetation, land use, natural hazards, and other information. This book provides a practical guide to preparing Digital Elevation Models (DEM) for analysis and extracting land-surface parameters and objects from DEMs through a variety of software.It further offers detailed instructions on applying parameters and objects in soil, agricultural, environmental and earth sciences. This is a manual of state-of-the-art methods to serve the various researchers who use geomorphometry. Soil scientists will use this book to further learn the methods for classifying and measuring the chemical, biological, and fertility properties of soils and gain a further understaing of the role of soil as a natural resource.Geologists will find value in the instruction this book provides for measuring the physical features of the soil such as elevation, porosity, and structure which geologists use to predict natural disasters such as earthquakes, volcanoes, and flooding.Technical details on a variety of software packages allow researchers to solve real-life mapping issues. This book provides soil and agronomy researchers best practice techniques for soil data analysis to assist in enhanced land-use and planning. It offers geologists essential tactics for better environmental management by providing a comprehensive analysis of the physical features of soil. The companion website includes access to the latest technological advancements previously unpublished in any other comprehensive source: geomorphometry software, DEM data sources, and applications.
    Type of Medium: Monograph available for loan
    Pages: xxix, 765 S.
    ISBN: 0123743451 , 978-0-12-374345-9
    Series Statement: Developments in soil science 33
    Classification:
    Geography and Geomorphology
    Location: Upper compact magazine
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  • 5
    Call number: S 00.0063(90)
    In: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften ; 90
    Type of Medium: Series available for loan
    Pages: 208 Seiten , Illustrationen , 30 cm
    ISBN: 3510492382 , 9783510492381
    Series Statement: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften Heft 90
    Classification:
    Geography and Geomorphology
    Language: German
    Location: Lower compact magazine
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  • 6
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: M 18.91647
    Description / Table of Contents: Provides a definitive overview of the global drivers of high-mountain cryosphere change and their implications for people across high-mountain regions
    Type of Medium: Monograph available for loan
    Pages: xii, 363 Seiten
    ISBN: 9781107065840
    Classification:
    Geography and Geomorphology
    Language: English
    Note: Introduction: human-environment dynamics in the high-mountain cryosphere; References; Part I Global drivers; 2 Influence of climate variability and large-scale circulation on the mountain cryosphere; 2.1 Introduction; 2.2 European mountains; 2.3 North American Cordillera; 2.4 Tibetan Plateau and the surrounding high-mountain ranges; 2.5 The tropical Andes; 2.6 Mt. Kilimanjaro: a case study from East Africa; 2.7 Conclusions; Acknowledgements; References. 3 Temperature, precipitation and related extremes in mountain areas3.1 Introduction; 3.2 Basic characteristics of near surface temperature in mountain topography; 3.2.1 Altitude dependence of 2m temperature; 3.2.2 Altitude dependence of daily temperature anomalies; 3.2.3 The relation between surface air pressure and 2m temperature; 3.3 Temperature extremes; 3.4 Precipitation patterns in mountain areas; 3.4.1 Measuring and monitoring precipitation; 3.5 Precipitation extremes; 3.5.1 Selected gridded data products; 3.5.1.1 Reanalyses; 3.5.1.2 Combined observations. 3.5.1.3 Interpolated rain-gauge station data3.5.2 Comparison and discussion of the gridded data products; 3.6 Conclusions; Acknowledgments; References; 4 Snow and avalanches; 4.1 Introduction; 4.1.1 Snow cover; 4.1.2 Snow avalanche hazard and risk; 4.2 Environmental change; 4.2.1 Climate change and mountain snow cover; 4.2.2 Effects on snow avalanches; 4.3 Socio-economic change; 4.3.1 Drivers of socio-economic change; 4.3.2 Effects on snow avalanche risk; 4.3.2.1 Temporal dynamics of socio-economic changes; 4.3.2.2 Spatial dynamics of socio-economic changes; 4.4 Conclusions; References. 5 The frozen frontier: the extractives super cycle in a time of glacier recession5.1 Introduction; 5.2 The icy edge of climate change; 5.3 The icy edge of the global extractives super cycle; 5.4 New mountains of mines and the frozen north; 5.5 Extending the extractives complex into the cryosphere; 5.6 Liquid relations and stratified societies; 5.7 The frigid fringe: extractive bio-futures and the freezing depths; 5.8 Conclusion; References; 6 Cultural values of glaciers; 6.1 Introduction; 6.2 Three cases in the Alps, the Andes, and the North Cascades. 6.3 Understanding the cultural values of glaciers6.4 Case study 1: Stilfs, South Tirol, Italian Alps; 6.4.1 The role of glaciers for community, identity, and self-reliance in Stilfs; 6.5 Case study 2: Siete Imperios, Cordillera Blanca, Peru; 6.5.1 The role of glaciers and mountains for community, identity, and self-reliance in Siete Imperios; 6.6 Case study 3: Glacier and Concrete, North Cascades, USA; 6.6.1 The role of glaciers and mountains for community, identity, and self-reliance in Glacier and Concrete; 6.7 Discussion and conclusions; Acknowledgments; References; Part II Processes. 7 Implications for hazard and risk of seismic and volcanic responses to climate change in the high-mountain cryosphere.
    Location: Upper compact magazine
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  • 7
    Call number: 9/M 07.0421(440)
    In: Geological Society Special Publication
    Description / Table of Contents: Abstract Alluvial and fluvial fans are the most widespread depositional landform bordering the margins of highland regions and actively subsiding continental basins, across a broad spectrum of tectonic and climatic settings. They are significant to the local morphodynamics of mountain regions and also to the evolution of sediment-routing systems, affecting the propagation and preservation of stratigraphic signals of environmental change over vast areas. The volume presents case studies discussing the geology and geomorphology of alluvial and fluvial fans from both active systems and ancient ones preserved in the stratigraphic record. It brings together case studies from a range of continents, climatic and tectonic settings, some introducing innovative monitoring and analysis techniques, and it provides an overview of current debates in the field. This volume will be of particular interest to geologists, geomorphologists, sedimentologists and the general reader with an interest in Earth science.
    Type of Medium: Monograph available for loan
    Pages: 353 Seiten , Illustationen, farbige Abbildungen
    ISBN: 978-1-78620-267-3
    Series Statement: Geological Society Special Publication 440
    Classification:
    Geography and Geomorphology
    Language: English
    Location: Reading room
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  • 8
    Call number: M 17.90865
    Type of Medium: Monograph available for loan
    Pages: XI, 394 S. : , Ill., graph. Darst., Kt.
    Edition: 3., verb. Aufl.
    ISBN: 3935638264
    Classification:
    Geography and Geomorphology
    Language: German
    Location: Upper compact magazine
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  • 9
    Call number: S 00.0063(42)
    In: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften
    Type of Medium: Series available for loan
    Pages: 109 S. , Ill., graph. Darst.
    ISBN: 3932537386 , 978-3-932537-38-7
    Series Statement: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 42
    Classification:
    Geography and Geomorphology
    Location: Lower compact magazine
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  • 10
    Monograph available for loan
    Monograph available for loan
    Chichester : Wiley
    Call number: AWI G3-08-0013 ; 13/M 13.0053 ; AWI G3-22-5374
    Description / Table of Contents: The periglacial environment, Third Edition, provides an authoritative overview of the world's cold, non-glacial environments. Emphasis is placed upon the North American and Eurasian polar lowlands. Examples are also drawn from Antarctica, the Qinghai-Xizang (Tibet) Plateau, and the northern mid-latitudes. [...] The Third Edition continues to be a personal interpretation of the frost-induced conditions, geomorphic processes, and landforms that typify periglacial environments. The text is divided into four parts. Part One discusses the periglacial concept and its interactions with geomorphology, geocryology and Quaternary science. It also outlines the range and variability of periglacial climates and the degree to which landscapes are in geomorphic equilibrium with prevailing periglacial conditions. Part Two describes present-day terrain that is either underlain by permafrost or experiencing intense frost action. The roles played by cryogenic weathering, ground ice, mass wasting, running water, wind action, snow and ice, and coastal processes are systematically analysed. Part Three summarizes evidence for the existence of periglacial conditions during the cold periods of the Pleistocene. Special reference is made to the mid-latitudes of Europe and North America. Part Four illustrates the geotechnical problems associated with human activity and resource development in periglacial environments, and discusses the potential impact of global climate change in the northern high latitudes.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 458 Seiten , Illustrationen
    Edition: Third edition
    ISBN: 9780470865897
    Classification:
    Geography and Geomorphology
    Language: English
    Note: Contents: Preface to First Edition. - Preface to Second Edition. - Preface to Third Edition. - Acknowledgments. - Part I The Periglacial Domain. - 1 Introduction. - 1.1 The Periglacial Concept. - 1.2 Disciplinary Considerations. - 1.2.1 The Growth of Geocryology. - 1.2.2 The Changing Nature of Quaternary Science. - 1.2.3 Modern Periglacial Geomorphology. - 1.3 The Growth of Periglacial Knowledge. - 1.4 The Periglacial Domain. - 1.5 The Scope of Periglacial Geomorphology. - 1.5.1 Permafrost-Related Processes and Landforms. - 1.5.2 Azonal Processes and Landforms. - 1.5.3 Paleo-Environmental Reconstruction. - 1.5.4 Applied Periglacial Geomorphology. - Advanced Reading. - Discussion Topics. - 2 Periglacial Landscapes?. - 2.1 Introduction. - 2.2 Proglacial, Paraglacial or Periglacial?. - 2.3 Unglaciated Periglacial Terrain. - 2.3.1 Beaufort Plain, Northwest Banks Island, Arctic Canada. - 2.3.2 Barn Mountains, Northern Interior Yukon Territory, Canada. - 2.4 Relict Periglacial Landscapes. - 2.4.1 Chalk Uplands, Southern England and Northern France. - 2.4.2 Pine Barrens, Southern New Jersey, Eastern USA. - 2.5 Conclusions. - Advanced Reading. - Discussion Topics. - 3 Periglacial Climates. - 3.1 Boundary Conditions. - 3.2 Periglacial Climates. - 3.2.1 High Arctic Climates. - 3.2.2 Continental Climates. - 3.2.3 Qinghai-Xizang (Tibet) Plateau. - 3.2.4 Alpine Climates. - 3.2.5 Climates of Low Annual Temperature Range. - 3.2.6 Antarctica: A Special Case. - 3.3 Ground Climates. - 3.3.1 The n-Factor. - 3.3.2 The Thermal Offset. - 3.4 Periglacial Climates and the Cryosphere. - Advanced Reading. - Discussion Topics. - Part II Present-Day Periglacial Environments. - 4 Cold-Climate Weathering. - 4.1 Introduction. - 4.2 Ground Freezing. - 4.2.1 The Freezing Process. - 4.2.2 Ice Segregation. - 4.2.3 The Frozen Fringe. - 4.2.4 Frost Heave. - 4.3 Freezing and Thawing. - 4.4 The Ground-Temperature Regime. - 4.4.1 The Seasonal Regime. - 4.4.2 Short-Term Fluctuations. - 4.5 Rock (Frost?) Shattering. - 4.5.1 Frost Action and Ice Segregation. - 4.5.2 Frost Weathering Models. - 4.5.3 Insolation Weathering and Thermal Shock. - 4.5.4 Discussion and Perspective. - 4.6 Chemical Weathering. - 4.6.1 General. - 4.6.2 Solution and Karstification. - 4.6.3 Salt Weathering. - 4.7 Cryogenic Weathering. - 4.8 Cryobiological Weathering. - 4.9 Cryopedology. - 4.9.1 Cryosols. - 4.9.2 Soil Micromorphology. - Advanced Reading. - Discussion Topics. - 5 Permafrost. - 5.1 Introduction. - 5.1.1 Definition. - 5.1.2 Moisture and Ice within Permafrost. - 5.2 Thermal and Physical Properties. - 5.2.1 The Geothermal Regime. - 5.2.2 Physical Properties. - 5.2.3 Thermal Properties. - 5.3 How Does Permafrost Aggrade?. - 5.3.1 General Principles. - 5.3.2 The Illisarvik Drained-Lake Experiment. - 5.4 Distribution of Permafrost. - 5.4.1 Latitudinal Permafrost. - 5.4.2 Alpine (Mountain) Permafrost. - 5.4.3 Montane Permafrost of Central Asia and China. - 5.5 Relict Permafrost. - 5.5.1 Sub-Sea Permafrost. - 5.5.2 Relict (Terrestrial) Permafrost. - 5.6 Permafrost Hydrology. - 5.6.1 Aquifers. - 5.6.2 Hydrochemistry. - 5.6.3 Groundwater Icings. - 5.7 Permafrost and Terrain Conditions. - 5.7.1 Relief and Aspect. - 5.7.2 Rock Type. - 5.7.3 Vegetation. - 5.7.4 Snow Cover. - 5.7.5 Fire. - 5.7.6 Lakes and Surface Water Bodies. - 5.8 The Active Layer. - 5.8.1 The Transient Layer. - 5.8.2 The Stefan Equation. - 5.8.3 Active-Layer Thermal Regime. - Advanced Reading. - Discussion Topics. - 6 Surface Features of Permafrost. - 6.1 Introduction. - 6.2 Thermal-Contraction-Crack Polygons. - 6.2.1 Coefficients of Thermal Expansion and Contraction. - 6.2.2 Ice, Sand, and Soil Wedges. - 6.2.3 Development of the Polygon Net. - 6.2.4 Polygon Morphology. - 6.2.5 Controls Over Cracking. - 6.2.6 Climatic Significance. - 6.3 Organic Terrain. - 6.3.1 Palsas. - 6.3.2 Peat Plateaus. - 6.4 Rock Glaciers. - 6.4.1 Creeping Permafrost. - 6.4.2 Types and Distribution. - 6.4.3 Origin. - 6.5 Frost Mounds. - 6.5.1 Perennial-Frost Mounds. - 6.5.2 Hydraulic (Open) System Pingos. - 6.5.3 Hydrostatic (Closed) System Pingos. - 6.5.4 Other Perennial-Frost Mounds. - 6.5.5 Seasonal-Frost Mounds. - 6.5.6 Hydrolaccoliths and Other Frost-Induced Mounds. - 6.6 Active-Layer Phenomena. - 6.6.1 Bedrock Heave. - 6.6.2 Needle Ice. - 6.6.3 Cryoturbation and Frost Heave. - 6.6.4 Frost Sorting. - 6.6.5 Patterned Ground. - Advanced Reading. - Discussion Topics. - 7 Ground lce. - 7.1 Introduction. - 7.2 Classification. - 7.2.1 Pore Ice. - 7.2.2 Segregated Ice. - 7.2.3 Intrusive Ice. - 7.2.4 Vein Ice. - 7.2.5 Other Types of Ice. - 7.3 Ice Distribution. - 7.3.1 Amounts. - 7.3.2 Distribution with Depth. - 7.3.3 Ice in Bedrock. - 7.3.4 Ice in Unconsolidated Sediments. - 7.4 Cryostratigraphy and Cryolithology. - 7.4.1 Cryostructures, Cryotextures, and Cryofacies. - 7.4.2 Epigenetic and Syngenetic Cryostructures. - 7.4.3 Thaw Unconformities. - 7.4.4 Ice Crystallography. - 7.4.5 Ice Geochemistry. - 7.4.6 Cryostratigraphy and Past Environments. - 7.5 Ice Wedges. - 7.5.1 Epigenetic Wedges. - 7.5.2 Syngenetic Wedges. - 7.5.3 Anti-Syngenetic Wedges. - 7.6 Massive Ice and Massive-Icy Bodies. - 7.6.1 Nature and Extent. - 7.6.2 Intra-Sedimental Ice. - 7.6.3 Buried Glacier Ice. - 7.6.4 Other Mechanisms. - Advanced Reading. - Discussion Topics. - 8 Thermokarst. - 8.1 Introduction. - 8.2 Causes of Thermokarst. - 8.2.1 General. - 8.2.2 Specific. - 8.3 Thaw-Related Processes. - 8.3.1 Thermokarst Subsidence. - 8.3.2 Thermal Erosion. - 8.3.3 Other Processes. - 8.4 Thermokarst Sediments and Structures. - 8.4.1 Involuted Sediments. - 8.4.2 Retrogressive-Thaw-Slumps and Debris-Flow Deposits. - 8.4.3 Ice-Wedge Pseudomorphs and Composite-Wedge Casts. - 8.4.4 Ice, Silt, Sand, and Gravel Pseudomorphs. - 8.5 Ice-Wedge Thermokarst Relief. - 8.5.1 Low-Centered Polygons. - 8.5.2 High-Centered Polygons. - 8.5.3 Badland Thermokarst Relief. - 8.6 Thaw Lakes and Depressions. - 8.6.1 Morphology. - 8.6.2 Growth and Drainage. - 8.6.3 Oriented Thaw Lakes. - 8.7 Thermokarst-Affected Terrain. - 8.7.1 The Lowlands of Central and Northern Siberia. - 8.7.2 The Western North American Arctic. - 8.8 Human-Induced Thermokarst. - 8.8.1 Causes. - 8.8.2 Case Studies. - Advanced Reading. - Discussion Topics. - 9 Hillslope Processes and Slope Evolution. - 9.1 Introduction. - 9.2 Slope Morphology. - 9.2.1 The Free-Face Model. - 9.2.2 Rectilinear Debris-Mantled Slopes. - 9.2.3 Convexo-Concavo Debris-Mantled Slopes. - 9.2.4 Pediment-Like Slopes. - 9.2.5 Stepped Profiles. - 9.3 Mass Wasting. - 9.4 Slow Mass-Wasting Processes. - 9.4.1 Solifluction. - 9.4.2 Frost Creep. - 9.4.3 Gelifluction. - 9.4.4 Solifluction Deposits and Phenomena. - 9.5 Rapid Mass Wasting. - 9.5.1 Active-Layer-Detachment Slides. - 9.5.2 Debris Flows, Slushflows, and Avalanches. - 9.5.3 Rockfall. - 9.6 Slopewash. - 9.6.1 Snow-Bank Hydrology. - 9.6.2 Surface and Subsurface Wash. - 9.7 Frozen and Thawing Slopes. - 9.7.1 Permafrost Creep. - 9.7.2 Thermokarst and Thaw Consolidation. - 9.7.3 Stability of Thawing Slopes. - 9.8 Cold-Climate Slope Evolution. - 9.8.1 Cryoplanation. - 9.8.2 Slope Replacement and Richter Denudation Slopes. - 9.8.3 Rapidity of Profile Change. - 9.8.4 Summary. - Advanced Reading. - Discussion Topics. - 10 Azonal Processes and Landforms. - 10.1 Introduction. - 10.2 Fluvial Processes and Landforms. - 10.2.1 Major Rivers. - 10.2.2 Freeze-Up and Break-Up. - 10.2.3 Basin Hydrology. - 10.2.4 Sediment Flow, Surface Transport, and Denudation. - 10.2.5 Fluvio-Thermal Erosion. - 10.2.6 Channel Morphology. - 10.2.7 Valley Asymmetry. - 10.3 Eolian Processes and Sediments. - 10.3.1 Wind Abrasion. - 10.3.2 Wind Deflation. - 10.3.3 Niveo-Eolian Sediments. - 10.3.4 Loess-Like Silt. - 10.3.5 Sand Dunes and San
    Location: AWI Reading room
    Location: Reading room
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