ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Keywords
Language
  • 1
    Call number: AWI A2-07-0016
    In: Developments in quaternary science
    Description / Table of Contents: Table of Contents: Preface. - Acknowledgements. - Section 1: Forcing Mechanisms. - Section 2: Methods of palaeoclimate reconstruction and dating. - Section 3: Climate and vegetation in Europe during MIS 5. - Section 4: Climate, Vegetation and Mammalian faunas in Europe during Middle Pleistocene Interglacials (MIS 7, 9, 11). - Section 5: Modelling past interglacial climates. - Section 6: Synthesis. - Index
    Type of Medium: Monograph available for loan
    Pages: XIII, 622 S. : Ill., graph. Darst. + 1 CD-ROM
    Edition: 1. ed.
    ISBN: 0444529551 , 978-0-444-52955-8
    Series Statement: Developments in quaternary science 7
    Classification:
    Meteorology and Climatology
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Monograph available for loan
    Monograph available for loan
    [Stuttgart] : [Theiss]
    Call number: M 09.0213
    Type of Medium: Monograph available for loan
    Pages: 208 S.
    Edition: 1. Aufl.
    ISBN: 9783806222685
    Classification:
    Meteorology and Climatology
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Call number: 9/M 08.0390
    In: Developments in quaternary science
    Description / Table of Contents: Abstract: Helps you learn about the climate-environment system, its sensitivity, thresholds and feedback. This book presents the science on reconstructions from the Earth System, on methodological advances and on the ability of numerical models to simulate low and high frequency changes of climate, environment, and chemical cycling related to interglacials. Contents: Chapter 1. Forcing mechanisms (ed. M. Claussen) Chapter 2. Methods of palaeoclimate reconstruction and dating (ed. Frank Sirocko) Chapter 3 Climate and vegetation in Europe during MIS5 (M.F. S nchez Goni) Chapter 4. Climate and vegetation history of MIS 5-15 in Europe (Ed. Thomas Litt). Chapter 5. Modelling past interglacial climates (ed. Martin Claussen) Chapter 6. Analysis (F. Sirocko, M,.Claussen, et al.)
    Type of Medium: Monograph available for loan
    Pages: XIII, 622 S. : Ill., graph. Darst. + 1 CD-ROM
    Edition: Reprint.
    ISBN: 0444529551 , 978-0-444-52955-8
    Series Statement: Developments in quaternary science 7
    Location: Reading room
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Monograph available for loan
    Monograph available for loan
    Darmstadt : WBG (Wiss. Buchges.)
    Call number: M 24.95644
    Description / Table of Contents: Waldbrände, Flutkatastrophen, Erderwärmung - ein Phänomen des 21. Jahrhunderts? Oder bestimmt der Klimawandel nicht schon immer den Weg des Menschen? Mit dieser brandaktuellen Fragestellung befasst sich der Geowissenschaftler Frank Sirocko, doch nicht mit dem Ziel, die Zukunft vorherzusagen, sondern vielmehr um einen Blick weit zurück in die Vergangenheit zu werfen. Hochrangige archäologische Funde und historisch bedeutsame Ereignisse werden auf der Grundlage jüngster, bislang unveröffentlichter Forschungsergebnisse mit Wetter- und Klimaphänomenen in einen konkreten Zusammenhang gebracht. Ort der Forschung: Die Dauner Maare in der Vulkaneifel. Die Sedimente der Eifelmaare sind der einzige Ort in Mitteleuropa, der die letzten 40.000 Jahre vollständig dokumentiert. Mit Hilfe der Ablagerungen in den tiefen und sauerstoffarmen Seen können Geowissenschaftler erstmals die Klima- und Wetterbedingungen von den Neandertalern bis heute genau rekonstruieren. Extreme Hochwasser sind ebenso abzulesen wie kaltzeitliche Trockenphasen oder Vulkanausbrüche!   Biographische Informationen Frank Sirocko leitet das Institut für Geowissenschaften der Johannes Gutenberg-Universität Mainz.
    Description / Table of Contents: [Titelinformationen] -- Verzeichnis der Autoren -- [Impressum] -- [Menü] -- Zum Geleit -- Danksagung -- Einführung -- 1 Geologie und Entstehung der Maare -- 2 Limnologie der Maarseen und typische Sedimente -- Limnologie -- Seesedimente -- 3 Pollenanalyse als Grundlage der Rekonstruktion von Umwelt- und Vegetationsgeschichte -- Pollenanalyse -- Vegetationsgeschichte -- 4 Korngrößenanalyse und Sedimentgeochemie als Grundlage der Klima- und Wetterrekonstruktion -- Korngrößenanalysen -- Geochemische Analytik -- Transportprozesse -- Wellenerosion -- Windstaubsedimente -- Hochwasserlagen und fluviatile Sedimente -- Turbidite -- Rutschungen -- Vulkanite -- Schutt und Geröll -- 5 Bohrungen und Untersuchungsgebiete -- Schalkenmehrener Maar -- Ulmener Maar -- Holzmaar -- Dehner Maar -- 6 Datierung der Sedimente -- Die letzten 50 Jahre anhand von 137Cs -- Die letzten 100 Jahre anhand von 210Pb -- Die letzten 55.000 Jahre anhand von 14C -- Tephrochronologie -- Palynostratigraphie -- Freeze-Kerne der letzten 1000 Jahre -- Rammkerne der letzten 10.000 Jahre -- Holzmaar: Kern HM1 -- Ulmener Maar: Kern UM2 -- Seilkern der letzten 60.000 Jahre -- 7 Grundlagen des Klimas und extremer Wettersituationen -- Wettersysteme und Extremwetterereignisse -- Meteorologie von Extremwetterereignissen -- Kalt- und Warmereignisse -- Stürme -- Starkniederschläge -- Trockenperioden -- Regionalität -- 8 Ursachen von Klimavariabilität in der Vergangenheit -- Global Player Nummer 1: Die orbitale Konstellation zwischen Erde und Sonne -- Global Player Nummer 2: Veränderungen der Sonnenaktivität -- Global Player Nummer 3: Treibhausgase -- Global Player Nummer 4: Vulkanaktivität -- Interne Variabilität des Klimasystems als Global Player Nummer 5 -- 9 Archäologische Grabungen und Denkmäler -- 10 600.000-40.000 BP.
    Type of Medium: Monograph available for loan
    Pages: 208 Seiten , Illustrationen, Diagramme, Karten
    Edition: 3., durchgesehene Auflage
    ISBN: 978-3-534-25520-7
    Language: German
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Monograph available for loan
    Monograph available for loan
    Stuttgart : Konrad Theiss Verlag
    Call number: M 24.95892
    Description / Table of Contents: Nach "Wetter, Klima, Menschheitsentwicklung" (BA 9/09) legt der Paläoklimaforscher F. Sirocko hier den Schwerpunkt auf Entwicklung und Geschichte des Klimas von der Kreidezeit bis heute. Nach der Beschreibung der unterschiedlichen Prozesse im Klimasystem (u.a. CO2-Kreislauf, Treibhausgase, vulkanische Aktivitäten, Golfstrom, Einstrahlungsintensität, Land-Meer-Verteilung, Albedo) und ihren Auswirkungen geht er auf unterschiedliche Untersuchungsmethoden, Klimaarchive (u.a. Marine Sedimente, Seesedimente, Bodenstrukturen) und Klimamodelle ein und stellt auch deren jeweilige Vor- und Nachteile dar. Im Hauptteil rekonstruiert er die Entwicklung des Klimas in Mitteleuropa mit verschiedenen Methoden, die er einander gegenüberstellt und die Rolle des Menschen. Gut verständlich geschrieben trotz der komplexen Materie. Mit zahlreichen Abbildungen, Diagrammen, Karten und Textkästen zu klimarelevanten Stichworten. Neben "Heisse Zeiten für die Erde" (ID-A 8/13), "Eine kurze Geschichte des Klimas" (BA 12/06) und "Klimageschichte Mitteleuropas" (ID-B 17/13) als aktueller Titel zur Klimadiskussion sehr empfohlen. (1 S)
    Type of Medium: Monograph available for loan
    Pages: 184 Seiten , Illustrationen, graphische Darstellungen, Karten , 220 mm x 160 mm
    ISBN: 380622711X , 9783806227116
    Series Statement: Theiss WissenKompakt
    Parallel Title: Rezension Frank Sirocko, "Geschichte des Klimas" (Rezension)
    Language: German
    Note: Literaturverzeichnis Seiten 167 - 172
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Sedimentology 52 (2005), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: RADIUS is a newly developed particle-size measurement technique, based on evaluation of digital images of thin sections. Analyses are performed with sub-millimetre sample resolution and are thus designed to work on a single lamina of laminated sediments. The method covers grain sizes from medium silt to coarse sand. The application contains pattern-recognition modules that allow the detection of typical particle distributions of loess, organic detritus, turbidites and tephra layers. Cutting and hiding effects of particles on thin sections are corrected by empirical correction matrices. The calculated analysis results are compared with manually counted and measured samples to calibrate the application settings. The method can be applied to all fine-grained clastic sediments, particularly to laminated lake sediments.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 423 (2003), S. 813-814 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] On page 853 of this issue, Siddall et al. present a new approach to reconstructing the history of sea-level change during the last glacial cycle. They provide a detailed record, with a resolution on the century scale, spanning the years between 70,000 and 25,000 years ago. This was a time of ...
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 80 (1991), S. 557-566 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract Modern summer sea surface temperatures (SST) of the Arabian Sea show a correlation to Holocene accumulation rates of biogenic opal. This relation is used to infer mean summer SST for the Holocene (24–28 °C) and the last glaciation. Reduced accumulation rates of biogenic opal suggest higher SST during glacial times, which can be interpretated as a record of reduced upwelling intensity. Increased flux-rates of eolomarine dust in the northwestern Arabian Sea during glacial times indicate that northwesterly winds from the Persian Gulf area have replaced the southwesterly winds, which were shifted towards the south by about 200 km in the ground layer and about 500 km in the mid-troposphere.
    Abstract: Résumé Dans la mer d'Oman, il existe, pour la période moderne, une corrélation entre le taux d'accumulation de l'opale biogénique et la température estivale de la surface de la mer. Cette relation est utilisée pour calculer la température moyenne de la surface à l'Holocène (24 à 28°). Lors du dernier âge glaciaire, on observe un faible taux d'accumulation, ce qui correspond à une température de surface élevée; ce phénomène est dû probablement à une diminution des remontées d'eau («upwelling») le long des côtes d'Oman et de Somalie. Le taux élevé d'accumulation des sédiments éoliens d'origine désertique dans les parties nord et ouest de la Mer d'Oman, au cours de l'âge glaciaire montre qu'à ce moment des vents du nord-ouest, venant du Golfe Persique, ont remplacé les vents de mousson du sud-ouest, dont le domaine a été repoussé vers le sud d'environ 200 Km dans la basse atmosphère et de 500 Km dans la troposphère moyenne.
    Notes: Zusammenfassung Rezente Akkumulationsraten opalschaliger Planktongehäuse in Tiefseesedimenten des Arabischen Meeres zeigen ein ähnliches Verteilungsmuster wie die sommerlichen Wassertemperaturen an der Meeresoberfläche. Aus dieser Beziehung wurde eine Korrelationsgleichung abgeleitet, um mittlere Meeresoberflächentemperaturen während des Holozäns zu errechnen (24–28 °C). Geringere Akkumulationsraten von biogenem Opal weisen zur Zeit der letzten Eiszeit auf erhöhte Meeresoberflächentemperaturen, wahrscheinlich verursacht durch eine verminderte Intensität des Küstenauftriebs vor Oman und Somalia. Erhöhte Akkumulationsraten von Wüstenstaubsedimenten im Norden und Westen des Arabischen Meeres deuten darauf hin, daß während des letzten Kaltstadiums nordwestliche Winde aus der Region des Persischen Golfes die nördlichsten Ausläufer der Südwestmonsunwinde zurückgedrängt haben. Die Windbahnen des Südwestmonsun verliefen damals in Bodennähe ca. 200 km, und in der mittleren Troposphäre ca. 500 km weiter südlich als heute.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Variations in the deep-sea carbon reservoir have been invoked to explain the observed atmospheric carbon dioxide (CO2) changes during glacial-interglacial cycles. In order to distinguish between the quantity of organic matter remineralized in the deep-sea and that permanently removed into sediments, we compared the bulk- and organic carbon-accumulation rates in Holocene and glacial sediments deposited below the oxygen minimum layer with total- and organic carbon fluxes to the deep Arabian Sea from continuous sediment trap deployments. This comparison shows that the mass of organic carbon remineralized at the sediment water interface is mainly a function of the bulk sediment flux. The oxygen consumed by the organic carbon remineralization is of the order of the observed oxygen deficiency of the modern deep Arabian Sea water. We use the evidence from the northern Indian Ocean to speculate on the possible effect of abiogenic mineral flux on the removal of organic carbon from upper layers of the world ocean to the deep-sea. We assume that if the bulk accumulation rate (not primary productivity) influences the flux of organic carbon (that is fixed from the atmosphere by marine organisms), then mineral matter flux will exert a significant control over atmospheric CO2 contents. Model calculations incorporating transient changes in global bulk flux, caused by natural or anthropogenic changes, show that significant proportions of the observed changes in atmospheric CO2 contents can be explained by this mechanism.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2024-11-11
    Description: This paper presents radon flux profiles from four regions in Schleswig–Holstein (Northern Germany). Three of these regions are located over deep-rooted tectonic faults or salt diapirs and one is in an area without any tectonic or halokinetic activity, but with steep topography. Contrary to recently published studies on spatial patterns of soil radon gas concentration we measured flux of radon from soil into the atmosphere. All radon devices of each profile were deployed simultaneously to avoid inconsistencies due to strong diurnal variations of radon exhalation. To compare data from different seasons, values had to be normalized. Observed radon flux patterns are apparently related to the mineralogical composition of the Quaternary strata (particularly to the abundance of reddish granite and porphyry), and its grain size (with a flux maximum in well-sorted sand/silt). Minimum radon flux occurs above non-permeable, clay-rich soil layers. Small amounts of water content in the pore space increase radon flux, whereas excessive water content lessens it. Peak flux values, however, are observed over a deep-rooted fault system on the eastern side of Lake Plön, i.e., at the boundary of the Eastholstein Platform and the Eastholstein Trough. Furthermore, high radon flux values are observed in two regions associated with salt diapirism and near-surface halokinetic faults. These regions show frequent local radon flux maxima, which indicate that the uppermost strata above salt diapirs are very inhomogeneous. Deep-rooted increased permeability (effective radon flux depth) or just the boundaries between permeable and impermeable strata appear to concentrate radon flux. In summary, our radon flux profiles are in accordance with the published evidence of low radon concentrations in the “normal” soils of Schleswig–Holstein. However, very high values of radon flux are likely to occur at distinct locations near salt diapirism at depth, boundaries between permeable and impermeable strata, and finally at the tectonically active flanks of the North German Basin.
    Description: Bundesministerium für Wirtschaft und Energie http://dx.doi.org/10.13039/501100006360
    Description: Johannes Gutenberg-Universität Mainz (1030)
    Keywords: ddc:551 ; Radon flux ; Local radon flux maxima ; Permeability ; Quaternary sediments ; Salt tectonics ; Schleswig–Holstein
    Language: English
    Type: info:eu-repo/semantics/article , doc-type:article
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...