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  • 1
    Monograph available for loan
    Monograph available for loan
    Ice sheets and late quaternary environmental change (2001)
    Chichester [u.a.] : Wiley
    Details Availability
    Call number: M 01.0426
    Type of Medium: Monograph available for loan
    Pages: xi, 231 S.
    ISBN: 0471985708
    Classification:
    Historical Geology
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Ice Sheets and Late Quaternary Environmental Change (2001)
    Cambridge, USA : Wiley
    Details Availability
    Call number: AWI G5-01-0098 ; AWI G7-02-0018
    Type of Medium: Monograph available for loan
    Pages: XI, 231 S. : Abb. ; 24 cm
    ISBN: 0471985694
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Exploration of Subsurface Antarctica : Uncovering Past Changes and Modern Processes (2018)
    London : Geological Society
    Associated volumes
    Details Availability
    Call number: 9/M 07.0421(461)
    In: Geological Society Special Publication
    Type of Medium: Monograph available for loan
    Pages: 255 Seiten , Illustrationen
    ISBN: 9781786203229
    Series Statement: Geological Society Special Publication 461
    URL: http://sp.lyellcollection.org/content/461/1
    Classification:
    Historical Geology
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    The Routledge handbook of the polar regions (2018)
    London : Routledge
    Details Availability
    Call number: IASS 19.91963
    Description / Table of Contents: Introduction : locating the polar regions / Mark Nuttall, Torben R. Christensen and Martin J. Siegert -- Exploring and mapping the Arctic : histories of discovery and knowledge / John McCannon -- Exploring and mapping the Antarctic : histories of discovery and knowledge / Ursula Rack -- The Arctic in literature and the popular imagination / Heidi Hansson -- The Antarctic in literature and the popular imagination / Elizabeth Leane -- Self-determination and indigenous governance in the Arctic / Mark Nuttall -- Indigenous cartographies of Arctic spaces and places / Kaitlin Young -- Circumpolar health and well-being / Helle Møller -- Education in the Arctic : trends, challenges and possibilities / Andrew Hodgkins -- Historical sites and heritage in the polar regions / Dag Avango -- Biodiversity in the polar regions in a warming world / Hans Meltofte -- The geological histories of polar environments / Tom Jordan -- Polar oceans and their global significance / Rory Bingham -- Polar sea ice as a barometer and driver of change / Jeremy Wilkinson and Julienne Stroeve -- The current health of polar ice sheets and implications for sea level / Mal McMillan -- Polar climatology and evidence for global warming / Gareth Marshall -- Post last glacial maximum processes in the polar regions / Pippa Whitehouse -- Biogeochemical cycling in glacial environments / Elizabeth A. Bagshaw -- Permafrost dynamics / Margareta Johansson -- Polar feedbacks in a changing climate / Richard Hodgkins -- The Antarctic Treaty, territorial claims and a continent for science / Klaus Dodds -- The polar regions and the law of the sea / Donald R. Rothwell -- The Arctic Council : governance and international relations / Timo Koivurova -- National Antarctic programmes : the politics-science interface / Anita Dey Nuttall -- Sustainable development and sustainability in Arctic political discourses / Birger Poppel -- Indigeneity, sovereignty and Arctic indigenous internationalism / Jessica Shadian -- Geopolitics and security in the Arctic / Andreas Østhagen -- Polar tourism : status, trends, futures / Emma J. Stewart and Daniela Liggett -- Consulting Arctic energy : from political hearings to roundtable events / Arthur Mason -- Social and environmental impact assessments in the Arctic / Anne Merrild Hansen, Sanne Vamme Larsen and Bram Noble -- Northern fisheries / Alf Håkon Hoel -- The future of Antarctica : minerals, bioprospecting and fisheries / Sanjay Chaturvedi -- Conservation and environmental governance in the polar regions / Mark Nuttall -- Polar technology and scientific discovery : exploring the great ice sheets through geophysics / Martin J. Siegert -- Looking into the past : ice and sediment cores / Robert McKay -- Subglacial access and investigation / Keith Makinson -- Upper atmosphere physics and chemistry / Sheila Kirkwood -- Ocean-land interactions and the Arctic carbon cycle / Frans-Jan Parmentier -- Back to the future : detecting past Arctic change and investing in future observations / Terry V. Callaghan, Margareta Johansson and Nadya Matveyeva
    Type of Medium: Monograph available for loan
    Pages: xxiii, 530 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9781138843998 , 9781315730639
    Series Statement: Routledge international handbooks
    Language: English
    Branch Library: RIFS Library
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  • 5
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    Exploration of Subsurface Antarctica : Uncovering Past Changes and Modern Processes (2018)
    London : The Geological Society
    Details
    Keywords: Antarctica ; glaciology ; subglacial Antarctica ; subglacial mountains ; subglacial lakes ; subglacial volcanoes ; glacier mass loss
    Description / Table of Contents: Exploration of subsurface Antarctica: uncovering past changes and modern processes / Martin J. Siegert, Stewart S. R. Jamieson and Duanne White / Geological Society, London, Special Publications, 461, 1-6, 25 September 2017, https://doi.org/10.1144/SP461.15 --- A 60-year international history of Antarctic subglacial lake exploration / Martin J. Siegert / Geological Society, London, Special Publications, 461, 7-21, 25 May 2017, https://doi.org/10.1144/SP461.5 --- Exploring the Recovery Lakes region and interior Dronning Maud Land, East Antarctica, with airborne gravity, magnetic and radar measurements / Rene Forsberg, Arne V. Olesen, Fausto Ferraccioli, Tom A. Jordan, Kenichi Matsuoka, Andres Zakrajsek, Marta Ghidella and Jamin S. Greenbaum / Geological Society, London, Special Publications, 461, 23-34, 20 September 2017, https://doi.org/10.1144/SP461.17 --- Ice-flow reorganization within the East Antarctic Ice Sheet deep interior / L. H. Beem, M. G. P. Cavitte, D. D. Blankenship, S. P. Carter, D. A. Young, G. R. Muldoon, C. S. Jackson and M. J. Siegert / Geological Society, London, Special Publications, 461, 35-47, 11 August 2017, https://doi.org/10.1144/SP461.14 --- Was South Georgia covered by an ice cap during the Last Glacial Maximum? / Duanne A. White, Ole Bennike, Martin Melles, Sonja Berg and Steven A. Binnie / Geological Society, London, Special Publications, 461, 49-59, 13 June 2017, https://doi.org/10.1144/SP461.4 --- The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica) / D. Casas, M. García, F. Bohoyo, A. Maldonado and G. Ercilla / Geological Society, London, Special Publications, 461, 61-75, 16 June 2017, https://doi.org/10.1144/SP461.10 --- Bathymetry of Schirmacher lakes as a tool for geomorphological evolution studies / Ashit Kumar Swain / Geological Society, London, Special Publications, 461, 77-93, 11 July 2017, https://doi.org/10.1144/SP461.13 --- Heavy mineral assemblage of marine sediments as an indicator of provenance and east antarctic ice sheet fluctuations / Mayuri Pandey, Naresh C. Pant, Paromita Biswas, Prakash K. Shrivastava, Sonalika Joshi and Neety Nagi / Geological Society, London, Special Publications, 461, 95-111, 22 June 2017, https://doi.org/10.1144/SP461.2 --- Position and variability of complex structures in the central East Antarctic Ice Sheet / Thilo Wrona, Michael J. Wolovick, Fausto Ferraccioli, Hugh Corr, Tom Jordan and Martin J. Siegert / Geological Society, London, Special Publications, 461, 113-129, 15 June 2017, https://doi.org/10.1144/SP461.12 --- Summit of the East Antarctic Ice Sheet underlain by thick ice-crystal fabric layers linked to glacial–interglacial environmental change / Bangbing Wang, Bo Sun, Carlos Martin, Fausto Ferraccioli, Daniel Steinhage, Xiangbin Cui and Martin J. Siegert / Geological Society, London, Special Publications, 461, 131-143, 26 May 2017, https://doi.org/10.1144/SP461.1 --- Drilling project at Gamburtsev Subglacial Mountains, East Antarctica: recent progress and plans for the future / Pavel Talalay, Youhong Sun, Yue Zhao, Yuansheng Li, Pinlu Cao, Alexey Markov, Huiwen Xu, Rusheng Wang, Nan Zhang, Xiaopeng Fan, Yang Yang, Mikhail Sysoev, Yongwen Liu and Yunchen Liu / Geological Society, London, Special Publications, 461, 145-159, 24 May 2017, https://doi.org/10.1144/SP461.9 --- A deep subglacial embayment adjacent to the grounding line of Institute Ice Stream, West Antarctica / Hafeez Jeofry, Neil Ross, Hugh F. J. Corr, Jilu Li, Prasad Gogineni and Martin J. Siegert / Geological Society, London, Special Publications, 461, 161-173, 13 June 2017, https://doi.org/10.1144/SP461.11 --- Ocean forced variability of Totten Glacier mass loss / Jason Roberts, Benjamin K. Galton-Fenzi, Fernando S. Paolo, Claire Donnelly, David E. Gwyther, Laurie Padman, Duncan Young, Roland Warner, Jamin Greenbaum, Helen A. Fricker, Antony J. Payne, Stephen Cornford, Anne Le Brocq, Tas van Ommen, Don Blankenship and Martin J. Siegert / Geological Society, London, Special Publications, 461, 175-186, 23 August 2017, https://doi.org/10.1144/SP461.6 --- Chemical characteristics of the ice cores obtained after the first unsealing of subglacial Lake Vostok / Irina Alekhina, Alexey Ekaykin, Alexey Moskvin and Vladimir Lipenkov / Geological Society, London, Special Publications, 461, 187-196, 24 May 2017, https://doi.org/10.1144/SP461.3 --- Antarctic subglacial groundwater: a concept paper on its measurement and potential influence on ice flow / Martin J. Siegert, Bernd Kulessa, Marion Bougamont, Poul Christoffersen, Kerry Key, Kristoffer R. Andersen, Adam D. Booth and Andrew M. Smith / Geological Society, London, Special Publications, 461, 197-213, 25 May 2017, https://doi.org/10.1144/SP461.8 --- Modern to Glacial age subglacial meltwater drainage at Law Dome, coastal East Antarctica from topography, sediments and jökulhlaup observations / Ian D. Goodwin, Jason L. Roberts, David M. Etheridge, John Hellstrom, Andrew D. Moy, Marta Ribo and Andrew M. Smith / Geological Society, London, Special Publications, 461, 215-230, 12 July 2017, https://doi.org/10.1144/SP461.16 --- A new volcanic province: an inventory of subglacial volcanoes in West Antarctica / Maximillian van Wyk de Vries, Robert G. Bingham and Andrew S. Hein / Geological Society, London, Special Publications, 461, 231-248, 29 May 2017, https://doi.org/10.1144/SP461.7
    Pages: Online-Ressource (VI, 255 Seiten) , Diagramme, Karten
    ISBN: 9781786203229
    URL: http://sp.lyellcollection.org/content/461/1
    Language: English
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  • 6
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    Vostok Subglacial Lake: A Review of Geophysical Data Regarding Its Discovery and Topographic Setting (2011)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: Vostok Subglacial Lake is the largest and best known sub-ice lake in Antarctica. The establishment of its water depth (〉500 m) led to an appreciation that such environments may be habitats for life and could contain ancient records of ice sheet change, which catalyzed plans for exploration and research. Here we discuss geophysical data used to identify the lake and the likely physical, chemical, and biological processes that occur in it. The lake is more than 250 km long and around 80 km wide in one place. It lies beneath 4.2 to 3.7 km of ice and exists because background levels of geothermal heating are sufficient to warm the ice base to the pressure melting value. Seismic and gravity measurements show the lake has two distinct basins. The Vostok ice core extracted 〉200 m of ice accreted from the lake to the ice sheet base. Analysis of this ice has given valuable insights into the lake s biological and chemical setting. The inclination of the ice-water interface leads to differential basal melting in the north versus freezing in the south, which excites circulation and potential mixing of the water. The exact nature of circulation depends on hydrochemical properties, which are not known at this stage. The age of the subglacial lake is likely to be as old as the ice sheet (approx.14 Ma). The age of the water within the lake will be related to the age of the ice melting into it and the level of mixing. Rough estimates put that combined age as approx.1 Ma.
    Keywords: Geophysics
    Type: GSFC.JA.6718.2012 , Geophysical Monograph Series; 192; 45-60
    Format: text
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    NASA TECHNICAL REPORTS
  • 7
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    Deep Radiostratigraphy of the East Antarctic Plateau: Connecting the Dome C and Vostok Ice Core Sites (2016)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: Several airborne radar-sounding surveys are used to trace internal reflections around the European Project for Ice Coring in Antarctica Dome C and Vostok ice core sites. Thirteen reflections, spanning the last two glacial cycles, are traced within 200 km of Dome C, a promising region for million-year-old ice, using the University of Texas Institute for Geophysics High-Capacity Radar Sounder. This provides a dated stratigraphy to 2318 m depth at Dome C. Reflection age uncertainties are calculated from the radar range precision and signal-to-noise ratio of the internal reflections. The radar stratigraphy matches well with the Multichannel Coherent Radar Depth Sounder (MCoRDS) radar stratigraphy obtained independently. We show that radar sounding enables the extension of ice core ages through the ice sheet with an additional radar-related age uncertainty of approximately 1/3-1/2 that of the ice cores. Reflections are extended along the Byrd-Totten Glacier divide, using University of Texas/Technical University of Denmark and MCoRDS surveys. However, core-to-core connection is impeded by pervasive aeolian terranes, and Lake Vostok's influence on reflection geometry. Poor radar connection of the two ice cores is attributed to these effects and suboptimal survey design in affected areas. We demonstrate that, while ice sheet internal radar reflections are generally isochronal and can be mapped over large distances, careful survey planning is necessary to extend ice core chronologies to distant regions of the East Antarctic ice sheet.
    Keywords: Meteorology and Climatology
    Type: GSFC-E-DAA-TN31687 , Journal of Glaciology (ISSN 0022-1430) (e-ISSN 1727-5652)
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    NASA TECHNICAL REPORTS
  • 8
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    The periglacial climate and environment in northern Eurasia during the Last Glaciation (2004)
    Elsevier
    In:  Quaternary Science Reviews, 23 (11-13). pp. 1333-1357.
    Details
    Publication Date: 2015-02-10
    Description: This paper summarizes the results of studies of the Late Weichselian periglacial environments carried out in key areas of northern Eurasia by several QUEEN teams (European Science Foundation (ESF) programme: “Quaternary Environment of the Eurasian North”). The palaeoglaciological boundary conditions are defined by geological data on timing and extent of the last glaciation obtained in the course of the EU funded project “Eurasian Ice Sheets”. These data prove beyond any doubt, that with the exception of the northwestern fringe of the Taymyr Peninsula, the rest of the Eurasian mainland and Severnaya Zemlya were not affected by the Barents–Kara Sea Ice Sheet during the Last Glacial Maximum (LGM). Inversed modelling based on these results shows that a progressive cooling which started around 30 ka BP, caused ice growth in Scandinavia and the northwestern areas of the Barents–Kara Sea shelf, due to a maritime climate with relatively high precipitation along the western flank of the developing ice sheets. In the rest of the Eurasian Arctic extremely low precipitation rates (less than 50 mm yr−1), did not allow ice sheet growth in spite of the very cold temperatures. Palaeoclimatic and palaeoenvironmental conditions for the time prior to, during, and after the LGM have been reconstructed for the non-glaciated areas around the LGM ice sheet with the use of faunal and vegetation records, permafrost, eolian sediments, alluvial deposits and other evidences. The changing environment, from interstadial conditions around 30 ka BP to a much colder and drier environment at the culmination of the LGM at 20–15 ka BP, and the beginning of warming around 15 ka BP have been elaborated from the field data, which fits well with the modelling results.
    Type: Article , PeerReviewed
    Format: text
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  • 9
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    Late Quaternary ice sheet history of northern Eurasia (2004)
    Elsevier
    In:  Quaternary Science Reviews, 23 (11-13). pp. 1229-1271.
    Details
    Publication Date: 2019-09-23
    Description: The maximum limits of the Eurasian ice sheets during four glaciations have been reconstructed: (1) the Late Saalian (〉140 ka), (2) the Early Weichselian (100–80 ka), (3) the Middle Weichselian (60–50 ka) and (4) the Late Weichselian (25–15 ka). The reconstructed ice limits are based on satellite data and aerial photographs combined with geological field investigations in Russia and Siberia, and with marine seismic- and sediment core data. The Barents-Kara Ice Sheet got progressively smaller during each glaciation, whereas the dimensions of the Scandinavian Ice Sheet increased. During the last Ice Age the Barents-Kara Ice Sheet attained its maximum size as early as 90–80,000 years ago when the ice front reached far onto the continent. A regrowth of the ice sheets occurred during the early Middle Weichselian, culminating about 60–50,000 years ago. During the Late Weichselian the Barents-Kara Ice Sheet did not reach the mainland east of the Kanin Peninsula, with the exception of the NW fringe of Taimyr. A numerical ice-sheet model, forced by global sea level and solar changes, was run through the full Weichselian glacial cycle. The modeling results are roughly compatible with the geological record of ice growth, but the model underpredicts the glaciations in the Eurasian Arctic during the Early and Middle Weichselian. One reason for this is that the climate in the Eurasian Arctic was not as dry then as during the Late Weichselian glacial maximum.
    Type: Article , PeerReviewed
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  • 10
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    Spatio-temporal variability of processes across Antarctic ice-bed–ocean interfaces (2018)
    Nature Research
    In:  Nature Communications, 9 (1). Art.Nr. 2289.
    Details
    Publication Date: 2021-02-08
    Description: Understanding how the Antarctic ice sheet will respond to global warming relies on knowledge of how it has behaved in the past. The use of numerical models, the only means to quantitatively predict the future, is hindered by limitations to topographic data both now and in the past, and in knowledge of how subsurface oceanic, glaciological and hydrological processes interact. Incorporating the variety and interplay of such processes, operating at multiple spatio-temporal scales, is critical to modeling the Antarctic’s system evolution and requires direct observations in challenging locations. As these processes do not observe disciplinary boundaries neither should our future research.
    Type: Article , PeerReviewed
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