Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum
Marine and terrestrial geological and marine geophysical data that constrain deglaciation since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) draining into the Amundsen Sea and Bellingshausen Sea have been collated and used as the basis for a set of time-slice r...
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Online Access: | https://hdl.handle.net/1911/88244 https://doi.org/10.1016/j.quascirev.2013.10.016 |
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ftriceuniv:oai:scholarship.rice.edu:1911/88244 2023-05-15T13:23:46+02:00 Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum Larter, Robert D. Anderson, John B. Graham, Alastair G.C. Gohl, Karsten Hillenbrand, Claus-Dieter Jakobsson, Martin Johnson, Joanne S. Kuhn, Gerhard Nitsche, Frank O. Smith, James A. Witus, Alexandra E. Bentley, Michael J. Dowdeswell, Julian 2014 application/pdf https://hdl.handle.net/1911/88244 https://doi.org/10.1016/j.quascirev.2013.10.016 eng eng Elsevier Larter, Robert D., Anderson, John B., Graham, Alastair G.C., et al. "Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum." Quaternary Science Reviews, 100, (2014) Elsevier: 55-86. http://dx.doi.org/10.1016/j.quascirev.2013.10.016. https://hdl.handle.net/1911/88244 http://dx.doi.org/10.1016/j.quascirev.2013.10.016 This is an open access article under the CC BY license. http://creativecommons.org/licenses/by/3.0/ CC-BY Ice sheet Last Glacial Maximum Holocene Ice stream Grounding line Radiocarbon Cosmogenic isotope Surface exposure age Multibeam swath bathymetry Sediment Glacimarine Diamicton Continental shelf Circumpolar deep water Subglacial meltwater Sea level Journal article Text publisher version 2014 ftriceuniv https://doi.org/10.1016/j.quascirev.2013.10.016 2022-08-09T20:46:31Z Marine and terrestrial geological and marine geophysical data that constrain deglaciation since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) draining into the Amundsen Sea and Bellingshausen Sea have been collated and used as the basis for a set of time-slice reconstructions. The drainage basins in these sectors constitute a little more than one-quarter of the area of the WAIS, but account for about one-third of its surface accumulation. Their mass balance is becoming increasingly negative, and therefore they account for an even larger fraction of current WAIS discharge. If all of the ice in these sectors of the WAIS were discharged to the ocean, global sea level would rise by ca 2 m. There is compelling evidence that grounding lines of palaeo-ice streams were at, or close to, the continental shelf edge along the Amundsen Sea and Bellingshausen Sea margins during the last glacial period. However, the few cosmogenic surface exposure ages and ice core data available from the interior of West Antarctica indicate that ice surface elevations there have changed little since the LGM. In the few areas from which cosmogenic surface exposure ages have been determined near the margin of the ice sheet, they generally suggest that there has been a gradual decrease in ice surface elevation since pre-Holocene times. Radiocarbon dates from glacimarine and the earliest seasonally open marine sediments in continental shelf cores that have been interpreted as providing approximate ages for post-LGM grounding-line retreat indicate different trajectories of palaeo-ice stream recession in the Amundsen Sea and Bellingshausen Sea embayments. The areas were probably subject to similar oceanic, atmospheric and eustatic forcing, in which case the differences are probably largely a consequence of how topographic and geological factors have affected ice flow, and of topographic influences on snow accumulation and warm water inflow across the continental shelf. Pauses in ice retreat are recorded where ... Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctica Bellingshausen Sea ice core Ice Sheet West Antarctica Rice University: Digital Scholarship Archive Antarctic West Antarctica Amundsen Sea West Antarctic Ice Sheet Bellingshausen Sea Quaternary Science Reviews 100 55 86 |
institution |
Open Polar |
collection |
Rice University: Digital Scholarship Archive |
op_collection_id |
ftriceuniv |
language |
English |
topic |
Ice sheet Last Glacial Maximum Holocene Ice stream Grounding line Radiocarbon Cosmogenic isotope Surface exposure age Multibeam swath bathymetry Sediment Glacimarine Diamicton Continental shelf Circumpolar deep water Subglacial meltwater Sea level |
spellingShingle |
Ice sheet Last Glacial Maximum Holocene Ice stream Grounding line Radiocarbon Cosmogenic isotope Surface exposure age Multibeam swath bathymetry Sediment Glacimarine Diamicton Continental shelf Circumpolar deep water Subglacial meltwater Sea level Larter, Robert D. Anderson, John B. Graham, Alastair G.C. Gohl, Karsten Hillenbrand, Claus-Dieter Jakobsson, Martin Johnson, Joanne S. Kuhn, Gerhard Nitsche, Frank O. Smith, James A. Witus, Alexandra E. Bentley, Michael J. Dowdeswell, Julian Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum |
topic_facet |
Ice sheet Last Glacial Maximum Holocene Ice stream Grounding line Radiocarbon Cosmogenic isotope Surface exposure age Multibeam swath bathymetry Sediment Glacimarine Diamicton Continental shelf Circumpolar deep water Subglacial meltwater Sea level |
description |
Marine and terrestrial geological and marine geophysical data that constrain deglaciation since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) draining into the Amundsen Sea and Bellingshausen Sea have been collated and used as the basis for a set of time-slice reconstructions. The drainage basins in these sectors constitute a little more than one-quarter of the area of the WAIS, but account for about one-third of its surface accumulation. Their mass balance is becoming increasingly negative, and therefore they account for an even larger fraction of current WAIS discharge. If all of the ice in these sectors of the WAIS were discharged to the ocean, global sea level would rise by ca 2 m. There is compelling evidence that grounding lines of palaeo-ice streams were at, or close to, the continental shelf edge along the Amundsen Sea and Bellingshausen Sea margins during the last glacial period. However, the few cosmogenic surface exposure ages and ice core data available from the interior of West Antarctica indicate that ice surface elevations there have changed little since the LGM. In the few areas from which cosmogenic surface exposure ages have been determined near the margin of the ice sheet, they generally suggest that there has been a gradual decrease in ice surface elevation since pre-Holocene times. Radiocarbon dates from glacimarine and the earliest seasonally open marine sediments in continental shelf cores that have been interpreted as providing approximate ages for post-LGM grounding-line retreat indicate different trajectories of palaeo-ice stream recession in the Amundsen Sea and Bellingshausen Sea embayments. The areas were probably subject to similar oceanic, atmospheric and eustatic forcing, in which case the differences are probably largely a consequence of how topographic and geological factors have affected ice flow, and of topographic influences on snow accumulation and warm water inflow across the continental shelf. Pauses in ice retreat are recorded where ... |
format |
Article in Journal/Newspaper |
author |
Larter, Robert D. Anderson, John B. Graham, Alastair G.C. Gohl, Karsten Hillenbrand, Claus-Dieter Jakobsson, Martin Johnson, Joanne S. Kuhn, Gerhard Nitsche, Frank O. Smith, James A. Witus, Alexandra E. Bentley, Michael J. Dowdeswell, Julian |
author_facet |
Larter, Robert D. Anderson, John B. Graham, Alastair G.C. Gohl, Karsten Hillenbrand, Claus-Dieter Jakobsson, Martin Johnson, Joanne S. Kuhn, Gerhard Nitsche, Frank O. Smith, James A. Witus, Alexandra E. Bentley, Michael J. Dowdeswell, Julian |
author_sort |
Larter, Robert D. |
title |
Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum |
title_short |
Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum |
title_full |
Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum |
title_fullStr |
Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum |
title_full_unstemmed |
Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum |
title_sort |
reconstruction of changes in the amundsen sea and bellingshausen sea sector of the west antarctic ice sheet since the last glacial maximum |
publisher |
Elsevier |
publishDate |
2014 |
url |
https://hdl.handle.net/1911/88244 https://doi.org/10.1016/j.quascirev.2013.10.016 |
geographic |
Antarctic West Antarctica Amundsen Sea West Antarctic Ice Sheet Bellingshausen Sea |
geographic_facet |
Antarctic West Antarctica Amundsen Sea West Antarctic Ice Sheet Bellingshausen Sea |
genre |
Amundsen Sea Antarc* Antarctic Antarctica Bellingshausen Sea ice core Ice Sheet West Antarctica |
genre_facet |
Amundsen Sea Antarc* Antarctic Antarctica Bellingshausen Sea ice core Ice Sheet West Antarctica |
op_relation |
Larter, Robert D., Anderson, John B., Graham, Alastair G.C., et al. "Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum." Quaternary Science Reviews, 100, (2014) Elsevier: 55-86. http://dx.doi.org/10.1016/j.quascirev.2013.10.016. https://hdl.handle.net/1911/88244 http://dx.doi.org/10.1016/j.quascirev.2013.10.016 |
op_rights |
This is an open access article under the CC BY license. http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.quascirev.2013.10.016 |
container_title |
Quaternary Science Reviews |
container_volume |
100 |
container_start_page |
55 |
op_container_end_page |
86 |
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1766374764056674304 |