Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum
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Evidence for a palaeo-subglacial lake on the Antarctic continental shelf.Limited grounding-line advance onto the West Antarctic continental shelf in the easternmost Amundsen Sea Embayment during the last glacial period.Technologies for retrieving sediment cores in Antarctic subglacial settings.West Antarctic Ice Sheet retreat driven by Holocene warm water incursions.Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks.Atmosphere-ocean-ice interactions in the Amundsen Sea Embayment, West Antarctica
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Reconstruction of changes in the Amundsen Sea and Bellingshausen Sea sector of the West Antarctic Ice Sheet since the Last Glacial Maximum
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article
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im September 2014 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована у вересні 2014
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Reconstruction of changes in t ...... since the Last Glacial Maximum
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Reconstruction of changes in t ...... since the Last Glacial Maximum
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Reconstruction of changes in t ...... since the Last Glacial Maximum
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Reconstruction of changes in t ...... since the Last Glacial Maximum
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Reconstruction of changes in t ...... since the Last Glacial Maximum
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Reconstruction of changes in t ...... since the Last Glacial Maximum
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P50
P1476
Reconstruction of changes in t ...... since the Last Glacial Maximum
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P2093
Alexandra E. Witus
Colm Ó Cofaigh
Cornelia Spiegel
James A. Smith
Joanne S. Johnson
John B. Anderson
Julia Lindow
Michael J. Bentley
Robert D. Larter
Werner Ehrmann
P356
10.1016/J.QUASCIREV.2013.10.016
P50
P577
2014-09-01T00:00:00Z