Grounding-line retreat of the West Antarctic Ice Sheet from inner Pine Island Bay

Ice loss from the marine-based, potentially unstable West Antarctic Ice Sheet (WAIS) contributes to current sea-level rise and may raise sea level by ≤3.3 m or even ≤5 m in the future. Over the past few decades, glaciers draining the WAIS into the Amundsen Sea Embayment (ASE) have shown accelerated...

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Bibliographic Details
Published in:Geology
Main Authors: Hillenbrand, Claus-Dieter, Kuhn, Gerhard, Smith, James A., Gohl, Karsten, Graham, Alastair G.C., Larter, Robert D., Klages, Johann P., Downey, Rachel, Moreton, Steven G., Forwick, Matthias, Vaughan, David G.
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 2013
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/21383/
https://doi.org/10.1130/G33469.1