Potential of the solid-Earth response for limiting long-term West Antarctic Ice Sheet retreat
The West Antarctic Ice Sheet (WAIS) is assumed to be inherently unstable because it is grounded below sea level in a large part, where the bedrock deepens from today’s grounding line towards the interior of the ice sheet. Idealized simulations have shown that bedrock uplift due to isostatic adjustme...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2016
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Subjects: | |
Online Access: | https://gfzpublic.gfz-potsdam.de/pubman/item/item_1503921 |