Coupled ice–ocean interactions during future retreat of West Antarctic ice streams in the Amundsen Sea sector
The Amundsen Sea sector has some of the fastest-thinning ice shelves in Antarctica, caused by high, ocean-driven basal melt rates, which can lead to increased ice streamflow, causing increased sea level rise (SLR) contributions. In this study, we present the results of a new synchronously coupled ic...
Published in: | The Cryosphere |
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Main Authors: | , , , , , |
Format: | Text |
Language: | English |
Published: |
2024
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-18-2653-2024 https://tc.copernicus.org/articles/18/2653/2024/ |