Slowdown of Shirase Glacier, East Antarctica, caused by strengthening alongshore winds
<p>Around large parts of West Antarctica and in Wilkes Land, East Antarctica, increased wind-forced intrusions of modified Circumpolar Deep Water (mCDW) onto the continental shelf have been associated with mass loss over the last few decades. Despite considerable seasonal variability, observat...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2023-02-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/17/445/2023/tc-17-445-2023.pdf |