Slowdown of Shirase Glacier, East Antarctica, caused by strengthening alongshore winds
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, observations in 2...
Published in: | The Cryosphere |
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Main Authors: | , , , , , |
Format: | Text |
Language: | English |
Published: |
2023
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-17-445-2023 https://tc.copernicus.org/articles/17/445/2023/ |