Slowdown of Shirase Glacier caused by strengthening alongshore winds
Observations have confirmed basal melt rates of up to 16 m a -1 underneath the Shirase ice tongue in East Antarctica. These high basal melt rates are caused by intrusions of warm modified Circumpolar Deep Water (mCDW) onto the continental shelf, a mechanism responsible for widespread mass loss in We...
Main Authors: | , , , , , |
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Format: | Text |
Language: | English |
Published: |
2022
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-2022-126 https://tc.copernicus.org/preprints/tc-2022-126/ |