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...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Miles, Bertie W. J., Stokes, Chris R., Jenkins, Adrian, Jordan, Jim R., Jamieson, Stewart S. R., Gudmundsson, G. Hilmar
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-445-2023
https://tc.copernicus.org/articles/17/445/2023/