Reversal of ocean gyres near ice shelves in the Amundsen Sea caused by the interaction of sea ice and wind

Floating ice shelves buttress the Antarctic Ice Sheet, which is losing mass rapidly mainly due to ocean-driven melting and the associated disruption to glacial dynamics. The local ocean circulation near ice shelves is therefore important for the prediction of future ice mass loss and related sea-lev...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Y. Zheng, D. P. Stevens, K. J. Heywood, B. G. M. Webber, B. Y. Queste
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-3005-2022
https://doaj.org/article/6f0c8d7148ef45998665ecea825af577