Wind– and sea-ice–driven interannual variability of Antarctic Bottom Water formation

Antarctic Bottom Water (AABW) is a major component of the global overturning circulation, originating around the Antarctic continental margin. In recent decades AABW has both warmed and freshened, but there is also evidence of large interannual variability. The causes of this underlying variability...

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Bibliographic Details
Main Authors: Schmidt, C., Morrison, A., England, M.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018258