Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea

The Filchner Trough (FT) is a key site for exchange of water masses between the Weddell Sea continental shelf and the deep ocean. Cold and dense Ice Shelf Water (ISW), a precursor for Antarctic Bottom Water, flows north along the FT and overflows the Filchner Sill. Although access of warm water to t...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Daae, Kjersti, Darelius, Elin Maria K., Fer, Ilker, Østerhus, Svein, Ryan, S.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2019
Subjects:
Online Access:https://hdl.handle.net/1956/20561
https://doi.org/10.1002/2017jc013579