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...
Published in: | Journal of Geophysical Research: Oceans |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2019
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Subjects: | |
Online Access: | https://hdl.handle.net/1956/20561 https://doi.org/10.1002/2017jc013579 |