On the seasonal signal of the Filchner overflow, Weddell Sea, Antarctica
The cold ice shelf water (ISW) that formed below the Filchner–Ronne Ice Shelf in the southwestern Weddell Sea, Antarctica, escapes the ice shelf cavity through the Filchner Depression and spills over its sill at a rate of 1.6 Sverdrups (Sv; 1 Sv ≡ 106 m3 s−1), thus contributing significantly to the...
Published in: | Journal of Physical Oceanography |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Meteorological Society
2016
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Subjects: | |
Online Access: | https://hdl.handle.net/1956/13069 https://doi.org/10.1175/jpo-d-13-0180.1 |