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...

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Bibliographic Details
Published in:Journal of Physical Oceanography
Main Authors: Darelius, Elin Maria K., Strand, Kjersti Opstad, Østerhus, Svein, Gammelsrød, Tor, Årthun, Marius, Fer, Ilker
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2016
Subjects:
Online Access:https://hdl.handle.net/1956/13069
https://doi.org/10.1175/jpo-d-13-0180.1