Time-Mean Flow as the Prevailing Contribution to the Poleward Heat Flux across the Southern Flank of the Antarctic Circumpolar Current: A Case Study in the Fawn Trough, Kerguelen Plateau

The major mechanisms of the oceanic poleward heat flux in the Southern Ocean are still in debate. The long-standing belief stipulates that the poleward heat flux across the Antarctic Circumpolar Current (ACC) is mainly due to mesoscale transient eddies and the cross-stream heat flux by time-mean flo...

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Bibliographic Details
Published in:Journal of Physical Oceanography
Main Authors: Sekma, H., Park, Y. -h., Vivier, F.
Format: Article in Journal/Newspaper
Language:English
Published: Amer Meteorological Soc 2013
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00181/29196/27591.pdf
https://doi.org/10.1175/JPO-D-12-0125.1
https://archimer.ifremer.fr/doc/00181/29196/