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Eddy cancellation of the Ekman cell in subtropical gyres

Abstract:
The presence of large-scale Ekman pumping associated with the climatological wind stress curl is the textbook explanation for low biological activity in the subtropical gyres. Using an idealized eddy-resolving model it is shown that Eulerian-mean Ekman pumping may be opposed by an eddy-driven circulation, analogous to the way in which the atmospheric Ferrel cell and the Southern Ocean Deacon cell are opposed by eddy-driven circulations. Lagrangian particle tracking, potential vorticity fluxes, and depth-density streamfunctions are used to show that, in the model, the rectified effect of eddies acts to largely cancel the Eulerian-mean Ekman downwelling. To distinguish this effect from eddy compensation, it is proposed that the suppression of Eulerian-mean downwelling by eddies be called ``eddy cancellation.''
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1175/JPO-D-16-0097.1

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Role:
Author


Publisher:
American Meteorological Society
Journal:
Journal of Physical Oceanography More from this journal
Volume:
46
Issue:
10
Pages:
2995–3010
Publication date:
2016-06-01
Acceptance date:
2016-06-09
DOI:
EISSN:
1520-0485
ISSN:
0022-3670


Pubs id:
pubs:627843
UUID:
uuid:b53bc9b2-c622-46b1-aecf-9ff86411f0f2
Local pid:
pubs:627843
Source identifiers:
627843
Deposit date:
2016-06-14

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