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Enhanced vertical propagation of storm-induced near-inertial energy in an eddying ocean channel model

Abstract:
The interaction between inertial oscillations generated by a storm and a mesoscale eddy field is studied using a Southern Ocean channel model. It is shown that the leakage of near-inertial energy out of the surface layer is strongly enhanced by the presence of the eddies, with the anticyclonic eddies acting as a conduit to the deep ocean. Given the ubiquity of the atmospheric storm tracks (a source of near-inertial energy for the ocean) and regions of strong ocean mesoscale variability, we argue that this effect could be important for understanding pathways by which near-inertial energy enters the ocean and is ultimately available for mixing. Copyright 2005 by the American Geophysical Union.
Publication status:
Published

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Publisher copy:
10.1029/2005GL023643

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Journal:
GEOPHYSICAL RESEARCH LETTERS More from this journal
Volume:
32
Issue:
18
Pages:
1-4
Publication date:
2005-09-16
DOI:
ISSN:
0094-8276


Language:
English
Pubs id:
pubs:160035
UUID:
uuid:45e9afc3-48ca-44ca-8789-2386b69018dd
Local pid:
pubs:160035
Source identifiers:
160035
Deposit date:
2012-12-19

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