Articles | Volume 12, issue 3
Ocean Sci., 12, 743–769, 2016
https://doi.org/10.5194/os-12-743-2016
Ocean Sci., 12, 743–769, 2016
https://doi.org/10.5194/os-12-743-2016
Research article
01 Jun 2016
Research article | 01 Jun 2016

Dissipation of the energy imparted by mid-latitude storms in the Southern Ocean

Julien Jouanno et al.

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Cited articles

Abernathey, R., Marshall, J., and Ferreira, D.: The Dependence of Southern Ocean Meridional Overturning on Wind Stress, J. Phys. Oceanogr., 41, 2261–2278, 2011.
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Alford, M. H., Cronin, M. F., and Klymak, J. M.: Annual Cycle and Depth Penetration of Wind-Generated Near-Inertial Internal Waves at Ocean Station Papa in the Northeast Pacific, J. Phys. Oceanogr., 42, 889–909, 2012.
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Badin, G. and Williams, R. G.: On the buoyancy forcing and residual circulation in the Southern Ocean: The feedback from Ekman and eddy transfer, J. Phys. Oceanogr., 40, 295–310, 2010.
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Short summary
The aim of this study is to clarify the role of the Southern Ocean storms on interior mixing and meridional overturning circulation. A periodic and idealized configuration of the NEMO model has been designed to represent the key physical processes of a zonal portion of the Southern Ocean. Challenging issues concerning how numerical models are able to represent interior mixing forced by high-frequency winds are exposed and discussed, particularly in the context of the overturning circulation.