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contributor authorIto, Taka
contributor authorMarshall, John
date accessioned2017-06-09T16:25:06Z
date available2017-06-09T16:25:06Z
date copyright2008/12/01
date issued2008
identifier issn0022-3670
identifier otherams-67498.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208951
description abstractA simple model is developed of the lower limb of the meridional overturning circulation in the Southern Ocean based on residual-mean theory. It is hypothesized that the strength of the lower-limb overturning (?) is strongly controlled by the magnitude of abyssal diapycnal mixing (?) and that of mesoscale eddy transfer (K). In particular, it is argued that ? ? ?K. The scaling and associated theory find support in a suite of sensitivity experiments with an idealized ocean general circulation model. This study shows that intense diapycnal mixing is required to close the buoyancy budget of the lower-limb overturning circulation, in contrast to the upper limb, where air?sea buoyancy fluxes can provide the required diabatic forcing.
publisherAmerican Meteorological Society
titleControl of Lower-Limb Overturning Circulation in the Southern Ocean by Diapycnal Mixing and Mesoscale Eddy Transfer
typeJournal Paper
journal volume38
journal issue12
journal titleJournal of Physical Oceanography
identifier doi10.1175/2008JPO3878.1
journal fristpage2832
journal lastpage2845
treeJournal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 012
contenttypeFulltext


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