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Dynamical roles of mixed layer in regulating the meridional mass/heat fluxes

The mixed layer is an important component of the oceanic circulation system. Recent progress in energetics of the oceanic circulation suggests that the amount of external mechanical energy available for mixing is directly linked to the strength of the meridional overturning circulation. Using an ana...

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Published in:Journal of Geophysical Research. C. Oceans 2007-05, Vol.112 (C5), p.n/a
Main Authors: Huang, Rui Xin, Huang, Chuan Jiang, Wang, Wei
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Language:English
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description The mixed layer is an important component of the oceanic circulation system. Recent progress in energetics of the oceanic circulation suggests that the amount of external mechanical energy available for mixing is directly linked to the strength of the meridional overturning circulation. Using an analytical two‐dimensional model and a three‐dimensional numerical model, it is shown that the meridional distribution of mixed layer depth plays an important role in regulating the meridional overturning circulation and poleward heat flux. In fact, if the mixed layer at low and middle latitudes is deeper because of increase in mechanical energy input to the turbulence in the upper ocean, the meridional overturning circulation and poleward heat flux are enhanced in a steady circulation system, and at the same time, it may take less mechanical energy to support the subsurface diapycnal mixing.
doi_str_mv 10.1029/2006JC004046
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identifier ISSN: 0148-0227
ispartof Journal of Geophysical Research. C. Oceans, 2007-05, Vol.112 (C5), p.n/a
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2156-2202
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language eng
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source Wiley; Wiley-Blackwell AGU Digital Library
subjects Earth sciences
Earth, ocean, space
Exact sciences and technology
Marine
mechanical energy
meridional overturning circulation
Mixed layer
poleward heat flux
title Dynamical roles of mixed layer in regulating the meridional mass/heat fluxes
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