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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 |
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creator | Huang, Rui Xin Huang, Chuan Jiang Wang, Wei |
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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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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