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A Simple Predictive Model for the Structure of the Oceanic Pycnocline

Science  26 Mar 1999:
Vol. 283, Issue 5410, pp. 2077-2079
DOI: 10.1126/science.283.5410.2077

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Abstract

A simple theory for the large-scale oceanic circulation is developed, relating pycnocline depth, Northern Hemisphere sinking, and low-latitude upwelling to pycnocline diffusivity and Southern Ocean winds and eddies. The results show that Southern Ocean processes help maintain the global ocean structure and that pycnocline diffusion controls low-latitude upwelling.

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