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The abyssal stratification and circulation deduced from the principle of maximal entropy production Cover

The abyssal stratification and circulation deduced from the principle of maximal entropy production

Open Access
|Jan 2006

Abstract

A theory for the abyssal stratification and circulation is derived from the principle of maximal production of information entropy used in non-equilibrium statistical dynamics. For an abyssal ocean of simple geometry and simple, though plausible, parameterization of the vertical diffusivity, stratification profiles together with their associated circulation are obtained. These profiles are characterized by an abyssal thermocline thickness scaling as √κvH/ws0, where ws0 is the upwelling velocity at the top of an abyssal ocean of depth H, and κv is its vertical diffusivity. Remarkably, the associated circulation is barotropic and coincides with the classical theory of the abyssal circulation by Stommel and Arons.

Language: English
Page range: 392 - 403
Submitted on: Dec 30, 2004
Accepted on: Nov 21, 2005
Published on: Jan 1, 2006
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2006 Mahdi Ben Jelloul, Rui Xin Huang, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.