Circulation characteristics in three eddy-permitting models of the North Atlantic


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jwillebrand [ at ] ifm.uni-kiel.de

Abstract

A systematic intercomparison of three realistic eddy-permitting models of the North Atlanticcirculation has been performed. The models use different concepts for the discretization of thevertical coordinate, namely geopotential levels, isopycnal layers, terrain-following (sigma)coordinates, respectively. Although these models were integrated under nearly identicalconditions, the resulting large-scale model circulations show substantial differences. The resultsdemonstrate that the large-scale thermohaline circulation is very sensitive to the modelrepresentation of certain localised processes, in particular to the amount and water massproperties of the overflow across the Greenland-Scotland region, to the amount of mixing withina few hundred kilometers south of the sills, and to several other processes at small or sub-gridscales. The different behaviour of the three models can to a large extent be explained as aconsequence of the different model representation of these processes.



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ISI/Scopus peer-reviewed
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Eprint ID
5009
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Willebrand, J. , Barnier, B. , Böning, C. , Dieterich, C. , Killworth, P. D. , Le Provost, C. , Jia, Y. , Molines, J. M. and New, A. L. (2001): Circulation characteristics in three eddy-permitting models of the North Atlantic , Progress in Oceanography, 48 (2), pp. 123-161 .


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