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• W2039470369 abstract "Linear instability theory is used to predict the lateral diffusivity K for eddy buoyancy fluxes in an idealized channel model, following a suggestion by Killworth (1997). The vertical structure and magnitude of K agree approximately with the non-linear model results. The lateral structure of K from linear theory lacks minima within eddy-driven zonal jets, pointing towards a non-linear mechanism for mixing barriers in the channel model. This effect can be accounted for by a modification of K from linear theory by the kinematic effect of the background flow following a recent suggestion by Ferrari and Nikurashin (2010). Implementation of this closure for K in an eddy mixing framework based on potential vorticity mixing in a zonally averaged model version yields approximate agreement with the zonally resolved version over a certain range of external parameters, in particular with respect to the reproduction of eddy-driven zonal jets." @default.
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• W2039470369 creator A5055136754 @default.
• W2039470369 date "2011-01-01" @default.
• W2039470369 modified "2023-10-18" @default.
• W2039470369 title "A closure for meso-scale eddy fluxes based on linear instability theory" @default.
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• W2039470369 doi "https://doi.org/10.1016/j.ocemod.2011.05.009" @default.
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