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• W2015621836 abstract "Abstract Considered is a pointwise energy diagnostic scheme for a multilayer, primitive equation, nonisopycnic ocean model. Both conservative as well as nonconservative energy exchange terms are considered. Moreover, the scheme is worked out for both the finite depth as well as the reduced gravity versions of the model. The work is motivated by the need to discern the various instability processes responsible for the observed and modeled mesoscale flow structures commonly found in oceanic frontal regions, for example, upwelling areas, and regions separating coastal and adjacent deep ocean currents. As is common the mathematical form of the conservative energy exchange terms are ambiguous. A careful analysis is therefore effectuated to interpret them in terms of known physical processes. The analysis reveals that four basic instability processes are supported. One is the barotropic or horizontal shear instability, which extracts its energy from the horizontal shear in the mean current. The remaining three ..." @default.
• W2015621836 created "2016-06-24" @default.
• W2015621836 creator A5001514773 @default.
• W2015621836 date "1999-08-01" @default.
• W2015621836 modified "2023-09-29" @default.
• W2015621836 title "A Pointwise Energy Diagnostic Scheme for Multilayer, Nonisopycnic, Primitive Equation Ocean Models" @default.
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• W2015621836 doi "https://doi.org/10.1175/1520-0493(1999)127<1897:apedsf>2.0.co;2" @default.
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