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- W2109393918 abstract "A finite-amplitude model of baroclinic instability is studied in the case where the cross-stream scale is large compared with the Rossby deformation radius and the dissipative and advective time scales are of the same order. A theory is developed that describes the nature of the wave field as the shear supercriticality increases beyond the stability threshold of the most unstable cross-stream mode and penetrates regions of higher supercriticality. The set of possible steady nonlinear modes is found analytically. It is shown that the steady cross-stream structure of each finite-amplitude mode is a function of the supercriticality. Integrations of initial-value problems show, in each case, that the final state realized is the state characterized by the finite-amplitude mode with the largest equilibrium amplitude. The approach to this steady state is oscillatory (nonmonotonic). Further, each steady-state mode is a well-defined mixture of linear cross-stream modes." @default.
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- W2109393918 date "1976-12-07" @default.
- W2109393918 modified "2023-09-26" @default.
- W2109393918 title "On the dynamics of finite-amplitude baroclinic waves as a function of supercriticality" @default.
- W2109393918 cites W4289981527 @default.
- W2109393918 doi "https://doi.org/10.1017/s0022112076002644" @default.
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