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Abstract
In this paper, beginning with two-level quasi-geostrophie equations describing the baroclinic Rossby waves and using the bifurcation theory, a simple model of the stability for the baroclinic Rossby waves is set up. We find the linear and nonlinear control parameters and modify some classical conclusions of the stabilities.
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In this paper, beginning with two-level quasi-geostrophie equations describing the baroclinic Rossby waves and using the bifurcation theory, a simple model of the stability for the baroclinic Rossby waves is set up. We find the linear and nonlinear control parameters and modify some classical conclusions of the stabilities.
Key concepts: Baroclinity, Rossby wave, Rossby radius of deformation, Nonlinear system, Rossby number, Stability (learning theory), Bifurcation, Linear stability