UNSTABLY STRATIFIED GEOPHYSICAL FLUID-DYNAMICS

The linear dynamics of the unstably stratified geophysical flows is in vestigated with a two-layer formulation. A 'convective' deformation ra dius classifies the dynamics into three regimes: 1. the scales smaller than the deformation radius: the dynamics characterized by unstable i nertial-gravity modes; 2, the scales larger than the deformation radiu s: a quasi-geostrophic regime; 3, the scales close to the deformation radius, where the dynamics transits from the inertial-gravity regime t o the quasi-geostrophic regime. The Rossby wave can propagate eastward in the unstably stratified quasi-geostrophic regime, The baroclinic i nstabilities are basically realized as a larger-scale extent of the in ertial-gravity instabilities, but the former can be isolated from the latter in a limit of small p-effect, with a very deep lower layer. The results suggest that the convectively unstable Jovian atmospheric dyn amics can be well described as a quasi-geostrophic system.