Minimum-enstrophy solutions exist, are nonlinearly stable, and display latitude-dependent patterns with polar topographic trapping and equatorial zonal flow in topographic quasi-geostrophic flow on the rotating sphere.
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Minimum-enstrophy solutions in topographic quasi-geostrophic flow on the rotating sphere
Minimum-enstrophy solutions exist, are nonlinearly stable, and display latitude-dependent patterns with polar topographic trapping and equatorial zonal flow in topographic quasi-geostrophic flow on the rotating sphere.