Applications of contour dynamics to two layer quasigeostrophic flows

Abstract
We determine stationary states and examine dynamic mergers of isolated piecewise constant regions of potential vorticity in a two-layer quasigeostrophic model. We focus on the behavior of the critical initial separation distance for merger, dc, as a function of γ-1 (inverse Rossby radius) and δ, the ration of layer depths.

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