Forced two layer beta-plane quasi-geostrophic row, Part II: Time and space analyticity
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In this paper we continue the mathematical study initiated in [7] for a model of quasigeostrophic turbulence. We show that the unique weak solution found in [7] produces, via the inverse Fourier transform, a classical solution for the system. Moreover, we prove that this solution is analytic in space and positive time. Indiana University Mathematics Journal .