Forced Two Layer Beta-Plane Quasi-Geostrophic Flow, Part II: Time and Space Analyticity
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In this paper we continue the mathematical study initiated in  for a model of quasigeostrophic turbulence. We show that the unique weak solution found in  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 ©.
author list (cited authors)
Onica, C., & Panetta, R. L.