Solutions to a class of forced drift-diffusion equations with applications to the magneto-geostrophic equations
Abstract
We prove the global existence of classical solutions to a class of forced drift-diffusion equations with L2 initial data and divergence free drift velocity \u\_0⊂ L∞t BMO-1x, and we obtain strong convergence of solutions as the viscosity vanishes. We then apply our results to a family of active scalar equations which includes the three dimensional magneto-geostrophic \MG\0 equation that has been proposed by Moffatt in the context of magnetostrophic turbulence in the Earth's fluid core. We prove the existence of a compact global attractor \A\0 in L2(T3) for the MG equations including the critical equation where =0. Furthermore, we obtain the upper semicontinuity of the global attractor as vanishes.
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