Under additional Lebesgue integrability assumptions, every smooth solution of the stationary fractional quasi-geostrophic system in dimensions 2, 3, and 4 with zero forcing is identically zero.
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The role of the dimension in uniqueness results for the stationary quasi-geostrophic system
Under additional Lebesgue integrability assumptions, every smooth solution of the stationary fractional quasi-geostrophic system in dimensions 2, 3, and 4 with zero forcing is identically zero.