Abstract
In this article, we study the critical dissipative surface quasi-geostrophic equation (SQG) in \({\mathbb{R}^2}\). Motivated by the study of the homogeneous statistical solutions of this equation, we show that for any large initial data θ 0 liying in the space \({\Lambda^{s} (\dot{H}^{s}_{uloc}(\mathbb{R}^2)) \cap L^\infty(\mathbb{R}^2)}\) the critical (SQG) has a global weak solution in time for 1/2 < s < 1. Our proof is based on an energy inequality verified by the equation \({(SQG)_{R,\epsilon}}\) which is nothing but the (SQG) equation with truncated and regularized initial data. By classical compactness arguments, we show that we are able to pass to the limit (\({R \rightarrow \infty}\), \({\epsilon \rightarrow 0}\)) in \({(SQG)_{R,\epsilon}}\) and that the limit solution has the desired regularity.
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Lazar, O. Global Existence for the Critical Dissipative Surface Quasi-Geostrophic Equation. Commun. Math. Phys. 322, 73–93 (2013). https://doi.org/10.1007/s00220-013-1693-2
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DOI: https://doi.org/10.1007/s00220-013-1693-2