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Global existence for the critical dissipative surface quasi-geostrophic equation

Published 30 Sep 2012 in math.AP | (1210.0213v3)

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 $\theta_{0}$ 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 all $1/2< s<1$. Our proof is based on an energy inequality verified by the truncated $(SQG){R,\ep}$ equation. By classical compactness arguments, we show that we are able to pass to the limit ($R \rightarrow \infty$, $\ep \rightarrow 0$) in $(SQG){R,\ep}$ and that the limit solution has the desired regularity.

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