Bae, Hantaek
2015-09-03T08:01:56Z
2015-09-03
2011-03
NONLINEAR ANALYSIS-THEORY METHODS & APPLICATIONS, v.74, no.5, pp.1995 - 2002
0362-546X
https://scholarworks.unist.ac.kr/handle/201301/16613
In this paper, we study the critical dissipative quasi-geostrophic equations in scaling invariant spaces. We prove that there exists a global-in-time small solution for small initial data theta(0) is an element of L-infinity boolean AND (H) over dot(1) such that R(theta(0)) is an element of L-infinity, where R is the Riesz transform. As a corollary, we prove that if in addition, theta(0) is an element of (B) over dot(infinity,q)(0), 1 <= q < 2, is small enough, then theta is an element of (L) over tilde (infinity)(t)(B) over dot(infinity,q)(0)boolean AND(L) over tilde (1)(t) (B) over dot(infinity,q)(1). (C) 2010 Elsevier Ltd. All rights reserved
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PERGAMON-ELSEVIER SCIENCE LTD
Global well-posedness for the critical dissipative quasi-geostrophic equations in L-infinity
ARTICLE
2041
23516
2-s2.0-78651371128
000286178200041
ART
0
0
2015-12-28
2015-11-04
10.1016/j.na.2010.11.006
http://www.sciencedirect.com/science/article/pii/S0362546X10007844