<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
<dc:title>Global regularity for a modified critical dissipative quasi-geostrophic equation</dc:title>
<dc:creator>Peter Constantin</dc:creator><dc:creator>Gautum Iyer</dc:creator><dc:creator>Jiahong Wu</dc:creator>
<dc:subject>35Q35</dc:subject><dc:subject>76B47</dc:subject><dc:subject>blow up</dc:subject><dc:subject>global regularity</dc:subject><dc:subject>quasi-geostrophic equations</dc:subject><dc:subject>nonlocal equations</dc:subject>
<dc:description>In this paper, we consider the modified quasi-geostrophic equation \begin{gather*} \partial_{t} \theta + (u \cdot \nabla) \theta  + \kappa \Lambda^{\alpha} \theta  = 0\\ u = \Lambda^{\alpha - 1} R^{\perp}\theta, \end{gather*} with $\kappa &gt; 0$, $\alpha \in (0,1]$ and $\theta_0 \in L^{2}(\mathbb{R}^2)$. We remark that the extra $\Lambda^{\alpha - 1}$ is introduced in order to make the scaling invariance of this system similar to the scaling invariance of the critical quasi-geostrophic equations. In this paper, we use Besov space techniques to prove global existence and regularity of strong solutions to this system.</dc:description>
<dc:publisher>Indiana University Mathematics Journal</dc:publisher>
<dc:date>2008</dc:date>
<dc:type>text</dc:type>
<dc:format>pdf</dc:format>
<dc:identifier>10.1512/iumj.2008.57.3629</dc:identifier>
<dc:source>10.1512/iumj.2008.57.3629</dc:source>
<dc:language>en</dc:language>
<dc:relation>Indiana Univ. Math. J. 57 (2008) 2681 - 2692</dc:relation>
<dc:coverage>state-of-the-art mathematics</dc:coverage>
<dc:rights>http://iumj.org/access/</dc:rights>
</oai_dc:dc>