Garra, Roberto Confinement of a hot temperature patch in the modified SQG model. (English) Zbl 1418.35344 Discrete Contin. Dyn. Syst., Ser. B 24, No. 6, 2407-2416 (2019). Summary: In this paper we study the time evolution of a temperature patch in \(\mathbb{R}^2\) according to the modified Surface Quasi-Geostrophic (SQG) patch equation. In particular we give a temporal estimate on the growth of the support, providing a rigorous proof of the confinement of a hot patch of temperature in absence of external forcing, under the quasi-geostrophic approximation. Cited in 3 Documents MSC: 35Q86 PDEs in connection with geophysics 76E20 Stability and instability of geophysical and astrophysical flows 37N10 Dynamical systems in fluid mechanics, oceanography and meteorology Keywords:modified surface quasi-geostrophic equation; confinement of temperature patch; active scalar flow PDF BibTeX XML Cite \textit{R. Garra}, Discrete Contin. Dyn. Syst., Ser. B 24, No. 6, 2407--2416 (2019; Zbl 1418.35344) Full Text: DOI arXiv OpenURL