2016
DOI: 10.1016/j.jde.2016.04.011
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On 2-D Boussinesq equations for MHD convection with stratification effects

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Cited by 33 publications
(29 citation statements)
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“…which is not enough to extend continuously the solution .u, Â/ beyond the time T. Fortunately, the 2D Euler equations in (1.1) provide the uniformly estimates (Theorem 3.2) in L 1 .0, T; L 2 .R 2 // about the vorticity ! :D @ 1 u 2 @ 2 u 1 , which also leads to the key estimate in [1,18]- is Hölder continuous (Lemma 3.2), by using the De Giorgi method in [1,18]. Another point is different from the method in [19]; thanks to the local well-posedness theory and the logarithmic Sobolev inequality, we need only to prove that r is bounded in L 2 .0, T; L 1 .R 2 // in order to extend the local solution to the global one (Theorem 3.2), which will be guaranteed by the fact that  is Hölder continuous as shown previously (Proposition 4.1).…”
Section: Introductionmentioning
confidence: 78%
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“…which is not enough to extend continuously the solution .u, Â/ beyond the time T. Fortunately, the 2D Euler equations in (1.1) provide the uniformly estimates (Theorem 3.2) in L 1 .0, T; L 2 .R 2 // about the vorticity ! :D @ 1 u 2 @ 2 u 1 , which also leads to the key estimate in [1,18]- is Hölder continuous (Lemma 3.2), by using the De Giorgi method in [1,18]. Another point is different from the method in [19]; thanks to the local well-posedness theory and the logarithmic Sobolev inequality, we need only to prove that r is bounded in L 2 .0, T; L 1 .R 2 // in order to extend the local solution to the global one (Theorem 3.2), which will be guaranteed by the fact that  is Hölder continuous as shown previously (Proposition 4.1).…”
Section: Introductionmentioning
confidence: 78%
“…In the first equation of , the θ e 2 represents the buoyancy force. The equation of θ describes the temperature fluctuation in which the term u2scriptN2(x2) stands for stratification effects about a positive linear mean temperature profile scriptN2(x2) in the direction of gravity ; here, the real quantity scriptN(x2) is called the buoyancy or Brunt–Väisärä frequency (stratification parameter). Recall that normalΔ:=(12+22),:=(1,2),i:=xi with i =1,2, and e 2 :=(0,1).…”
Section: Introductionmentioning
confidence: 99%
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