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Blowup in Stagnation-point Form Solutions of the Inviscid 2d Boussinesq Equations

Published 28 Aug 2014 in math.AP | (1408.6625v3)

Abstract: The 2d Boussinesq equations model large scale atmospheric and oceanic flows. Whether its solutions develop a singularity in finite-time remains a classical open problem in mathematical fluid dynamics. In this work, blowup from smooth nontrivial initial velocities in stagnation-point form solutions of this system is established. On an infinite strip $\Omega={(x,y)\in[0,1]\times\mathbb{R}+}$, we consider velocities of the form $u=(f(t,x),-yf_x(t,x))$, with scalar temperature\, $\theta=y\rho(t,x)$. Assuming $f_x(0,x)$ attains its global maximum only at points $x_i*$ located on the boundary of $[0,1]$, general criteria for finite-time blowup of the vorticity $-yf_{xx}(t,x_i*)$ and the time integral of $f_x(t,x_i*)$ are presented. Briefly, for blowup to occur it is sufficient that $\rho(0,x)\geq0$ and $f(t,x_i)=\rho(0,x_i^)=0$, while $-yf_{xx}(0,x_i*)\neq0$. To illustrate how vorticity may suppress blowup, we also construct a family of global exact solutions. A local-existence result and additional regularity criteria in terms of the time integral of $\left|f_x(t,\cdot)\right|_{L\infty([0,1])}$ are also provided.

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