Global well-posedness for axisymmetric Boussinesq system with horizontal viscosity
Abstract
In this paper, we are concerned with the tridimensional anisotropic Boussinesq equations which can be described by equation* arrayll (∂t+u·∇)u-h u+∇ = e3,(t,x)∈R+×R3, (∂t+u·∇)=0, divu=0. array. equation* Under the assumption that the support of the axisymmetric initial data 0(r,z) does not intersect the axis (Oz), we prove the global well-posedness for this system with axisymmetric initial data. We first show the growth of the quantity r for large time by taking advantage of characteristic of transport equation. This growing property together with the horizontal smoothing effect enables us to establish H1-estimate of the velocity via the L2-energy estimate of velocity and the Maximum principle of density. Based on this, we further establish the estimate for the quantity \|ω(t)\|L:=2≤ p<∞ω(t)Lp(R3)p<∞ which implies \|∇ u(t)\|L3/2:=2≤ p<∞∇ u(t)Lp(R3)pp<∞. However, this regularity for the flow admits forbidden singularity since L (see eq-kl for the definition) seems be the minimum space for the gradient vector field u(x,t) ensuring uniqueness of flow. To bridge this gap, we exploit the space-time estimate about 2≤ p<∞∫0t\|∇ u(τ)\|Lp(R3)pdτ<∞ by making good use of the horizontal smoothing effect and micro-local techniques. The global well-posedness for the large initial data is achieved by establishing a new type space-time logarithmic inequality.
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