2009
DOI: 10.1142/s0219530509001414
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Well-Posedness of the Infinite Prandtl Number Model for Convection With Temperature-Dependent Viscosity

Abstract: We establish the well-posedness of the infinite Prandtl number model for convection with temperature-dependent viscosity, free-slip boundary condition and zero horizontal fluxes.

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Cited by 12 publications
(9 citation statements)
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“…In this paper, we consider the following Boussinesq equations, which take the form (see Diaz and Galiano, Gunzburger et al, and Turcotte and Schubert) tbolduμdivfalse(italic∇boldufalse)+boldubolduγboldgθ+p=0,divboldu=0,tθdivfalse(κθfalse)+bolduθ=0, where u = ( u 1 , u 2 ) and θ are the velocity and the temperature of the fluid, respectively. p is the hydrostatic pressures.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…In this paper, we consider the following Boussinesq equations, which take the form (see Diaz and Galiano, Gunzburger et al, and Turcotte and Schubert) tbolduμdivfalse(italic∇boldufalse)+boldubolduγboldgθ+p=0,divboldu=0,tθdivfalse(κθfalse)+bolduθ=0, where u = ( u 1 , u 2 ) and θ are the velocity and the temperature of the fluid, respectively. p is the hydrostatic pressures.…”
Section: Introductionmentioning
confidence: 99%
“…In this paper, we consider the following Boussinesq equations, which take the form (see Diaz and Galiano, 9 Gunzburger et al, 10 and Turcotte and Schubert 11 ) ∂ t u − μdivð∇uÞ þ u∇u − γgθ þ ∇p ¼ 0; divu ¼ 0;…”
Section: Introductionmentioning
confidence: 99%
“…The Boussinesq system is a system of nonlinear partial differential equations that models the thermal convection and geophysical flows and plays an important role in the atmospheric sciences and oceanographic turbulence (e.g., ). In the two‐dimensional case, the standard Boussinesq system takes the form (e.g., ) {utdiv(νu)+u·u+P=θe2,e2=(0,1),divu=0,θtdiv(κθ)+u·θ=0, where u = ( u 1 , u 2 ) is the velocity vector field, ui=ui(x,t)3.0235pt(i=1,2),3.0235pt(x,t)double-struckR2×(0,+), θ ( x , t ), and P ( x , t ) denote the scalar temperature and pressure of the fluid, respectively. The unknown function θ e 2 represents the buoyancy force.…”
Section: Introductionmentioning
confidence: 99%
“…The Boussinesq system is a system of nonlinear partial differential equations that models the thermal convection and geophysical flows and plays an important role in the atmospheric sciences and oceanographic turbulence (e.g., [1][2][3]). In the two-dimensional case, the standard Boussinesq system takes the form (e.g., [4][5][6]) 8 < : u t div. ru/ C u ru C rP D Âe 2 , e 2 D .0, 1/, div u D 0, and further proved the global existence and large time asymptotic behavior.…”
Section: Introductionmentioning
confidence: 99%
“…From the mathematical point of view it has recently been proven that convection problems in which viscosity is a function of temperature is a well posed problem [16,17] for dependences which are smooth bounded positive analytical functions, so it stands a good chance of solution on a computer using a stable algorithm. The variability in viscosity introduces strong couplings between the momentum and heat equations, as well as introducing important nonlinearities into the whole problem.…”
Section: Introductionmentioning
confidence: 99%