Abstract
A new method to simulate thermal convection in a stratified fluid flow has developed. In the present method, the compressible Navier-Stokes equations are modified, based on the assumption that flow speed is in a subsonic range. The basic equations are obtained similar to the incompressible equations as a result of the formulation. Using these basic equations, thermal convection in a stratified fluid flow is simulated with a multidirectional finite-difference method in 3-dimensional Cartesian coordinates system.
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