Viscous fluid flow in a horizontal layee due to thermal inhomogeneity of the lower boundary
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The nature of the flow induced in a layer by thermal inhomogeneity of one of the boundaries is determined on the basis of a numerical solution of the complete Navier -Stokes equations. It is found that stable stratification effectively suppresses the generated flow.
KeywordsStatistical Physic Stratification Fluid Flow Lower Boundary Viscous Fluid
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