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- W2567532169 abstract "Buoyancy-driven (convective) flows above differentially cooled horizontal surfaces have a boundary-layer character with a dominant flow component directed along the surface. Combined analytical and numerical analyses of prototypical flows of this kind are presented. Motion is induced by a surface cooling (in terms of surface buoyancy or surface buoyancy flux) that varies laterally as a piecewise constant function with a step change. It is demonstrated that the unsteady Boussinesq equations of motion, thermodynamic energy, and mass conservation for particular cases of such flows admit solutions that are invariant to a stretching transformation. This property provides a class of self-similarity models for horizontal convection flows in unstratified and stratified fluids. Solutions of the models equations are in good agreement with data from high-resolution numerical simulations in which no boundary-layer approximations are made." @default.
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- W2567532169 date "2012-01-01" @default.
- W2567532169 modified "2023-09-27" @default.
- W2567532169 title "Similarity Solutions for Horizontal Convection Flow along a Discontinuously Cooled Surface" @default.
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