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10. Buoyancy-driven flow

10.7. Stability of horizontal layers T = T 1 T = T 2 x y y = h T 1 < T 2 (hot above cold) – stable (and stably stratified) horizontal thermal layer, heat transfer – by conduction only T 1 > T 2 (cold above hot) – for some DT, unstable stratification leads to convection? Buoyancy

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