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Why does hot less dense air rise and cold more dense air sink? Also, why is hot air less dense than cold air?
If the system is not at hydrostatic equilibrium, there are also viscous forces involved, and these need to be taken into account in the momentum balance. With natural convection like this, the pressures are close to being equal, but not quite. The small difference in density results in small differences in vertical pressure gradients between the hot and cold regions, and this gives rise to the buoyant forces. When you get into natural convective heat transfer, all these factors will be taken into account in determining the flow and the heat transfer. For such a detailed analysis, see Bird, Stewart, and Lightfoot, Transport Phenomena.Scheuerf said:But if you had a region of less dense air surrounded by more dense air, why wouldn't the less dense air be filled with air from the more dense area?
As Chestermiller said ... yet in my wording.Scheuerf said:But if you had a region of less dense air surrounded by more dense air, why wouldn't the less dense air be filled with air from the more dense area?