A heat transfer process in the atmosphere that depends upon the movement of air is convection.
Heat is conveyed through convection, a process in which heated fluids like air or water move about. When heated, most fluids have a tendency to expand, which causes them to become less dense and rise due to their enhanced buoyancy.
The consistent heating of air in a heated room or water in a kettle is due to circulation generated by this effect: heated molecules expand the space they move in by moving faster against one another, rise, and then cool and close again, increasing density and causing a corresponding sinking. The best ways to describe convection are as follows: In gases and liquids, convection takes place. Thermal energy is transferred by convection. Convection continues until the fluid is uniformly heated.
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