
The transfer of heat by the physical movement of fluid, often driving atmospheric mixing.Convection is the transfer of heat through the bulk movement of a fluid—liquid or gas. When a fluid is heated from below, it expands, becomes less dense, and rises; cooler, denser fluid sinks to take its place, setting up a circulation loop. This process drives atmospheric weather, ocean currents, and mantle tectonics, and it is also central to many engineering systems, from boiling water to cooling electronics.
The phenomenon was described by Count Rumford in 1797, but the first quantitative experiments were done by Henri Bénard in 1900, and Lord Rayleigh developed the theoretical criterion for convection onset in 1916.
The driving force is buoyancy: a parcel of fluid that is warmer than its surroundings is less dense and experiences an upward force. As it rises, it carries heat with it, and cooler fluid flows in to replace it. This creates convection cells, whose size and shape depend on the temperature difference, fluid properties, and geometry. In turbulent convection, the flow becomes chaotic, with swirling eddies that mix heat much more efficiently than simple conduction.
Convection governs heat transfer in nuclear reactors, computer cooling systems, and atmospheric circulation models; it also explains why hot air balloons rise.
On the Sun, convection in the outer layers transports heat from the core to the surface, creating the granular pattern visible on the solar photosphere.












