Thermal Convection
Thermal convection is the process by which heat is transferred through fluids, such as liquids and gases. When a fluid is heated, it becomes less dense and rises, while cooler, denser fluid sinks. This movement creates a circulation pattern, allowing heat to distribute evenly throughout the fluid.
In nature, thermal convection is responsible for various phenomena, including ocean currents and weather patterns. For example, warm air rising and cool air sinking contributes to the formation of wind and can lead to the development of storms. This process plays a crucial role in regulating temperatures in the environment.