Atmospheric

Heat Transfer Atmospheric heat transfer is the movement of heat energy between the atmosphere and the surface of the Earth. This heat transfer occurs through radiation, convection, and evaporation processes. The processes are essential to the climate of the Earth's surface, since they allow the Earth to maintain a livable temperature. Heat transfer is also important for the production of wind and clouds, as well as for the circulation of ocean currents. As a result, atmospheric heat transfer plays a significant role in the global climate system, helping to regulate temperature and moisture levels. In addition, it has a direct impact on the environment, from air quality to the growth of plants and animals on land, in the sea and in the atmosphere.