general circulation theory

General circulation theory explains how Earth's atmosphere distributes heat and moisture globally through large-scale wind patterns and circulation cells. It involves the movement of air in a structured way, driven by the uneven heating of the planet, which creates high and low-pressure zones. These patterns, such as the Hadley, Ferrel, and Polar cells, help transport warm air toward the poles and cold air toward the equator, regulating climate and weather systems across the globe. This circulation is vital for maintaining the planet's climate balance and influencing regional weather phenomena.