The main task of atmospheric circulation is to distribute heat and moisture around the Earth, maintaining Earth's climate system. It is responsible for transporting warm air from the equator to the poles and cold air from the poles to the equator, creating global winds and weather patterns. This circulation is driven by the uneven heating of the Earth's surface by the sun, which results in the formation of high and low-pressure systems, as well as the development of jet streams and trade winds. Atmospheric circulation also plays a crucial role in the distribution of precipitation and the formation of weather phenomena such as hurricanes and tornadoes.
