1. Large-scale circulation consisting of warm air that rises near the equator and moves poleward in the upper troposphere creating a low-pressure belt at the equator
2. As it rises to the top of the troposphere, the air cools to the same temperature as its surroundings and begins to flow toward the north and south poles
3. The cooled air descends gently again to reach the Earth's surface at around 30 degrees North and 30 degrees South, creating a zone of high subtropical atmospheric pressure
4. The air thus compressed and heated prevents the formation of clouds, resulting in clear skies, high temperature at the Earth's surface, permanent dry weather, and the formation of large tropical deserts