Air flows from the poles to the equator primarily due to the differences in temperature and pressure between these regions. The poles are colder, causing high-pressure systems, while the equator is warmer, leading to low-pressure areas. This difference drives the movement of air, creating a circulation pattern known as the Hadley Cell, where warm air rises at the equator and cool air sinks at the poles, facilitating the flow from high to low pressure. Additionally, the Earth's rotation influences this movement through the Coriolis effect, altering wind direction.
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