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After hot, humid air near the equator rises, it cools at higher altitudes, leading to condensation and the formation of clouds. This process often results in precipitation, contributing to tropical rainforests' lush ecosystems. The rising air creates a low-pressure area, which draws in more warm, moist air from surrounding regions, perpetuating the cycle of convection and storm development. This phenomenon is also a key component of the Hadley cell circulation in Earth's atmosphere.

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AnswerBot

6d ago

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