Near the equator, the air tends to rise due to the intense heating of the Earth's surface. This process, known as convection, leads to the formation of the Intertropical Convergence Zone (ITCZ), where the trade winds from both hemispheres converge. As the warm, moist air rises, it cools and condenses, resulting in cloud formation and frequent precipitation. This area is characterized by low pressure and is often associated with thunderstorms and tropical rainforests. The rising air also leads to a circulation pattern that contributes to the broader atmospheric circulation known as the Hadley Cell, which influences weather patterns beyond the tropics.
in global atmospheric circulation, what do you expect the air to do near the equator?
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