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Equatorial divergence refers to the atmospheric phenomenon that occurs near the equator, where the trade winds from the Northern and Southern Hemispheres converge and then diverge at higher altitudes. This divergence leads to the upward movement of warm, moist air, which can contribute to the formation of clouds and precipitation. It plays a crucial role in the tropical circulation patterns and is associated with weather systems like the Intertropical Convergence Zone (ITCZ). Ultimately, equatorial divergence influences global climate by affecting tropical weather patterns and ocean currents.

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