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Global convection currents between the equator and the poles are primarily driven by the uneven heating of the Earth's surface by the sun. At the equator, the intense solar radiation warms the air, causing it to rise and create a low-pressure area. As this warm air rises and moves poleward, it cools and sinks at higher latitudes, creating a circulation pattern known as the Hadley, Ferrel, and Polar cells. The Coriolis effect also influences these currents, causing them to curve and contributing to the establishment of prevailing winds.

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1mo ago

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