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A convection cell forms when warm air rises, creating a low-pressure area, while cooler air moves in to replace it, resulting in a circulating pattern. As the warm air rises, it cools and eventually descends, creating a continuous cycle. This movement of air generates winds, as the differences in air pressure drive the flow from high-pressure areas to low-pressure areas. The strength and direction of the winds depend on the temperature gradients and the Earth's rotation.

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