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Convection cells in Earth's atmosphere are driven by the uneven heating of the Earth's surface, causing air to warm and rise in certain areas while cooler air sinks in others. This process creates regions of low pressure where warm air ascends and high pressure where cool air descends. As warm air rises, it expands and cools, leading to cloud formation and precipitation in low-pressure systems, while descending air in high-pressure systems tends to be drier and clearer. Thus, the movement of air in convection cells is crucial for the development and dynamics of weather patterns.

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1mo ago

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