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When moist air rises, it expands and cools due to the decrease in atmospheric pressure at higher altitudes. As the air cools, the water vapor it contains can condense into tiny droplets, forming clouds. This process releases latent heat, which can further enhance the upward motion of the air, potentially leading to the development of storms or precipitation. If the rising continues, it can result in various weather phenomena, such as rain or thunderstorms.

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1w ago

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