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Warm air is less dense than cool air. The moisture has an interesting role to play. As a mass of air rises, it cools, but the surrounding air generally cools with altitude as well. When the rising air is moist, the moisture can eventually condense to form clouds. The condensation releases heat, which slows the rate at which the air cools. If there is enough moisture present and the surrounding air cools quickly enough, this extra heat allows the rising air mass to remain warmer than its surroundings and continue to rise. It is through this process that the towering clouds of thunderstorms form.

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