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cumulonimbus

meteorology
Also known as: thundercloud, thunderhead

Quick Summary

Cumulonimbus clouds are a type of cloud that forms within the troposphere, the lowest layer of Earth's atmosphere where weather primarily occurs. These clouds are characterized by their vertical development, often appearing as towering domes or towers with an anvil-shaped top.123

The formation of cumulonimbus clouds is driven by atmospheric instability, where warm, moist air rises rapidly. As this air ascends, it cools, causing water vapor to condense and release latent heat, which further fuels the upward motion. This process creates strong updrafts that can carry air to great heights.2

Cumulonimbus clouds are associated with thunderstorms and are known to produce significant precipitation, lightning, and thunder. They develop from smaller cumulus clouds that grow and merge, extending throughout much of the troposphere.21

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