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Why are the bottoms of large clouds flat?
The flat bottoms of large clouds are primarily due to a layer of air with differing temperature or pressure that inhibits cloud formation. This phenomenon is similar to the flat "anvil-shaped" tops of tall clouds, such as thunderheads. The cloud base, where significant condensation occurs, is defined by the point at which warm, humid air rises and cools to its dew point. A uniform temperature and humidity at a specific height contribute to the flatness of the cloud base.
PREREQUISITESMeteorologists, atmospheric scientists, and students of meteorology seeking to understand cloud formation dynamics and the factors influencing cloud structure.