Mystery of Large Cloud Bottoms: Why Are They Flat?

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SUMMARY

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.

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  • Knowledge of dew point and condensation processes
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Why are the bottoms of large clouds flat?
 
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Because there's a layer of air there with a different temperature or pressure (depending) that's not conducive to cloud formation. It's the same reason that very tall clouds, thunderheads for instance, have flat "anvil-shaped" tops.
 
Why is this layer so abrupt instead of being like a transitional gradient?
 
in convective cloud formation, warm humid air rises until the point that it is cooled sufficiently for water to condense (i.e. reaches its dew point). This point is called the cloud base, and significant condensation will not occur below it. As long as the air has a fairly uniform temperature at a given height, and the rising air is of fairly uniform humidity, this should give a pretty flat cloud base.
 

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