Etymology:
Meaning:
Origin:
Cirrocumulus clouds are formed by the condensation of water vapor at high altitudes, typically between 5,000 and 12,000 meters (16,000 and 39,000 feet). They are usually associated with stable atmospheric conditions and are often seen on clear or partly cloudy days.
The name "cirrocumulus" was first used by Luke Howard in his 1802 work "On the Modifications of Clouds." Howard classified clouds based on their shape and altitude, and cirrocumulus was one of the 14 cloud types he identified.
Characteristics:
Cirrocumulus clouds are typically white or pale gray in color and have a delicate, wispy appearance. They are often arranged in rows or patches, and their individual elements may appear to be merging or dissolving. Cirrocumulus clouds are typically thin and transparent, allowing sunlight to pass through them.
These clouds are composed of ice crystals and are often associated with fair weather. However, they can occasionally indicate the approach of a warm front or a change in the weather.
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