A cirrocumulus is a high-altitude cloud, usually occurring at 20,000-40,000 ft (6,000-12,000 m). The term derives from the
Latin cirrus "curl of hair", and cumulus "heaped".Like other
cumulus clouds, cirrocumulus clouds signify
convection. Unlike other
cirrus clouds, cirrocumulus include liquid water droplets, although these are in a
supercooled state. Ice crystals are also present, and typically, the ice crystals cause the supercooled water drops in the cloud to rapidly freeze, transforming the cirrocumulus into cirrostratus. This process can also produce precipitation in the form of a
virga consisting of ice or snow. Thus cirrocumulus clouds are usually short-lived.
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