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Cirrocumulus clouds are a high-altitude cloud formation characterized by small, white, rounded masses, often arranged in regular patterns. These clouds are composed of ice crystals and are typically seen in fair weather. They are one of the ten main cloud genera, classified by their altitude and appearance. Cirrocumulus clouds are part of the broader category of clouds, which are essential for the Earth's hydrologic cycle as they are the source of all precipitation.12

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