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Stratocumulus is a type of low-altitude cloud characterized by large, lumpy, white or gray patches that often cover the sky. These clouds typically form in stable air conditions and can indicate fair weather, though they may also bring light precipitation. Stratocumulus clouds differ from cumulus clouds in that they are less vertically developed and tend to appear in layers or patches rather than as distinct, puffy formations. They are commonly found at altitudes between 2,000 and 6,500 feet.

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