Stratocumulus clouds are low, lumpy clouds that often appear in patches or layers. They typically form at altitudes between 2,000 and 6,500 feet and can cover large areas of the sky. These clouds are usually white or gray and can indicate fair weather, although they may also bring light rain or drizzle. Stratocumulus clouds are formed when warm, moist air rises and cools, leading to condensation. They are different from cumulus clouds, which are puffier and more vertical. Observing stratocumulus can help in understanding local weather patterns and atmospheric conditions.