Stratocumulus clouds are low, puffy clouds that form in a layer, often covering large portions of the sky. They are typically found between 1,000 and 6,500 feet (300 to 2,000 meters) above the ground and consist primarily of water droplets, though ice crystals can also be present at higher altitudes. Stratocumulus clouds often appear as thick, white or gray masses with a rounded, lumpy shape. They are generally less dense and less vertically developed than cumulonimbus clouds, but they can still bring light precipitation, such as drizzle or light rain, especially if they thicken. While stratocumulus clouds don’t usually produce heavy storms, they can lead to overcast skies and periods of gloomy weather.
