![]() ![]() The cirrocumulus type (with smaller puffs still) is found about 4 to 5 miles up.Ĭirrus clouds occur at an altitude of 4 miles or more, where the temperature is always below freezing hence, these clouds are always filled with ice crystals. Its greater distance from the ground makes the cumulus puffs appear smaller than those of stratocumulus clouds. Are you interested in learning about different kinds of clouds In this video, I share information on the different types including cirrus clouds, stratus, n. Altocumulus is a similar cloud at an altitude of 2 miles. Stratocumulus is a layered cumulus cloud about a mile above the ground. If it becomes very tall, it can form a cumulonimbus or thunderstorm cloud, with its top reaching an altitude of7 miles or more.Ĭumulus clouds can also develop in layers. Stratus clouds are like flat sheets of paper. Cumulus clouds are the clouds that look like cotton balls in the sky. They are located so high in the sky that they are formed by ice crystals. ![]() This cloud type literally bubbles upward. The main characteristics of cirrus, cumulus, and stratus clouds are: Cirrus clouds are wispy clouds. True cumulus clouds form about a mile above the surface of the Earth they often develop as sunlight heats the ground and the ground, in turn, heats the air. When these clouds rain or snow, they are called nimbostratus.Ĭirrostratus clouds lie at an altitude ofabout miles. Cirrus cloud layers are in general statically stable in an absolute sense, with lapse rates less than the moist-adiabatic rates with respect to either water or ice. Altostratus is a stratus cloud about 2 miles above the Earth. Stratus clouds look a little like wide gray blankets in the sky. Stratus clouds, which are flat or layered, are much longer and wider than they are tall. Cirrus clouds are formed at high altitudes of 8,000 12,000m. ![]()
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