text size: small medium large Clouds form when the air temperature reaches the condensation point or dew point, which is the point at which water vapor becomes a liquid. When it reaches this point, the liquid collects on dust particles in the air and become visible. If the temperature is far below freezing ice crystals will form instead of water droplets.
An Englishman named Luke Howard (1773-1864) developed a classification for clouds that is still largely in use. Howard noted that there are three basic shapes to clouds:
- heaps of separated cloud masses with flat bottoms and cauliflower tops, which he named Cumulus (Latin for heap);
- layers of cloud much wider than they are thick, like a blanket or a mattress, which he named Stratus (Latin for layer);
- wispy curls, like a child's hair, which he called Cirrus (Latin for curl).
- To clouds generating precipitation, he gave the name Nimbus (Latin for rain).
| Heaps: Cumulus family
fair weather cumulus swelling cumulus cumulus congestus |
Layers: Stratus family
stratus altostratus cirrostratus |
Layered Heaps
stratocumulus altocumulus cirrocumulus |
Precipitating clouds
cumulonimbus cirrus nimbostratus |
High clouds include Cirrus, Cirrocumulus, and Cirrostratus. These are higher than 18,000 feet.
Middle clouds include Altostratus, Altocumulus. These can range in height from 6,000 feet to 20,000 feet.
Low clouds include Stratus, Nimbostratus, and fair weather Cumulus. These are typically below 6,000 feet.
The Cumulonimbus is in a special category since Cumulus clouds can grow to over 60,000 feet high!


