Cumulus Cloud
Cumulus clouds are a type of low-level cloud that can have noticeable vertical development and clearly defined edges. Cumulo- means "heap" in Latin. They are often described as "puffy" or "cotton-like" in appearance, and are generally less than 6,500 feet (2,000 m) in altitude, unless they are of the vertical cumulus congestus form. Cumulus clouds may appear alone, in lines, or in clusters. Cumulus clouds are often precursors of other types of clouds, such as cumulonimbus, when influenced by weather factors such as instability, moisture, and temperature gradient. Cumulus clouds are part of the larger category of cumuliform clouds, which include stratocumulus clouds, cumulonimbus clouds, cirrocumulus clouds, and altocumulus clouds.
Read more about Cumulus Cloud: Formation, Description, Forecast, Effects On Climate, Relation To Other Clouds
Famous quotes containing the word cloud:
“The sea was wet as wet could be,
The sands were dry as dry.
You could not see a cloud, because
No cloud was in the sky:
No birds were flying overhead
There were no birds to fly.”
—Lewis Carroll [Charles Lutwidge Dodgson] (18321898)