Nimbus cloud
From Wikipedia, the free encyclopedia
(Redirected from Nimbus (meteorology))
A nimbus cloud is a cloud that produces precipitation. Usually the precipitation reaches the ground as rain, hail, snow, or sleet. Falling precipitation may evaporate as virga. Nimbus is a Latin word meaning in cloud or rain storm. The prefix nimbo- or the suffix -nimbus indicates a precipitating cloud; for example, a nimbostratus cloud is a precipitating stratus cloud, and a cumulonimbus cloud is a precipitating cumulus cloud.
[edit] Further reading
- Smith, Alastair & Clarke, Philip (2001) Spotter's Guide to Weather. London: Usborne
[edit] External links
- "Cloud Types: common cloud classifications". WW2010. University of Illinois. http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/cld/cldtyp/home.rxml.
|
|||||||||||||||||||||||||||||
| This climatology/meteorology-related article is a stub. You can help Wikipedia by expanding it. |