A pileus (Latin for cap) is a small, horizontal cloud that can appear above a cumulus or cumulonimbus cloud, giving the parent cloud a characteristic "hoodlike" appearance. Pilei tend to change shape rapidly.[citation needed] They are formed by strong updrafts acting upon moist air at lower altitudes, causing the air to cool to its dewpoint. As such, they are usually indicators of severe weather, and a pileus found atop a cumulus cloud often foreshadows transformation into a cumulonimbus cloud, as it indicates a strong updraft within the cloud.
Clouds that are attached to pileus are often given the suffix "pileus" or "with pileus". For example, a cumulonimbus cloud with a pileus attached to it would be called "cumulonimbus with pileus".
Pilei can also form above ash clouds from erupting volcanoes (see the image to the right).
See also
References
| Wikimedia Commons has media related to: Pileus |
- Factbytes article on cumulonimbus clouds - An interesting, if sparse, resource on the various types of cumulonimbus clouds.
|
|||||||||||||||||
| This climatology/meteorology-related article is a stub. You can help Wikipedia by expanding it. |
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)




