From Surf Wiki (app.surf) — the open knowledge base
Cumulus mediocris cloud
Form of cumulus cloud
Form of cumulus cloud
| Field | Value |
|---|---|
| name | Cumulus mediocris cloud |
| image location | Mt Eden, Auckland2.jpg |
| image name | Cumulus mediocris clouds over Auckland, with a light precipitation shaft visible in the distance under cumulus congestus clouds. |
| abbreviation | Cu med |
| symbol | Clouds CL 2.svg |
| genus | Cumulus (heaped) |
| species | Mediocris (moderate) |
| variety | * Radiatuse |
| altitude_m | 500–3000 |
| altitude_ft | 1,500–10,000 |
| level | low |
| appearance | Low-altitude, medium height, tall as it is wide, fluffy heaps of clouds with cotton-like appearance. |
| precipitation | Uncommon rain, snow or snow pellets, but it can develop into a cumulus congestus which has a greater chance of precipitation |
Cumulus mediocris is a low- to middle-level cloud with some vertical extent (Family D1) of the genus cumulus, taller than cumulus humilis. It also may exhibit small protuberances from the top and may show the cauliflower form characteristic of cumulus clouds.
Cumulus mediocris clouds do not generally produce precipitation of more than very light intensity, but can further develop into clouds such as cumulus congestus or cumulonimbus, which do produce precipitation and severe storms.
Cumulus mediocris is also classified as a low cloud and is coded CL2 by the World Meteorological Organization.
Description
Cumulus mediocris is brilliantly white when sunlit, and is dark underneath. A single pattern-based variety, Cumulus radiatus, is sometimes seen when the individual clouds are arranged into parallel rows. The resulting formations are known as "cloud streets" and are aligned approximately parallel to the wind.
Cumulus mediocris may have precipitation-based features like virga, and may form Cumulus praecipitato clouds. The pannus supplementary feature is sometimes seen with precipitating Cumulus mediocris, but in this case the CL7 reporting code normally used with to identify pannus is usually superseded by CL2 due to the additional presence of significant vertical development. Pileus (cap cloud), velum (apron), arcus (roll or shelf cloud) and tuba (vertical column) features are also occasionally seen with Cumulus mediocris. Cumulus mediocris may form as a result of a partial transformation of altocumulus or stratocumulus. This genus and species type may also be the result of a complete transformation of stratocumulus or stratus.
Forecasting
These clouds are common in the advance of a cold front or in unstable atmospheric conditions such as an area of low pressure. They can grow into larger cumulus congestus which could bring rain and winds. The presence of cumulus mediocris in the morning or early afternoon indicates significant instability in the atmosphere which will likely lead to thunderstorms later in the afternoon or evening.
Formation
Like any Cumulus cloud, Cumulus mediocris forms via convection from thermal air columns. Pockets of air warmer than the air around them (due to ground surface irregularities or other factors) are also less dense than the air around them, and are buoyant. As the air pockets float upwards, they cool, eventually reaching their dew point and condensing, forming Cumulus humilis clouds. If the thermals are powerful enough, they will continue to push air upwards and the Cumulus humilis clouds will develop into Cumulus mediocris clouds.
References
References
- "L2 Clouds: Cumulus (Cu) of moderate/strong development". [[National Oceanic and Atmospheric Administration.
- "Meteorological Codes".
- "CL = 2".
- "Cumulus praecipitatio".
- "Mediocris_Clouds_Wolstaton".
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
Ask Mako anything about Cumulus mediocris cloud — get instant answers, deeper analysis, and related topics.
Research with MakoFree with your Surf account
Create a free account to save articles, ask Mako questions, and organize your research.
Sign up freeThis content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.
Report