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Cumulonimbus capillatus incus
|Genus||Cumulonimbus (heap, storm/rain)|
|Classification||Family D (Vertically developed)|
|Appearance||Very tall and large clouds|
|Precipitation cloud?||Yes, often intense, but may be virga (virga—occasionally a streak of precipitation but evaporates before it hits the ground)|
Cumulonimbus, from the Latin cumulus ("heap") and nimbus ("rainstorm", "storm cloud"), is a dense towering vertical cloud associated with thunderstorms and atmospheric instability, forming from water vapor carried by powerful upward air currents. Cumulonimbus may form alone, in clusters, or along cold front squall lines. They are capable of producing lightning and other dangerous severe weather, such as gusts, hail, and occasional tornadoes. Cumulonimbus progress from overdeveloped cumulus congestus clouds and may further develop as part of a supercell. Cumulonimbus is abbreviated Cb and are designated in the D2 family.
- Cumulonimbus calvus: cloud with puffy top, similar to cumulus congestus, but larger;
- Cumulonimbus capillatus - cloud with cirrus-like, fibrous-edged top;
- Cumulonimbus arcus.
- Cumulonimbus incus: subtype of Cumulonimbus capillatus, with flat anvil-like top.
- Cumulonimbus mammatus.
- Cumulonimbus pannus.
- Cumulonimbus pileus.
- Cumulonimbus praecipitatio.
- Cumulonimbus tuba.
- Cumulonimbus velum.
- Cumulonimbus virga.
Cumulonimbus storm cells can produce torrential rain of a convective nature and flash flooding, as well as straight-line winds. Most storm cells die after about 20 minutes, when the precipitation causes more downdraft than updraft, causing the energy to dissipate. If there is enough solar energy in the atmosphere, however (on a hot summer's day, for example), the moisture from one storm cell can evaporate rapidly—resulting in a new cell forming just a few miles from the former one. This can cause thunderstorms to last for several hours. Cumulonimbus clouds can also bring dangerous winter storms (called "blizzards") which bring lightning, thunder, and torrential snow.
Clouds form when the dewpoint of water is reached in the presence of condensation nuclei in the troposphere. The atmosphere is a dynamic system, and the local conditions of turbulence, uplift and other parameters give rise to many types of clouds. Various types of clouds occur frequently enough to have been categorized. Furthermore, some atmospheric processes can make the clouds organize in distinct patterns such as wave clouds or actinoform clouds. These are large-scale structures and are not always readily identifiable from single point of view.
Cumulonimbus incus cloud formation with anvil over Margalla Hills, Islamabad. A cirrus cloud has formed from a part of the anvil that has been broken off.
- Atmospheric convection
- Atmospheric thermodynamics
- Convective instability
- Funnel cloud
- Hot tower
- William Rankin
|Wikimedia Commons has media related to Cumulonimbus clouds.|
- Clouds-Online.com Cloud Atlas with many photos and description of the different cloud genus
- Cumulonimbus cloud at BBC Weather
- Weather Pictures and Storm Chasing – Cumulonimbus clouds