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Large cloud
stability at which cumulonimbus forms into cumulonimbus capillatus (fibrous-top) or cumulonimbus incus (anvil-top). Cumulonimbus calvus develops from cumulus
Cumulonimbus_calvus
Type of cumulus cloud
thunderstorm in its mature stage, succeeding the cumulonimbus calvus stage. Cumulonimbus incus is a subtype of cumulonimbus capillatus. These clouds are commonly
Cumulonimbus_incus
Genus of dense, towering vertical clouds
a cumulonimbus capillatus. Cumulonimbus capillatus: cloud with cirrus-like, fibrous-edged top. Cumulonimbus calvus A clearly developed cumulonimbus fibrous-edged
Cumulonimbus_cloud
Hazardous cloud
stage between cumulonimbus calvus and cumulonimbus incus. The name comes from the Latin word capillatus, meaning "with hair". A cumulonimbus capillatus is
Cumulonimbus_capillatus
winds, and/or tornadoes at ground level. Cumulonimbus calvus Cumulonimbus with high domed top. Cumulonimbus capillatus Towering vertical cloud with high
List_of_cloud_types
Visible mass of particles suspended in the atmosphere
cumulus may continue to grow into even more strongly convective cumulonimbus calvus (essentially a very tall congestus cloud that produces thunder),
Cloud
Topics referred to by the same term
Tanganyika, Africa Cumulonimbus calvus, a type of cloud This disambiguation page lists articles associated with the title Calvus. If an internal link
Calvus
Small, horizontal, lenticular cloud
is a small, horizontal, lenticular cloud appearing above a cumulus or cumulonimbus cloud. Pileus clouds are often short-lived, appearing for typically only
Pileus_(meteorology)
Optical phenomenon
Tenerife Parker Canyon, AZ. Aug 6th, 2022 2 iridescent clouds above a cumulonimbus calvus cloud. Seen in Khon Kaen, Thailand, on June 13th, 2026 Weather portal
Cloud_iridescence
Form of cumulus clouds
thunderstorms.[citation needed] Cumulus congestus will develop into cumulonimbus calvus under conditions of sufficient instability. This transformation can
Cumulus_congestus_cloud
Type of cumulus cloud
Cumulonimbus cauda is a type of cumulonimbus cloud, cauda is derived from Latin, meaning "tail", this cloud type may appear as a defined horizontal cloud
Caudus_cloud
Cloud formation occurring at the base of a thunderstorm
abrupt lowering of cloud that develops beneath the surrounding base of a cumulonimbus cloud and from which tornadoes sometimes form. It is typically beneath
Wall_cloud
A flanking line is an area of cumulus congestus or small cumulonimbus that mark an area of widespread updrafts on the edge of strong thunderstorms. These
Flanking_line_(meteorology)
Thunderstorm that is generally weak and usually not severe
low-pressure zone beneath the forming thunderstorm, otherwise known as a cumulonimbus cloud. In a typical thunderstorm, approximately 5×108 kg of water vapor
Air-mass_thunderstorm
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