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Cumulus cloud information


Cumulus
Small cumulus humilis clouds that can have noticeable vertical development and clearly defined edges.
AbbreviationCu
Symbol
GenusCumulus (heap)
Species
  • Fractus
  • Humilis
  • Mediocris
  • Congestus
Variety
  • Radiatuse
Altitude200–2,000 m
(1,000–6,600 ft)
ClassificationFamily C (Low-level)
AppearanceLow-altitude, fluffy heaps of clouds with cotton-like appearance.
PrecipitationUncommon rain, snow, or snow pellets

Cumulus clouds are clouds that have flat bases and are often described as puffy, cotton-like, or fluffy in appearance. Their name derives from the Latin cumulus, meaning "heap" or "pile".[1] Cumulus clouds are low-level clouds, generally less than 2,000 m (6,600 ft) in altitude unless they are the more vertical cumulus congestus form. Cumulus clouds may appear by themselves, in lines, or in clusters.

Cumulus clouds are often precursors of other types of clouds, such as cumulonimbus, when influenced by weather factors such as instability, humidity, and temperature gradient. Normally, cumulus clouds produce little or no precipitation, but they can grow into the precipitation-bearing cumulus congestus or cumulonimbus clouds. Cumulus clouds can be formed from water vapour, supercooled water droplets, or ice crystals, depending upon the ambient temperature. They come in many distinct subforms and generally cool the earth by reflecting the incoming solar radiation.

Cumulus clouds are part of the larger category of free-convective cumuliform clouds, which include cumulonimbus clouds. The latter genus-type is sometimes categorized separately as cumulonimbiform due to its more complex structure that often includes a cirriform or anvil top.[2] There are also cumuliform clouds of limited convection that comprise stratocumulus (low-étage), altocumulus (middle-étage) and cirrocumulus (high-étage).[3] These last three genus-types are sometimes classified separately as stratocumuliform.[2]

  1. ^ Cite error: The named reference CRH-NOAA was invoked but never defined (see the help page).
  2. ^ a b Barrett, E. C.; Grant, C. K. (1976). "The identification of cloud types in LANDSAT MSS images". NASA. Archived from the original on 2013-10-05. Retrieved 2012-08-22.
  3. ^ Geerts, B. (April 2000). "Cumuliform Clouds: Some Examples". Resources in Atmospheric Sciences. University of Wyoming College of Atmospheric Sciences. Retrieved 2013-02-11.

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Cumulus cloud

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Cumulus humilis are cumuliform clouds with little vertical extent, common in the summer, that are often referred to as "fair weather cumulus". If they...

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Cumulus mediocris cloud

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Fractus cloud

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of its particles. Cumulus fractus clouds actually look like ragged cumulus clouds. They may originate from dissipated cumulus clouds, appearing in this...

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Cumulus castellanus (from Latin castellanus, castle) is an unofficial name of a species of cumulus cloud that is distinctive because it displays multiple...

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Stratocumulus cloud

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nimbostratus clouds, either as evaporating precipitation condenses into a cloud or as the nimbostratus cloud itself thins and breaks up. If a cumulus cloud becomes...

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Nimbostratus cloud

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which denotes "cloud" or "halo". Downward-growing nimbostratus can have the same vertical extent as most large upward-growing cumulus, but its horizontal...

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Altocumulus cloud

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Altocumulus (from Latin altus 'high', and cumulus 'heaped') is a middle-altitude cloud genus that belongs mainly to the stratocumuliform physical category...

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Horseshoe cloud

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vortex deforms a cumulus cloud. The clouds are relatively short-lived and is the last stage before one dissipates. Horseshoe vortex clouds are a form of...

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a flammagenitus cloud. According to the American Meteorological Society’s Glossary of Meteorology, a flammagenitus is "a cumulus cloud formed by a rising...

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thermal under the base of cumulus clouds, especially towering cumulus and cumulonimbus. The vertical extent of a cumulus cloud is a good indicator of the...

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Stratus cloud

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stratiform cloud. Like stratus clouds, they form at low levels; but like cumulus clouds (and unlike stratus clouds), they form via convection. Unlike cumulus clouds...

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CSIRO scientists dropped dry ice into the tops of cumulus clouds. The method worked reliably with clouds that were very cold, producing rain that would not...

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Thermal

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indicated by the presence of visible isolated cumulus clouds at the top of the thermal. Cumulus clouds are formed by the rising air in a thermal as it...

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Flammagenitus cloud

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datacenter, cloud computing, and enterprise environments. In May 2020, American semiconductor manufacturer Nvidia announced it was acquiring Cumulus. Post acquisition...

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Cirrocumulus cloud

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both the surface of the Earth and a cumulonimbus cloud or, in rare cases, the base of a cumulus cloud. It is often referred to as a twister, whirlwind...

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Project Cumulus

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Project Cumulus was a 1950s UK government initiative to investigate weather manipulation, in particular through cloud seeding experiments. Known jokingly...

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