Editing Cumulonimbus cloud

{{Short description|Genus of dense, towering vertical clouds}}
{{Redirect|Thundercloud|the song by LSD|Thunderclouds (song)}}
{{Infobox cloud
| name = Cumulonimbus
| image location = Fly00890 - Flickr - NOAA Photo Library.jpg
| image name = ''Cumulonimbus incus''
| abbreviation = Cb.
| symbol = Clouds_CL_9.svg
| genus=Cumulonimbus (''heap, rain'')
| species= * [[Cumulonimbus calvus|Calvus]]
* [[Cumulonimbus capillatus|Capillatus]]
| variety = None
<!-- Please do not change the values in the altitude parameters without citing a reliable source that verifies the information -->
| altitude_m = 500–16,000
| altitude_ft = 2,000–52,000
| level = vertical
| appearance = Dark-based storm cloud capable of impressive vertical growth.
| precipitation = Very common [[rain]], [[snow]], [[snow pellets]], or [[hail]], heavy at times
}}
{{Weather}}
'''Cumulonimbus''' ({{etymology|la|{{Wikt-lang|la|cumulus}}|swell||{{Wikt-lang|la|nimbus}}|cloud}}) is a dense, towering, vertical [[cloud]],<ref name="Cumulonimbus">{{cite book |editor=[[World Meteorological Organization]] |title=Cumulonimbus, International Cloud Atlas |volume=I |year=1975 |url=https://archive.org/details/manualonobservat00worl/page/48 |pages=48–50 |publisher=Secretariat of the World Meteorological Organization |isbn=92-63-10407-7 |access-date=28 November 2014 }}</ref> typically forming from [[water vapor]] condensing in the lower [[troposphere]] that builds upward carried by powerful [[buoyancy|buoyant]] air currents. Above the lower portions of the cumulonimbus the water vapor becomes [[ice crystal]]s, such as [[snow]] and [[graupel]], the interaction of which can lead to [[hail]] and to [[lightning]] formation, respectively.

When causing [[thunderstorm]]s, these clouds may be called '''thunderheads'''. Cumulonimbus can form alone, in clusters, or along [[squall line]]s. These clouds are capable of producing lightning and other dangerous [[severe weather]], such as [[tornado]]es, hazardous [[wind]]s, and large hailstones. Cumulonimbus progress from overdeveloped [[cumulus congestus cloud]]s and may further develop as part of a [[supercell]]. Cumulonimbus is abbreviated as '''Cb'''.

== Description ==
[[File:Large cloud over Mexican landscape.jpg|upright=1.2|thumb|A cumulonimbus calvus over [[El Bajío]], Guanajuato, Mexico.]]
Towering cumulonimbus clouds are typically accompanied by smaller [[cumulus cloud]]s. The cumulonimbus [[cloud base|base]] may extend several kilometres (miles) across, or be as small as several tens of metres (yards) across, and occupy low to upper altitudes within the troposphere - formed at altitude from approximately {{convert|200|to|4000|m|ft|abbr=on|sigfig=1}}. Normal peaks usually reach to as much as {{convert|12000|m|ft|abbr=on}}, with unusually high ones typically topping out around {{convert|20000|m|ft|abbr=on}}   <ref>[https://spaceplace.nasa.gov/review/posters/GOES_clouds/goes-r-cloudsat-front-8x11.pdf Wild World of Clouds] Cloudsat, NASA.com</ref> and extreme instances claimed to be as high as {{convert|21000|m|ft|abbr=on}} or more.<ref>{{cite web |url=http://www.theweatherprediction.com/habyhints2/536/ |title=Factors Influencing Thunderstorm Height |last1=Haby |first1=Jeff |publisher=theweatherprediction.com |access-date=15 July 2016 |archive-date=13 August 2020 |archive-url=https://web.archive.org/web/20200813031146/http://theweatherprediction.com/habyhints2/536/ |url-status=live }}</ref> Well-developed cumulonimbus clouds are characterized by a flat, [[anvil]] shaped top (anvil dome), caused by [[wind shear]] or [[Inversion (meteorology)|inversion]] at the [[equilibrium level]] near the [[tropopause]]. The shelf of the anvil may precede the main cloud's vertical component for many kilometres (miles), and be accompanied by lightning. Occasionally, rising air parcels surpass the equilibrium level (due to momentum) and form an [[overshooting top]] culminating at the [[maximum parcel level]]. When vertically developed, this largest of all clouds usually extends through all three cloud regions. Even the smallest cumulonimbus cloud dwarfs its neighbors in comparison.

=== Subtypes ===
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==== Species ====
* [[Cumulonimbus calvus]]: cloud with puffy top, similar to cumulus congestus which it develops from; under the correct conditions it can become a cumulonimbus capillatus.
* [[Cumulonimbus capillatus]]: cloud with cirrus-like, fibrous-edged top.<ref name="Species">{{cite book|editor=World Meteorological Organization|editor-link=World Meteorological Organization|title=Species, International Cloud Atlas|volume=I|year=1975|url=https://archive.org/details/manualonobservat00worl/page/17|pages=[https://archive.org/details/manualonobservat00worl/page/17 17–20]|publisher=Secretariat of the World Meteorological Organization |isbn=92-63-10407-7|access-date=26 August 2014}}</ref>

<gallery mode="packed">

File:Wagga-Cumulonimbus.jpg|Cumulonimbus calvus
Storm cloud.jpg|A clearly developed cumulonimbus fibrous-edged top capillatus
</gallery>

==== Types ====
* [[Cumulonimbus flammagenitus]] (pyrocumulonimbus): rapidly growing cloud forming from non-atmospheric heat and condensation nuclei sources such as [[wildfire]]s and [[volcanic eruption]]s.
[[File:Willow Fire AZ 7 8 2004 SE burnout 035-001.jpg|thumb|center|Pyrocumulonimbus with pileus]]

==== Supplementary features ====

=====Accessory clouds=====
* [[Arcus cloud|Arcus]] (including [[Arcus cloud#Roll cloud|roll]] and [[Arcus cloud#Shelf cloud|shelf]] clouds): low, horizontal cloud formation associated with the leading edge of thunderstorm [[Outflow (meteorology)|outflow]].<ref>{{cite book|title=National Audubon Society Field Guide to Weather|year=2000|publisher=Alfred A. Knopf|isbn=0-679-40851-7|oclc=56559729|last=Ludlum|first=David McWilliams|page=[https://archive.org/details/audubonsocietyfi00ludl/page/473 473]|url=https://archive.org/details/audubonsocietyfi00ludl/page/473}}</ref>
* [[Fractus cloud|Pannus]]: accompanied by a lower layer of fractus species cloud forming in precipitation.<ref>{{cite encyclopedia|editor-first=Michael|editor-last=Allaby|encyclopedia=A Dictionary of Ecology|title=Pannus|url=http://www.oxfordreference.com/view/10.1093/acref/9780199567669.001.0001/acref-9780199567669-e-4082|edition=4|year=2010|publisher=[[Oxford University Press]]|isbn=9780199567669|access-date=2014-08-10|archive-date=2015-09-24|archive-url=https://web.archive.org/web/20150924120253/http://www.oxfordreference.com/view/10.1093/acref/9780199567669.001.0001/acref-9780199567669-e-4082|url-status=live}}</ref>
* [[Pileus (meteorology)|Pileus]] (species calvus only): small cap-like cloud over parent cumulonimbus.
* [[Cumulonimbus velum|Velum]]: a thin horizontal sheet that forms around the middle of a cumulonimbus.<ref name="Features">{{cite book|editor=World Meteorological Organization|editor-link=World Meteorological Organization|title=Features, International Cloud Atlas|volume=I|year=1975|url=https://archive.org/details/manualonobservat00worl/page/22|pages=[https://archive.org/details/manualonobservat00worl/page/22 22–24]|publisher=Secretariat of the World Meteorological Organization |isbn=92-63-10407-7|access-date=26 August 2014}}</ref>

=====Supplementary features=====
* [[Cumulonimbus incus|Incus]] (species capillatus only): cumulonimbus with flat anvil-like cirriform top caused by wind shear where the rising air currents hit the [[inversion (meteorology)|inversion]] layer at the tropopause.<ref>{{cite web|url=http://epod.usra.edu/blog/2009/08/cumulonimbus-incus.html|title=Cumulonimbus Incus|date=5 August 2009|publisher=Universities Space Research Association|access-date=23 October 2012|archive-date=28 June 2012|archive-url=https://web.archive.org/web/20120628015404/http://epod.usra.edu/blog/2009/08/cumulonimbus-incus.html|url-status=live}}</ref>
* Mamma or [[Mammatus cloud|mammatus]]: consisting of bubble-like protrusions on the underside.
* Tuba: column hanging from the cloud base which can develop into a [[funnel cloud]] or tornado. They are known to drop very low, sometimes just {{convert|20|ft|m|order=flip|0}} above ground level.<ref name="Features"/>
* [[Flanking line (meteorology)|Flanking line]] is a line of small cumulonimbus or cumulus generally associated with severe thunderstorms.
* An [[overshooting top]] is a dome that rises above the thunderstorm; it is associated with severe weather.

=====Precipitation-based supplementary features=====
* [[Rain]]: precipitation that reaches the ground as liquid, often in a [[precipitation shaft]].<ref>{{cite book|first=Storm |last=Dunlop |year=2003 |title=The Weather Identification Handbook |pages=77–78 |publisher=[[The Lyons Press]] |isbn=1585748579}}</ref>
* [[Virga]]: precipitation that evaporates before reaching the ground.<ref name="Features"/>

<gallery mode="packed" heights="150">
File:Rolling-thunder-cloud.jpg|Arcus cloud (shelf cloud) leading a thunderstorm
File:Fly00890 - Flickr - NOAA Photo Library.jpg|Incus with a velum edge
File:Mammatus clouds regina sk june 2012.JPG|Mammatocumulus with drooping pouches
File:Cumulonimbus tuba.jpg|A funnel cloud (tuba) over the Netherlands
File:Anvil shaped cumulus panorama edit.jpg|Flanking line in front of a strong thunderstorm
File:Cumulonimbus13 - NOAA.jpg|An overshooting top is a dome of clouds atop a cumulonimbus
File:Cb virga 1.JPG|Rain evaporating before reaching the ground (virga)
</gallery>

== Effects ==
{{See also|Severe weather|Thunderstorm|Tornado|Crown flash}}
Cumulonimbus storm cells can produce torrential [[rain]] of a [[convection|convective]] nature (often in the form of a [[rain shaft]]) and [[flash flood]]ing, as well as [[straight-line winds]]. Most storm cells die after about 20&nbsp;minutes, when the [[precipitation (meteorology)|precipitation]] causes more [[downdraft]] than [[updraft]], causing the energy to dissipate. If there is sufficient instability and moisture in the [[Earth's atmosphere|atmosphere]], however (on a hot summer day, for example), the [[Outflow boundary|outflowing]] moisture and [[Gust front|gusts]] from one storm cell can lead to new cells forming just a few kilometres (miles) from the former one a few tens of minutes later or in some cases hundreds of kilometres (miles) away many hours later. This process cause thunderstorm formation (and decay) to last for several hours or even over multiple days. Cumulonimbus clouds can also occur as dangerous winter storms called "[[thundersnow]]" which are associated with particularly intense snowfall rates and with [[blizzard]] conditions when accompanied by strong winds that further reduce [[visibility]]. However, cumulonimbus clouds are most common in [[tropics|tropical]] regions and are also frequent in moist environments during the warm season in the [[middle latitudes]].<ref>{{cite web|url=https://www.nst.com.my/news/2015/09/flying-through-‘thunderstorm-alley’|title=Flying through 'Thunderstorm Alley'|url-status=dead|archive-url=https://web.archive.org/web/20180618075755/https://www.nst.com.my/news/2015/09/flying-through-%E2%80%98thunderstorm-alley%E2%80%99|archive-date=18 June 2018|date=31 December 2014|website=[[New Straits Times]]}}</ref> A [[dust storm]] caused by a cumulonimbus downburst is a [[haboob]].

=== Aviation ===
{{Main|Cumulonimbus and aviation}}
[[File:Cumulonimbo con pileus. Volando a 11.000 metros sobre Brasil.jpg|thumb|Aerial view of a cumulonimbus with pileus, flying over Brazil]]
Cumulonimbus are a notable hazard to aviation mostly due to potent wind currents but also reduced visibility and lightning, as well as [[atmospheric icing]] and hail if flying inside the cloud. Within and in the vicinity of thunderstorms there is significant [[turbulence]] and [[clear-air turbulence]] (particularly [[downwind]]), respectively. Wind shear within and under a cumulonimbus is often intense with [[downburst]]s being responsible for many accidents in earlier decades before training and technological [[Convective storm detection|detection]] and [[Nowcasting (meteorology)|nowcasting]] measures were implemented. A small form of downburst, the microburst, is the most often implicated in crashes because of their rapid onset and swift changes in wind and aerodynamic conditions over short distances. Most downbursts are associated with visible precipitation shafts, however, dry microbursts are generally invisible to the naked eye. At least one fatal commercial airline [[NLM CityHopper Flight 431|accident]] was associated with flying through a tornado.

== Life cycle or stages ==
[[File:Thunderstorm formation.jpg|thumb|300px|Stages of a cumulonimbus cloud's life.]]
[[File:Cumulus congestus to cumulonimbus incus.png|thumb|Transformation from a mature cumulus congestus cloud to a mature cumulonimbus incus]]
In general, cumulonimbus require moisture, an [[Atmospheric instability|unstable]] [[air mass]], and a lifting force in order to form. Cumulonimbus typically go through three stages: the '''developing stage''', the '''mature stage''' (where the main cloud may reach supercell status in favorable conditions), and the '''dissipation stage'''.<ref name="Extreme Weather">{{cite book |title=Extreme Weather |author=Michael H. Mogil |year=2007 |publisher=Black Dog & Leventhal Publisher |location=New York |isbn=978-1-57912-743-5 |pages=[https://archive.org/details/extremeweatherun0000mogi/page/210 210–211] |url=https://archive.org/details/extremeweatherun0000mogi/page/210 }}</ref> The average thunderstorm has a {{convert|24|km|mi|abbr=on}} diameter and a height of approximately {{convert|12.2|km|ft|abbr=on}}. Depending on the conditions present in the atmosphere, these three stages take an average of 30 minutes to go through.<ref name="tsbasics">{{cite web |url=http://www.nssl.noaa.gov/primer/tstorm/tst_basics.html |title=A Severe Weather Primer: Questions and Answers about Thunderstorms |author=National Severe Storms Laboratory |publisher=[[National Oceanic and Atmospheric Administration]] |date=15 October 2006 |access-date=1 September 2009 |archive-url=https://web.archive.org/web/20090825000832/http://www.nssl.noaa.gov/primer/tstorm/tst_basics.html |archive-date=25 August 2009 |url-status=dead }}</ref>

== See also ==
{{Portal|weather}}
* [[Atmospheric convection]]
* [[Atmospheric thermodynamics]]
* [[Convective instability]]
* [[Hot tower]]
* [[Lifted condensation level]] (LCL), [[convective condensation level]] (CCL), [[level of free convection]] (LFC), and [[free convective layer]] (FCL)
* [[William Rankin]]
* [[Ewa Wiśnierska]]

== References ==
{{Reflist}}

== External links ==
{{Commons category|Cumulonimbus clouds}}
* [http://www.clouds-online.com Clouds-Online.com Cloud Atlas with many photos and description of the different cloud genera]
* [https://www.metoffice.gov.uk/learning/learn-about-the-weather/thunder-and-lightning MetOffice.gov.uk Learn about thunderstorms and how cumulonimbus clouds form ]

{{Cloud types}}

{{DEFAULTSORT:Cumulonimbus Cloud}}
[[Category:Cirrus]]
[[Category:Cumulus]]
[[Category:Severe weather and convection]]