cumulus cloud

File:Bubbles in the Sky.ogv]]

Cumulus clouds form via atmospheric convection as air warmed by the surface begins to rise. As the air rises, the temperature drops (following the lapse rate), causing the relative humidity (RH) to rise. If convection reaches a certain level the RH reaches one hundred percent, and the "wet-adiabatic" phase begins. At this point a positive feedback ensues: since the RH is above 100%, water vapor condenses, releasing latent heat, warming the air and spurring further convection.

In this phase, water vapor condenses on various nuclei present in the air, forming the cumulus cloud. This creates the characteristic flat-bottomed puffy shape associated with cumulus clouds.{{cite news|url=http://usatoday30.usatoday.com/weather/wcumulus.htm|work=Weather|title=Cumulus clouds|access-date=16 October 2012|date=16 October 2005|archive-date=28 June 2017|archive-url=https://web.archive.org/web/20170628202558/http://usatoday30.usatoday.com/weather/wcumulus.htm|url-status=dead}}{{harvnb|Stommel|1947|p=91}} The height of the cloud (from its bottom to its top) depends on the temperature profile of the atmosphere and of the presence of any inversions.{{harvnb|Mossop|Hallett|1974|pp=632–634}} During the convection, surrounding air is entrained (mixed) with the thermal and the total mass of the ascending air increases.

Rain forms in a cumulus cloud via a process involving two non-discrete stages. The first stage occurs after the droplets coalesce onto the various nuclei. Langmuir writes that surface tension in the water droplets provides a slightly higher pressure on the droplet, raising the vapor pressure by a small amount. The increased pressure results in those droplets evaporating and the resulting water vapor condensing on the larger droplets. Due to the extremely small size of the evaporating water droplets, this process becomes largely meaningless after the larger droplets have grown to around 20 to 30 micrometres, and the second stage takes over.{{harvnb|Langmuir|1948|p=175}} In the accretion phase, the raindrop begins to fall, and other droplets collide and combine with it to increase the size of the raindrop. Langmuir was able to develop a formulaThe formula was $t=\{18\backslash eta\; \backslash over\; Egwr\_0\}$, with $t$ being the time to infinite radius, $\backslash eta$ being the viscosity of air, $E$ being the fractional percentage of water droplets accreted per unit volume of air that the drop falls through, $w$ being the concentration of water in the cloud in grams per cubic metre, and $r\_0$ being the initial radius of the droplet. which predicted that the droplet radius would grow unboundedly within a discrete time period.{{harvnb|Langmuir|1948|p=177}}

File:Brittany 01.jpg, France]]

The liquid water density within a cumulus cloud has been found to change with height above the cloud base rather than being approximately constant throughout the cloud. In one particular study, the concentration was found to be zero at cloud base. As altitude increased, the concentration rapidly increased to the maximum concentration near the middle of the cloud. The maximum concentration was found to be anything up to 1.25 grams of water per kilogram of air. The concentration slowly dropped off as altitude increased to the height of the top of the cloud, where it immediately dropped to zero again.{{harvnb|Stommel|1947|p=94}}

Cumulus clouds can form in lines stretching over {{convert|480|km|mi}} long called cloud streets. These cloud streets cover vast areas and may be broken or continuous. They form when wind shear causes horizontal circulation in the atmosphere, producing the long, tubular cloud streets.{{harvnb|Weston|1980|p=433}} They generally form during high-pressure systems, such as after a cold front.{{harvnb|Weston|1980|pp=437–438}}

The height at which the cloud forms depends on the amount of moisture in the thermal that forms the cloud. Humid air will generally result in a lower cloud base. In temperate areas, the base of the cumulus clouds is usually below {{convert|550|m|ft}} above ground level, but it can range up to {{convert|2400|m|ft}} in altitude. In arid and mountainous areas, the cloud base can be in excess of {{convert|6100|m|ft}}.

Cumulus clouds can be composed of ice crystals, water droplets, supercooled water droplets, or a mixture of them.{{cite web|title=Cloud Classification and Characteristics|url=http://www.crh.noaa.gov/lmk/?n=cloud_classification|url-status=dead|archive-url=https://web.archive.org/web/20121017002436/http://www.crh.noaa.gov/lmk/?n=Cloud_classification|archive-date=17 October 2012|access-date=18 October 2012|publisher=National Oceanic and Atmospheric Administration}}

One study found that in temperate regions, the cloud bases studied ranged from {{convert|500|to|1500|m|ft}} above ground level. These clouds were normally above {{convert|25|C|F}}, and the concentration of droplets ranged from {{convert|23|to|1300|/cm3|/cuin|abbr=off|adj=pre|droplets}}. This data was taken from growing isolated cumulus clouds that were not precipitating.{{harvnb|Warner|1969|p=1049}} The droplets were very small, ranging down to around 5 micrometres in diameter. Although smaller droplets may have been present, the measurements were not sensitive enough to detect them.{{harvnb|Warner|1969|p=1051}} The smallest droplets were found in the lower portions of the clouds, with the percentage of large droplets (around 20 to 30 micrometres) rising dramatically in the upper regions of the cloud. The droplet size distribution was slightly bimodal in nature, with peaks at the small and large droplet sizes and a slight trough in the intermediate size range. The skew was roughly neutral.{{harvnb|Warner|1969|p=1052}} Furthermore, large droplet size is roughly inversely proportional to the droplet concentration per unit volume of air.{{harvnb|Warner|1969|p=1054}}

In places, cumulus clouds can have "holes" where there are no water droplets. These can occur when winds tear the cloud and incorporate the environmental air or when strong downdrafts evaporate the water.{{harvnb|Warner|1969|p=1056}}{{harvnb|Warner|1969|p=1058}}

File:Cumulusmediocrissweden.jpg]]

Cumulus clouds come in four distinct species, cumulus humilis, mediocris, congestus, and fractus. These species may be arranged into the variety, cumulus radiatus; and may be accompanied by up to seven supplementary features, cumulus pileus, velum, virga, praecipitatio, arcus, pannus, and tuba.{{harvnb|Pretor-Pinney|2007|p=17}}

The species Cumulus fractus is ragged in appearance and can form in clear air as a precursor to cumulus humilis and larger cumulus species-types; or it can form in precipitation as the supplementary feature pannus (also called scud) which can also include stratus fractus of bad weather.{{cite web|title=L7 Clouds: Stratus fractus (StFra) and/or Cumulus fractus (CuFra) bad weather|url=http://www.srh.noaa.gov/jetstream/synoptic/l7.htm|url-status=dead|archive-url=https://web.archive.org/web/20120118151256/http://www.srh.noaa.gov/jetstream/synoptic/l7.htm|archive-date=18 January 2012|access-date=11 February 2013|work=JetStream - Online School for Weather: Cloud Classifications|publisher=National Weather Service}}{{cite encyclopedia|editor-first=Michael |editor-last=Allaby|encyclopedia=A Dictionary of Ecology|title=Pannus |edition=4th|year=2010 |publisher=Oxford University Press|isbn=978-0-19-956766-9|doi=10.1093/acref/9780199567669.001.0001}} Cumulus humilis clouds look like puffy, flattened shapes. Cumulus mediocris clouds look similar, except that they have some vertical development. Cumulus congestus clouds have a cauliflower-like structure and tower high into the atmosphere, hence their alternate name "towering cumulus". The variety Cumulus radiatus forms in radial bands called cloud streets and can comprise any of the four species of cumulus.{{harvnb|Pretor-Pinney|2007|p=20}}

Cumulus supplementary features are most commonly seen with the species congestus. Cumulus virga clouds are cumulus clouds producing virga (precipitation that evaporates while aloft), and cumulus praecipitatio produce precipitation that reaches the Earth's surface.{{harvnb|Dunlop|2003|pp=77–78}} Cumulus pannus comprise shredded clouds that normally appear beneath the parent cumulus cloud during precipitation. Cumulus arcus clouds have a gust front,{{harvnb|Ludlum|2000|p=473}} and cumulus tuba clouds have funnel clouds or tornadoes.{{harvnb|Dunlop|2003|p=79}} Cumulus pileus clouds refer to cumulus clouds that have grown so rapidly as to force the formation of pileus over the top of the cloud.{{harvnb|Garrett et al.|2006|page=i}} Cumulus velum clouds have an ice crystal veil over the growing top of the cloud.{{Cite web|url=http://www.weatheranswer.com/public/Clouds_WMO.pdf |archive-url=https://web.archive.org/web/20050226160200/http://www.weatheranswer.com/public/Clouds_WMO.pdf |archive-date=2005-02-26 |url-status=live|access-date=18 October 2012|title=WMO classification of clouds|publisher=World Meteorological Organization}}

There are also cumulus cataractagenitus, which are formed by waterfalls.{{cite web |title=Cataractagenitus |url=https://cloudatlas.wmo.int/en/cataractagenitus.html |publisher=International Cloud Atlas}}

Cumulus humilis clouds usually indicate fair weather.{{cite web|url=http://www.weather.com/glossary/c.html |title=Weather Glossary |publisher=The Weather Channel |access-date=18 October 2012 |url-status=dead |archive-url=https://web.archive.org/web/20121017165021/http://www.weather.com/glossary/c.html |archive-date=17 October 2012 }} Cumulus mediocris clouds are similar, except that they have some vertical development, which implies that they can grow into cumulus congestus or even cumulonimbus clouds, which can produce heavy rain, lightning, severe winds, hail, and even tornadoes.{{cite book|last=Thompson|first=Philip|author2=Robert O'Brien|title=Weather|url=https://archive.org/details/weather00thom|url-access=registration|publisher=Time Inc.|location=New York|year=1965|pages=[https://archive.org/details/weather00thom/page/86 86–87]}} Cumulus congestus clouds, which appear as towers, will often grow into cumulonimbus storm clouds. They can produce precipitation. Glider pilots often pay close attention to cumulus clouds, as they can be indicators of rising air drafts or thermals underneath that can suck the plane high into the sky—a phenomenon known as cloud suck.{{harvnb|Pagen|2001|pp=105–108}}

File:Anvil of Cumulonimbus and Cu con.JPG

Due to reflectivity, clouds cool the earth by around {{convert|12|C-change|abbr=on}}, an effect largely caused by stratocumulus clouds. However, at the same time, they heat the earth by around {{convert|7|C-change|abbr=on}} by reflecting emitted radiation, an effect largely caused by cirrus clouds. This averages out to a net loss of {{convert|5|C-change|abbr=on}}.{{cite web |url=http://isccp.giss.nasa.gov/role.html|title=Cloud Climatology|work=International Satellite Cloud Climatology Program|publisher=National Aeronautics and Space Administration|access-date=12 July 2011}} Cumulus clouds, on the other hand, have a variable effect on heating the Earth's surface.{{cite web|title=Will Clouds Speed or Slow Global Warming?|publisher=National Science Foundation|url=https://www.nsf.gov/news/special_reports/clouds/question.jsp|url-status=dead|archive-url=https://web.archive.org/web/20130129231359/http://www.nsf.gov/news/special_reports/clouds/question.jsp|archive-date=29 January 2013|access-date=23 October 2012}} The more vertical cumulus congestus species and cumulonimbus genus of clouds grow high into the atmosphere, carrying moisture with them, which can lead to the formation of cirrus clouds. The researchers speculated that this might even produce a positive feedback, where the increasing upper atmospheric moisture further warms the earth, resulting in an increasing number of cumulus congestus clouds carrying more moisture into the upper atmosphere.{{harvnb|Del Genfo|Lacis|Ruedy|1991|p=384}}

Cumulus clouds are a genus of free-convective low-level cloud along with the related limited-convective cloud stratocumulus. These clouds form from ground level to {{convert|2000|m|ft}} at all latitudes. Stratus clouds are also low-level. In the middle level are the alto- clouds, which consist of the limited-convective stratocumuliform cloud altocumulus and the stratiform cloud altostratus. Mid-level clouds form from {{convert|2000|m|ft}} to {{convert|7000|m|ft}} in polar areas, {{convert|7000|m|ft}} in temperate areas, and {{convert|7600|m|ft}} in tropical areas. The high-level cloud, cirrocumulus, is a stratocumuliform cloud of limited convection. The other clouds in this level are cirrus and cirrostratus. High clouds form {{convert|3000|to|7600|m|ft}} in high latitudes, {{convert|5000|to|12000|m|ft}} in temperate latitudes, and {{convert|6100|to|18000|m|ft}} in low, tropical latitudes. Cumulonimbus clouds, like cumulus congestus, extend vertically rather than remaining confined to one level.{{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}}

File:Cirrocumulus in Hong Kong.jpg

{{main article|Cirrocumulus cloud}}

Cirrocumulus clouds form in patches{{harvnb|Miyazaki|Yoshida|Dobashi|Nishita|2001|p=364}} and cannot cast shadows. They commonly appear in regular, rippling patterns{{harvnb|Hubbard|2000|p=340}} or in rows of clouds with clear areas between.{{cite web|last=Funk|first=Ted|title=Cloud Classifications and Characteristics|url=http://www.crh.noaa.gov/lmk/soo/docu/cloudchart.pdf|url-status=dead|archive-url=https://web.archive.org/web/20040720234037/http://www.crh.noaa.gov/lmk/soo/docu/cloudchart.pdf|archive-date=July 20, 2004|access-date=19 October 2012|work=The Science Corner|publisher=National Oceanic and Atmospheric Administration|page=1}} Cirrocumulus are, like other members of the cumuliform and stratocumuliform categories, formed via convective processes.{{harvnb|Parungo|1995|p=251}} Significant growth of these patches indicates high-altitude instability and can signal the approach of poorer weather. The ice crystals in the bottoms of cirrocumulus clouds tend to be in the form of hexagonal cylinders. They are not solid, but instead tend to have stepped funnels coming in from the ends. Towards the top of the cloud, these crystals have a tendency to clump together.{{harvnb|Parungo|1995|p=252}} These clouds do not last long, and they tend to change into cirrus because as the water vapor continues to deposit on the ice crystals, they eventually begin to fall, destroying the upward convection. The cloud then dissipates into cirrus.{{harvnb|Parungo|1995|p=254}} Cirrocumulus clouds come in four species which are common to all three genus-types that have limited-convective or stratocumuliform characteristics: stratiformis, lenticularis, castellanus, and floccus.{{cite web|title=Common Cloud Names, Shapes, and Altitudes|publisher=Georgia Institute of Technology|url=http://nenes.eas.gatech.edu/Cloud/Clouds.pdf|access-date=12 February 2011|pages=2, 10–13|archive-url=https://web.archive.org/web/20110512162814/http://nenes.eas.gatech.edu/Cloud/Clouds.pdf|archive-date=12 May 2011|url-status=dead}} They are iridescent when the constituent supercooled water droplets are all about the same size.{{harvnb|Ludlum|2000|p=448}}

File:Altocumulus stratiformis clouds-01.jpg

{{main article|Altocumulus cloud}}

Altocumulus clouds are a mid-level cloud that forms from {{convert|2000|m|ft}} high to {{convert|4000|m|ft}} in polar areas, {{convert|7000|m|ft}} in temperate areas, and {{convert|7600|m|ft}} in tropical areas.{{cite web|title=Cloud Classifications|url=http://oceanservice.noaa.gov/education/yos/resource/JetStream/synoptic/clouds_max.htm|url-status=dead|archive-url=https://web.archive.org/web/20141107063301/http://oceanservice.noaa.gov/education/yos/resource/JetStream/synoptic/clouds_max.htm|archive-date=7 November 2014|access-date=21 July 2014|work=JetStream|publisher=National Weather Service}} They can have precipitation and are commonly composed of a mixture of ice crystals, supercooled water droplets, and water droplets in temperate latitudes. However, the liquid water concentration was almost always significantly greater than the concentration of ice crystals, and the maximum concentration of liquid water tended to be at the top of the cloud while the ice concentrated itself at the bottom.{{harvnb|Carey et al.|2008|p=2490}}{{harvnb|Carey et al.|2008|p=2491}} The ice crystals in the base of the altocumulus clouds and in the virga were found to be dendrites or conglomerations of dendrites while needles and plates resided more towards the top. Altocumulus clouds can form via convection or via the forced uplift caused by a warm front.{{harvnb|Carey et al.|2008|p=2494}}

File:Flat Stratocumulus Cloud.jpg

{{main article|Stratocumulus cloud}}

A stratocumulus cloud is another type of stratocumuliform cloud. Like cumulus clouds, they form at low levels and via convection. However, unlike cumulus clouds, their growth is almost completely retarded by a strong inversion. As a result, they flatten out like stratus clouds, giving them a layered appearance. These clouds are extremely common, covering on average around twenty-three percent of the Earth's oceans and twelve percent of the Earth's continents. They are less common in tropical areas and commonly form after cold fronts. Additionally, stratocumulus clouds reflect a large amount of the incoming sunlight, producing a net cooling effect.{{harvnb|Wood|2012|p=2374}} Stratocumulus clouds can produce drizzle, which stabilizes the cloud by warming it and reducing turbulent mixing.{{harvnb|Wood|2012|p=2398}}

{{main article|Cumulonimbus cloud}}

Cumulonimbus clouds are the final form of growing cumulus clouds. They form when cumulus congestus clouds develop a strong updraft that propels their tops higher and higher into the atmosphere until they reach the tropopause at {{convert|18000|m|ft}} in altitude. Cumulonimbus clouds, commonly called thunderheads, can produce high winds, torrential rain, lightning, gust fronts, waterspouts, funnel clouds, and tornadoes. They commonly have anvil clouds.{{harvnb|Ludlum|2000|p=471}}

{{main article|Horseshoe cloud}}

A short-lived horseshoe cloud may occur when a horseshoe vortex deforms a cumulus cloud.{{cite web |title=An incredibly rare 'horseshoe cloud' was spotted in Nevada and it kept the meme-makers busy |url=https://www.independent.ie/world-news/and-finally/an-incredibly-rare-horseshoe-cloud-was-spotted-in-nevada-and-it-kept-the-mememakers-busy-36691086.html |website=Independent.ie |date=12 March 2018 |access-date=12 March 2018 }}

Some cumuliform and stratocumuliform clouds have been discovered on most other planets in the Solar System. On Mars, the Viking Orbiter detected cirrocumulus and stratocumulus clouds forming via convection primarily near the polar icecaps.{{cite web|url=https://history.nasa.gov/SP-441/ch12.htm|title=NASA SP-441: Viking Orbiter Views of Mars|publisher=National Aeronautics and Space Administration|access-date=26 January 2013}} The Galileo space probe detected massive cumulonimbus clouds near the Great Red Spot on Jupiter.{{cite web|url=http://photojournal.jpl.nasa.gov/catalog/pia00506|title=Thunderheads on Jupiter|work=Jet Propulsion Laboratory|publisher=National Aeronautics and Space Administration|access-date=26 January 2013}} Cumuliform clouds have also been detected on Saturn. In 2008, the Cassini spacecraft determined that cumulus clouds near Saturn's south pole were part of a cyclone over {{convert|4000|km|mi}} in diameter.{{cite news|last=Minard|first=Anne|date=14 October 2008|title=Mysterious Cyclones Seen at Both of Saturn's Poles|newspaper=National Geographic News|url=http://news.nationalgeographic.com/news/2008/10/081014-saturn-cyclones.html|url-status=dead|access-date=26 January 2013|archive-url=https://web.archive.org/web/20121123054759/http://news.nationalgeographic.com/news/2008/10/081014-saturn-cyclones.html|archive-date=23 November 2012}} The Keck Observatory detected whitish cumulus clouds on Uranus.{{cite magazine|url=http://www.popsci.com/science/article/2012-10/most-richly-detailed-image-ever-taken-icy-distant-uranus|title=Check Out The Most Richly Detailed Image Ever Taken Of Uranus|magazine=Popular Science|last=Boyle|first=Rebecca|date=18 October 2012|access-date=26 January 2013}} Like Uranus, Neptune has methane cumulus clouds.{{harvnb|Irwin|2003|p=115}} Venus, however, does not appear to have cumulus clouds.{{harvnb|Bougher|Phillips|1997|pp=127–129}}

{{Portal|Weather}}

• List of cloud types

{{reflist|group=note}}

{{reflist|30em}}

{{refbegin}}

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• {{cite book|last=Dunlop|first=Storm|url=https://books.google.com/books?id=BR2ft4G5TgQC|title=The Weather Identification Handbook|date=June 2003|publisher=Lyons Press|isbn=978-1-58574-857-0}}
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• {{cite book|last=Irwin|first=Patrick|title=Giant Planets of Our Solar System: Atmospheres, Composition, and Structure|url=https://books.google.com/books?id=p8wCsJweUb0C&pg=PA115|isbn=978-3-540-00681-7|date=July 2003 |edition=1st |publisher=Springer|page=115}}
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• {{cite book|title=National Audubon Society Field Guide to Weather|year=2000|publisher=Alfred A. Knopf |isbn=978-0-679-40851-2|oclc=56559729|last=Ludlum|first=David McWilliams|url-access=registration |url=https://archive.org/details/audubonsocietyfi00ludl}}
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• {{cite journal|last1=Mossop|first1=S. C.|last2=Hallett|first2=J.|title=Ice Crystal Concentration in Cumulus Clouds: Influence of the Drop Spectrum|volume=186|issue=4164|pages=632–634|date=November 1974|doi=10.1126/science.186.4164.632|journal=Science Magazine|bibcode=1974Sci...186..632M|pmid=17833720|s2cid=19285155 }}
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• {{cite book|last=Pretor-Pinney|first=Gavin|author-link=Gavin Pretor-Pinney|url=https://books.google.com/books?id=ix4qy7FihDcC|title=The Cloudspotter's Guide: The Science, History, and Culture of Clouds|isbn=978-1-101-20331-6|date=June 2007|publisher=Penguin Group}}
• {{cite journal|last=Stommel|first=Harry|doi=10.1175/1520-0469(1947)004<0091:EOAIAC>2.0.CO;2|title=Entrainment of Air Into a Cumulus Cloud|date=June 1947|journal=Journal of Meteorology|volume=4|issue=3|pages=91–94|bibcode=1947JAtS....4...91S|doi-access=free}}
• {{cite journal|last=Warner|first=J.|title=The Micro structure of Cumulus Cloud. Part I. General Features of the Droplet Spectrum|doi=10.1175/1520-0469(1969)026<1049:TMOCCP>2.0.CO;2|journal=Journal of the Atmospheric Sciences|date=September 1969|volume=26|issue=5|pages=1049–1059|bibcode=1969JAtS...26.1049W|doi-access=free}}
• {{cite journal|last=Weston|first=K. J.|title=An Observational Study of Convective Cloud Streets|doi=10.1111/j.2153-3490.1980.tb00970.x|date=October 1980|journal=Tell Us|volume=32|issue=35|pages=433–438|bibcode=1980Tell...32..433W}}
• {{cite journal|last=Wood|first=Robert|title=Stratocumulus Clouds|journal=Monthly Weather Review|doi=10.1175/MWR-D-11-00121.1|date=August 2012|volume=140|issue=8|pages=2373–2423|bibcode=2012MWRv..140.2373W|doi-access=free}}

{{refend}}

{{commons category|Cumulus clouds}}

• [http://glossary.ametsoc.org/wiki/Main_Page AMS Glossary of Meteorology]

{{Cloud types}}

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{{DEFAULTSORT:Cumulus Cloud}}

Category:Cloud types

Category:Articles containing video clips