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| Stratocumulus clouds | |
|---|---|
 Aerial photograph of Stratocumulus perlucidus clouds over the midwestern United States | |
| Abbreviation | Sc |
| Symbol |  |
| Genus | Stratocumulus (layer heap) |
| Species |
|
| Variety |
|
| Altitude | 500-2,000 m (2,000-7,000 ft) |
| Classification | Family C (Low-level) |
| Appearance | Thicker, dark gray, and somewhat conjoined heaps of clouds. |
| Precipitation | UncommonRain,Snow orSnow pellets |
Astratocumuluscloud, occasionally called acumulostratus, belongs to a genus-type of clouds characterized by large dark, rounded masses, usually in groups, lines, or waves, the individual elements being larger than those inaltocumulus, and the whole being at a lower height, usually below 2,000 metres (6,600 ft).[1][2] Weakconvectivecurrents create shallow cloud layers (see also:sea of clouds) because of drier, stable air above preventing continued vertical development. Historically, in English, this type of cloud has been referred to as atwain cloud for being a combination of two types of clouds.
Stratocumulus clouds are rounded clumps or patches of white to dark gray clouds that normally form in groups. The individual cloud elements, which cover more than 5 degrees of arc each, can connect with each other and are sometimes arranged in a regular pattern.[3][4][5]
Vast areas of subtropical andpolaroceans are covered with massive sheets of stratocumulus. These may organize into distinctive patterns which are currently under active study. In subtropics, they cover the edges of thehorse latitude climatological highs, and reduce the amount of solar energy absorbed in the ocean. When these drift over land the summer heat or winter cold is reduced. 'Dull weather' is a common expression incorporated with overcast stratocumulus days, which usually occur either in awarm sector between a warm and cold front in a depression, or in an area of high pressure, in the latter case, sometimes persisting over a specific area for several days. If the air over land is moist and hot enough, stratocumulus may develop to variouscumulus clouds, or, more commonly, the sheet of stratocumulus may become thick enough to produce some light rain. On drier areas they quickly dissipate over land, resemblingcumulus humilis. This often occurs in late morning in areas under anticyclonic weather, the stratocumulus breaking up under the sun's heat and often reforming again by evening as the heat of the sun decreases again.
Most often, stratocumulus produce no precipitation, and when they do, it is generally only lightrain orsnow. However, these clouds are often seen at either the front or tail end of worse weather, so they may indicate storms to come, in the form ofthunderheads orgusty winds. They are also often seen underneath the cirrostratus and altostratus sheets that often precede a warm front, as these higher clouds decrease the sun's heat and therefore convection, causing any cumulus clouds to spread out into stratocumulus clouds.
Stratocumulus clouds are similar in appearance toaltocumulus and can be mistaken for such. A simple test to distinguish these is to compare the size of individual masses or rolls: when pointing one's hand in the direction of the cloud, if the cloud is about the size of the thumb, it is altocumulus; if it is the size of one's fist, it is stratocumulus.[3] This often does not apply when stratocumulus is of a broken, fractus form, when it may appear as small as altocumulus.
Stratocumulus clouds are the main type of cloud that can producecrepuscular rays. Thin stratocumulus clouds are also often the cause ofcorona effects around the Moon at night. All stratocumulus subtypes are coded CL5 except when formed from free convective mother clouds (CL4) or when formed separately from co-existing (CL8).
Stratocumulus clouds usually form from the rising and breakup of astratus cloud.[3][6] They can also form fromaltostratus andnimbostratus clouds, either as evaporating precipitation condenses into a cloud or as the nimbostratus cloud itself thins and breaks up. If a cumulus cloud becomes flattened (for example, bywind shear ortemperature inversion), it too can become a stratocumulus cloud.[6]
Stratocumulus Stratiformis are extensive flat but slightly lumpy sheets that show only minimal convective activity.
Stratocumulus Lenticularis are separate flat elongated seed-shaped clouds. They are typical for polar countries or warmer climate during winter seasons. They also can be formed by winds passing hills or mountains, such asFoehn winds, and in this case they can be very regularly shaped.
Stratocumulus Castellanus have stronger convective activity due to the presence of increasingly unstable air. They are distinct from other stratocumulus by puffy tower-like formations atop the cloud layer.[7] They look likecumulus congestus, but can be easily confused: "towers" of cumulus congestus grow above separate clouds, whereas in the case of stratocumulus castellanus, there is always a more or less defined layer of clouds. Stratocumulus castellanus may develop into cumulus congestus (and even further intocumulonimbus) under auspicious conditions. Any showers from stratocumulus castellanus are not usually as heavy as those from cumulus congestus.
Stratocumulus Opacus is a dark layer of clouds covering entire sky without any break. However, the cloud sheet is not completely uniform, so that separate cloud bases still can be seen. This is the main precipitating type, however any rain is usually light. If the cloud layer becomes grayer to the point when individual clouds cannot be distinguished, stratocumulus turn intostratus clouds.
Stratocumulus Perlucidus is a layer of stratocumulus clouds with small spaces, appearing in irregular pattern, through which clear sky or higher clouds can be seen.
Stratocumulus Translucidus consist of separate groups of stratocumulus clouds, with a clear sky (or higher clouds) visible between them. No precipitation in most cases.[8]
Stratocumulus Undulatus clouds appear as nearly parallel waves, rolls or separate elongated clouds, without significant vertical development.[8]
Stratocumulus Radiatus clouds appear as the same as stratocumulus undulatus, but stratocumulus undulatus move perpendicular to the wind shear, while stratocumulus radiatus move parallel to the wind shear.
Stratocumulus Duplicatus clouds appear as stratocumulus clouds with two or more layers or sheets. Stratocumulus duplicatus is common on species lenticularis orlenticular cloud.
Stratocumulus Lacunosus clouds are very uncommon. They only occur when there are localizeddowndrafts striking through the stratocumuliform cloud.
Stratocumulus Mamma is a type ofmammatus cloud.[9]
Stratocumulus Asperitas is a rare, newly recognized supplementary feature that presents itself as chaotic, wavy undulations appearing in the base of a stratocumulus cloud cover. It is thought these clouds are formed by severe wind shear.
Stratocumulus Fluctus is also a rare, newly recognized supplementary feature in which short-lived "sea waves" form on top of a stratocumulus cloud, they are caused by wind speed and direction differences directly under and over the cloud.
Stratocumulus Virga is a form of precipitation that evaporates in mid-air and doesn't reach the ground.
Stratocumulus Praecipitatio is a form of precipitation that reaches the ground as light rain or snow.
Stratocumulus Cumulomutatus the specific type of stratocumulus clouds, are flat and elongated. They form in the evening, when updrafts caused by convection decrease makingcumulus clouds lose vertical development and spread horizontally. They also can occur underaltostratus cloud preceding a warm or occluded front, when cumulus usually lose vertical development as the sun's heat decreases. Like all other forms of stratocumulus apart from castellanus, they are also often found inanticyclones.
Stratocumulus Cumulogenitus out ofcumulus orcumulonimbus clouds, disrupted by decreasing convection. During formation period, puffy tops of cumulus clouds can protrude from stratocumulus cumulogenitus for a relatively long time until they completely spread in horizontal direction. Stratocumulus cumulogenitus appear as lengthy sheet or as group of separate elongated cloud rolls or waves.
In 2019, a study employed alarge eddy simulation model to estimate that equatorial stratocumulus clouds could break up and scatter whenCO2 levels rise above 1,200 ppm (almost three times higher than the current levels, and over 4 times greater than the preindustrial levels). The study estimated that this would cause a surface warming of about 8 °C (14 °F) globally and 10 °C (18 °F) in the subtropics, which would be in addition to at least 4 °C (7.2 °F) already caused by such CO2 concentrations. In addition, stratocumulus clouds would not reform until the CO2 concentrations drop to a much lower level.[10] It was suggested that this finding could help explain past episodes of unusually rapid warming such asPaleocene-Eocene Thermal Maximum.[11] In 2020, further work from the same authors revealed that in their large eddy simulation, thistipping point cannot be stopped withsolar radiation modification: in a hypothetical scenario where very high CO2 emissions continue for a long time but are offset with extensive solar radiation modification, the break-up of stratocumulus clouds is simply delayed until CO2 concentrations hit 1,700 ppm, at which point it would still cause around 5 °C (9.0 °F) of unavoidable warming.[12]
However, because large eddy simulation models are simpler and smaller-scale than thegeneral circulation models used for climate projections, with limited representation of atmospheric processes likesubsidence, this finding is currently considered speculative.[13] Other scientists say that the model used in that study unrealistically extrapolates the behavior of small cloud areas onto all cloud decks, and that it is incapable of simulating anything other than a rapid transition, with some comparing it to "a knob with two settings".[14] Additionally, CO2 concentrations would only reach 1,200 ppm if the world followsRepresentative Concentration Pathway 8.5, which represents the highest possible greenhouse gas emission scenario and involves a massive expansion ofcoal infrastructure. In that case, 1,200 ppm would be passed shortly after 2100.[13]
