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Terrestrial clouds can be found throughout most of the homosphere , which includes the troposphere , stratosphere , and mesosphere.

Within these layers of the atmosphere , air can become saturated as a result of being cooled to its dew point or by having moisture added from an adjacent source.

The main mechanism behind this process is adiabatic cooling. This condensation normally occurs on cloud condensation nuclei such as salt or dust particles that are small enough to be held aloft by normal circulation of the air.

Frontal and cyclonic lift occur when stable air is forced aloft at weather fronts and around centers of low pressure by a process called convergence.

Another agent is the convective upward motion of air caused by daytime solar heating at surface level. A third source of lift is wind circulation forcing air over a physical barrier such as a mountain orographic lift.

However, if the air becomes sufficiently moist and unstable, orographic showers or thunderstorms may appear. Along with adiabatic cooling that requires a lifting agent, there are three major non-adiabatic mechanisms for lowering the temperature of the air to its dew point.

Conductive, radiational, and evaporative cooling require no lifting mechanism and can cause condensation at surface level resulting in the formation of fog.

There are several main sources of water vapor that can be added to the air as a way of achieving saturation without any cooling process: Tropospheric classification is based on a hierarchy of categories with physical forms and altitude levels at the top.

Clouds in the troposphere assume five physical forms based on structure and process of formation. These forms are commonly used for the purpose of satellite analysis.

Non-convective stratiform clouds appear in stable airmass conditions and, in general, have flat sheet-like structures that can form at any altitude in the troposphere.

Conversely, low stratiform cloud results when advection fog is lifted above surface level during breezy conditions.

Cirriform clouds are generally of the genus cirrus and have the appearance of detached or semi-merged filaments. They form at high tropospheric altitudes in air that is mostly stable with little or no convective activity, although denser patches may occasionally show buildups caused by limited high-level convection where the air is partly unstable.

Clouds of this structure have both cumuliform and stratiform characteristics in the form of rolls, ripples, or elements. Cumuliform clouds generally appear in isolated heaps or tufts.

In general, small cumuliform clouds tend to indicate comparatively weak instability. Larger cumuliform types are a sign of moderate to strong atmospheric instability and convective activity.

The largest free-convective clouds comprise the genus cumulonimbus which are multi-level because of their towering vertical extent.

They occur in highly unstable air [9] and often have fuzzy outlines at the upper parts of the clouds that sometimes include anvil tops.

The grouping of clouds into levels is commonly done for the purposes of cloud atlases , surface weather observations [26] and weather maps.

The standard levels and genus-types are summarised below in approximate descending order of the altitude at which each is normally based.

Stratocumuliform and stratiform clouds in the high altitude range carry the prefix cirro- , yielding the respective genus names cirrocumulus Cc and cirrostratus Cs.

When limited-resolution satellite images of high clouds are analysed without supporting data from direct human observations, it becomes impossible to distinguish between individual forms or genus types, which are then collectively identified as high-type or informally as cirrus-type even though not all high clouds are of the cirrus form or genus.

Non-vertical clouds in the middle level are prefixed by alto- , yielding the genus names altocumulus Ac for stratocumuliform types and altostratus As for stratiform types.

Without the support of human observations, these clouds are usually collectively identified as middle-type on satellite images.

Clouds that form in the low level of the troposphere are generally of larger structure than those that form in the middle and high levels, so they can usually be identified by their forms and genus types using satellite photography alone.

Nimbostratus and some cumulus in this group usually achieve moderate or deep vertical extent, but without towering structure.

However, with sufficient airmass instability, upward-growing cumuliform clouds can grow to high towering proportions. Although genus types with vertical extent are often informally considered a single group, [58] the International Civil Aviation Organization ICAO distinguishes towering vertical clouds more formally as a separate group or sub-group.

It is specified that these very large cumuliform and cumulonimbiform types must be identified by their standard names or abbreviations in all aviation observations METARS and forecasts TAFS to warn pilots of possible severe weather and turbulence.

This is a diffuse dark-grey non-convective stratiform layer with great horizontal extent and moderate to deep vertical development.

It lacks towering structure and looks feebly illuminated from the inside. It commonly achieves deep vertical development when it simultaneously grows upward into the high level due to large scale frontal or cyclonic lift.

These clouds are sometimes classified separately from the other vertical or multi-level types because of their ability to produce severe turbulence.

Genus types are commonly divided into subtypes called species that indicate specific structural details which can vary according to the stability and windshear characteristics of the atmosphere at any given time and location.

Despite this hierarchy, a particular species may be a subtype of more than one genus, especially if the genera are of the same physical form and are differentiated from each other mainly by altitude or level.

There are a few species, each of which can be associated with genera of more than one physical form. The forms, genera, and species are listed in approximate ascending order of instability or convective activity.

Genus and species types are further subdivided into varieties whose names can appear after the species name to provide a fuller description of a cloud.

Some cloud varieties are not restricted to a specific altitude level or form, and can therefore be common to more than one genus or species.

Of the stratiform group, high-level cirrostratus comprises two species. Cirrostratus nebulosus has a rather diffuse appearance lacking in structural detail.

Low stratus is of the species nebulosus [74] except when broken up into ragged sheets of stratus fractus see below. Cirriform clouds have three non-convective species that can form in mostly stable airmass conditions.

Cirrus fibratus comprise filaments that may be straight, wavy, or occasionally twisted by non-convective wind shear.

Cirrus spissatus appear as opaque patches that can show light grey shading. Stratocumuliform genus-types cirrocumulus, altocumulus, and stratocumulus that appear in mostly stable air have two species each.

The stratiformis species normally occur in extensive sheets or in smaller patches where there is only minimal convective activity.

They are most commonly seen as orographic mountain- wave clouds , but can occur anywhere in the troposphere where there is strong wind shear combined with sufficient airmass stability to maintain a generally flat cloud structure.

These two species can be found in the high, middle, or low level of the troposphere depending on the stratocumuliform genus or genera present at any given time.

The species fractus shows variable instability because it can be a subdivision of genus-types of different physical forms that have different stability characteristics.

This subtype can be in the form of ragged but mostly stable stratiform sheets stratus fractus or small ragged cumuliform heaps with somewhat greater instability cumulus fractus.

These species are subdivisions of genus types that can occur in partly unstable air. The species castellanus appears when a mostly stable stratocumuliform or cirriform layer becomes disturbed by localized areas of airmass instability, usually in the morning or afternoon.

This results in the formation of cumuliform buildups arising from a common stratiform base. They are sometimes seen with cirrus, cirrocumulus, altocumulus, and stratocumulus.

A newly recognized species of stratocumulus or altocumulus has been given the name volutus , a roll cloud that can occur ahead of a cumulonimbus formation.

Perhaps the strangest geographically specific cloud of this type is the Morning Glory , a rolling cylindrical cloud that appears unpredictably over the Gulf of Carpentaria in Northern Australia.

Associated with a powerful "ripple" in the atmosphere, the cloud may be "surfed" in glider aircraft. More general airmass instability in the troposphere tends to produce clouds of the more freely convective cumulus genus type, whose species are mainly indicators of degrees of atmospheric instability and resultant vertical development of the clouds.

A cumulus cloud initially forms in the low level of the troposphere as a cloudlet of the species humilis that shows only slight vertical development.

If the air becomes more unstable, the cloud tends to grow vertically into the species mediocris , then congestus , the tallest cumulus species [72] which is the same type that the International Civil Aviation Organization refers to as 'towering cumulus'.

With highly unstable atmospheric conditions, large cumulus may continue to grow into cumulonimbus calvus essentially a very tall congestus cloud that produces thunder , then ultimately into the species capillatus when supercooled water droplets at the top of the cloud turn into ice crystals giving it a cirriform appearance.

All cloud varieties fall into one of two main groups. One group identifies the opacities of particular low and mid-level cloud structures and comprises the varieties translucidus thin translucent , perlucidus thick opaque with translucent or very small clear breaks , and opacus thick opaque.

These varieties are always identifiable for cloud genera and species with variable opacity. All three are associated with the stratiformis species of altocumulus and stratocumulus.

However, only two varieties are seen with altostratus and stratus nebulosus whose uniform structures prevent the formation of a perlucidus variety.

Opacity-based varieties are not applied to high clouds because they are always translucent, or in the case of cirrus spissatus, always opaque.

A second group describes the occasional arrangements of cloud structures into particular patterns that are discernible by a surface-based observer cloud fields usually being visible only from a significant altitude above the formations.

These varieties are not always present with the genera and species with which they are otherwise associated, but only appear when atmospheric conditions favor their formation.

Intortus and vertebratus varieties occur on occasion with cirrus fibratus. They are respectively filaments twisted into irregular shapes, and those that are arranged in fishbone patterns, usually by uneven wind currents that favor the formation of these varieties.

The variety radiatus is associated with cloud rows of a particular type that appear to converge at the horizon. It is sometimes seen with the fibratus and uncinus species of cirrus, the stratiformis species of altocumulus and stratocumulus, the mediocris and sometimes humilis species of cumulus, [87] [88] and with the genus altostratus.

Another variety, duplicatus closely spaced layers of the same type, one above the other , is sometimes found with cirrus of both the fibratus and uncinus species, and with altocumulus and stratocumulus of the species stratiformis and lenticularis.

The variety undulatus having a wavy undulating base can occur with any clouds of the species stratiformis or lenticularis, and with altostratus. It is only rarely observed with stratus nebulosus.

The variety lacunosus is caused by localized downdrafts that create circular holes in the form of a honeycomb or net.

It is occasionally seen with cirrocumulus and altocumulus of the species stratiformis, castellanus, and floccus, and with stratocumulus of the species stratiformis and castellanus.

It is possible for some species to show combined varieties at one time, especially if one variety is opacity-based and the other is pattern-based.

An example of this would be a layer of altocumulus stratiformis arranged in seemingly converging rows separated by small breaks. The full technical name of a cloud in this configuration would be altocumulus stratiformis radiatus perlucidus , which would identify respectively its genus, species, and two combined varieties.

Supplementary features and accessory clouds are not further subdivisions of cloud types below the species and variety level.

Rather, they are either hydrometeors or special cloud types with their own Latin names that form in association with certain cloud genera, species, and varieties.

Accessory clouds, by contrast, are generally detached from the main cloud. One group of supplementary features are not actual cloud formations, but precipitation that falls when water droplets or ice crystals that make up visible clouds have grown too heavy to remain aloft.

Virga is a feature seen with clouds producing precipitation that evaporates before reaching the ground, these being of the genera cirrocumulus, altocumulus, altostratus, nimbostratus, stratocumulus, cumulus, and cumulonimbus.

When the precipitation reaches the ground without completely evaporating, it is designated as the feature praecipitatio. Of the latter, upward-growing cumulus mediocris produces only isolated light showers, while downward growing nimbostratus is capable of heavier, more extensive precipitation.

Towering vertical clouds have the greatest ability to produce intense precipitation events, but these tend to be localized unless organized along fast-moving cold fronts.

Showers of moderate to heavy intensity can fall from cumulus congestus clouds. Cumulonimbus, the largest of all cloud genera, has the capacity to produce very heavy showers.

Low stratus clouds usually produce only light precipitation, but this always occurs as the feature praecipitatio due to the fact this cloud genus lies too close to the ground to allow for the formation of virga.

Incus is the most type-specific supplementary feature, seen only with cumulonimbus of the species capillatus.

A cumulonimbus incus cloud top is one that has spread out into a clear anvil shape as a result of rising air currents hitting the stability layer at the tropopause where the air no longer continues to get colder with increasing altitude.

The mamma feature forms on the bases of clouds as downward-facing bubble-like protuberances caused by localized downdrafts within the cloud.

It is also sometimes called mammatus , an earlier version of the term used before a standardization of Latin nomenclature brought about by the World Meterorological Organization during the 20th century.

The best-known is cumulonimbus with mammatus , but the mamma feature is also seen occasionally with cirrus, cirrocumulus, altocumulus, altostratus, and stratocumulus.

A tuba feature is a cloud column that may hang from the bottom of a cumulus or cumulonimbus. A newly formed or poorly organized column might be comparatively benign, but can quickly intensify into a funnel cloud or tornado.

An arcus feature is a roll cloud with ragged edges attached to the lower front part of cumulus congestus or cumulonimbus that forms along the leading edge of a squall line or thunderstorm outflow.

The feature fluctus can form under conditions of strong atmospheric wind shear when a stratocumulus, altocumulus, or cirrus cloud breaks into regularly spaced crests.

This variant is sometimes known informally as a Kelvin—Helmholtz wave cloud. This phenomenon has also been observed in cloud formations over other planets and even in the sun's atmosphere.

The supplementary feature cavum is a circular fall-streak hole that occasionally forms in a thin layer of supercooled altocumulus or cirrocumulus.

Fall streaks consisting of virga or wisps of cirrus are usually seen beneath the hole as ice crystals fall out to a lower altitude.

This type of hole is usually larger than typical lacunosus holes. A murus feature is a cumulonimbus wall cloud with a lowering, rotating cloud base than can lead to the development of tornadoes.

A cauda feature is a tail cloud that extends horizontally away from the murus cloud and is the result of air feeding into the storm.

Supplementary cloud formations detached from the main cloud are known as accessory clouds. A group of accessory clouds comprise formations that are associated mainly with upward-growing cumuliform and cumulonimbiform clouds of free convection.

Pileus is a cap cloud that can form over a cumulonimbus or large cumulus cloud, [97] whereas a velum feature is a thin horizontal sheet that sometimes forms like an apron around the middle or in front of the parent cloud.

It is formed by the warm, humid inflow of a super-cell thunderstorm, and can be mistaken for a tornado. Although the flumen can indicate a tornado risk, it is similar in appearance to pannus or scud clouds and does not rotate.

Clouds initially form in clear air or become clouds when fog rises above surface level. The genus of a newly formed cloud is determined mainly by air mass characteristics such as stability and moisture content.

If these characteristics change over time, the genus tends to change accordingly. When this happens, the original genus is called a mother cloud.

If the mother cloud retains much of its original form after the appearance of the new genus, it is termed a genitus cloud.

One example of this is stratocumulus cumulogenitus , a stratocumulus cloud formed by the partial spreading of a cumulus type when there is a loss of convective lift.

If the mother cloud undergoes a complete change in genus, it is considered to be a mutatus cloud. The genitus and mutatus categories have been expanded to include certain types that do not originate from pre-existing clouds.

The term flammagenitus Latin for 'fire-made' applies to cumulus congestus or cumulonimbus that are formed by large scale fires or volcanic eruptions.

Smaller low-level "pyrocumulus" or "fumulus" clouds formed by contained industrial activity are now classified as cumulus homogenitus Latin for 'man-made'.

Contrails formed from the exhaust of aircraft flying in the upper level of the troposphere can persist and spread into formations resembling any of the high cloud genus-types and are now officially designated as cirrus, cirrostratus, or cirrocumulus homogenitus.

If a homogenitus cloud of one genus changes to another genus type, it is then termed a homomutatus cloud. Stratus cataractagenitus Latin for 'cataract-made' are generated by the spray from waterfalls.

Silvagenitus Latin for 'forest-made' is a stratus cloud that forms as water vapor is added to the air above a forest canopy. Stratocumulus clouds can be organized into "fields" that take on certain specially classified shapes and characteristics.

In general, these fields are more discernible from high altitudes than from ground level. They can often be found in the following forms:. When the wind and clouds encounter high elevation land features such as a vertically prominent islands, they can form eddies around the high land masses that give the clouds a twisted appearance.

Although the local distribution of clouds can be significantly influenced by topography, the global prevalence of cloud cover in the troposphere tends to vary more by latitude.

It is most prevalent in and along low pressure zones of surface tropospheric convergence which encircle the Earth close to the equator and near the 50th parallels of latitude in the northern and southern hemispheres.

These extratropical convergence zones are occupied by the polar fronts where air masses of polar origin meet and clash with those of tropical or subtropical origin.

Divergence is the opposite of convergence. In the Earth's troposphere, it involves the horizontal outflow of air from the upper part of a rising column of air, or from the lower part of a subsiding column often associated with an area or ridge of high pressure.

The latter are sometimes referred to as the horse latitudes. The presence of a large-scale high-pressure subtropical ridge on each side of the equator reduces cloudiness at these low latitudes.

The luminance or brightness of a cloud is determined by how light is reflected, scattered, and transmitted by the cloud's particles.

Its brightness may also be affected by the presence of haze or photometeors such as halos and rainbows. Tiny particles of water are densely packed and sunlight cannot penetrate far into the cloud before it is reflected out, giving a cloud its characteristic white color, especially when viewed from the top.

As a result, the cloud base can vary from a very light to very-dark-grey depending on the cloud's thickness and how much light is being reflected or transmitted back to the observer.

High thin tropospheric clouds reflect less light because of the comparatively low concentration of constituent ice crystals or supercooled water droplets which results in a slightly off-white appearance.

However, a thick dense ice-crystal cloud appears brilliant white with pronounced grey shading because of its greater reflectivity.

As a tropospheric cloud matures, the dense water droplets may combine to produce larger droplets. If the droplets become too large and heavy to be kept aloft by the air circulation, they will fall from the cloud as rain.

By this process of accumulation, the space between droplets becomes increasingly larger, permitting light to penetrate farther into the cloud.

If the cloud is sufficiently large and the droplets within are spaced far enough apart, a percentage of the light that enters the cloud is not reflected back out but is absorbed giving the cloud a darker look.

A simple example of this is one's being able to see farther in heavy rain than in heavy fog. Striking cloud colorations can be seen at any altitude, with the color of a cloud usually being the same as the incident light.

Thin clouds may look white or appear to have acquired the color of their environment or background. When the sun is just below the horizon, low-level clouds are gray, middle clouds appear rose-colored, and high clouds are white or off-white.

Clouds at night are black or dark grey in a moonless sky, or whitish when illuminated by the moon. They may also reflect the colors of large fires, city lights, or auroras that might be present.

A cumulonimbus cloud that appears to have a greenish or bluish tint is a sign that it contains extremely high amounts of water; hail or rain which scatter light in a way that gives the cloud a blue color.

A green colorization occurs mostly late in the day when the sun is comparatively low in the sky and the incident sunlight has a reddish tinge that appears green when illuminating a very tall bluish cloud.

Supercell type storms are more likely to be characterized by this but any storm can appear this way. Coloration such as this does not directly indicate that it is a severe thunderstorm, it only confirms its potential.

In addition, the stronger the updraft is, the more likely the storm is to undergo tornadogenesis and to produce large hail and high winds.

Yellowish clouds may be seen in the troposphere in the late spring through early fall months during forest fire season. The yellow color is due to the presence of pollutants in the smoke.

Yellowish clouds are caused by the presence of nitrogen dioxide and are sometimes seen in urban areas with high air pollution levels.

An occurrence of cloud iridescence with altocumulus volutus and cirrocumulus stratiformis. Sunset reflecting shades of pink onto grey stratocumulus stratiformis translucidus becoming perlucidus in the background.

Stratocumulus stratiformis perlucidus before sunset. Late-summer rainstorm in Denmark. Nearly black color of base indicates main cloud in foreground probably cumulonimbus.

Particles in the atmosphere and the sun 's angle enhance colors of stratocumulus cumulogenitus at evening twilight. Clouds exert numerous influences on Earth's troposphere and climate.

First and foremost, they are the source of precipitation, thereby greatly influencing the distribution and amount of precipitation.

Because of their differential buoyancy relative to surrounding cloud-free air, clouds can be associated with vertical motions of the air that may be convective, frontal, or cyclonic.

The motion is upward if the clouds are less dense because condensation of water vapor releases heat, warming the air and thereby decreasing its density.

This can lead to downward motion because lifting of the air results in cooling that increases its density. All of these effects are subtly dependent on the vertical temperature and moisture structure of the atmosphere and result in major redistribution of heat that affect the Earth's climate.

The complexity and diversity of clouds is a major reason for difficulty in quantifying the effects of clouds on climate and climate change. On the one hand, white cloud tops promote cooling of Earth's surface by reflecting shortwave radiation visible and near infrared from the sun, diminishing the amount of solar radiation that is absorbed at the surface, enhancing the Earth's albedo.

Most of the sunlight that reaches the ground is absorbed, warming the surface, which emits radiation upward at longer, infrared, wavelengths.

At these wavelengths, however, water in the clouds acts as an efficient absorber. The water reacts by radiating, also in the infrared, both upward and downward, and the downward longwave radiation results in increased warming at the surface.

This is analogous to the greenhouse effect of greenhouse gases and water vapor. High-level genus-types particularly show this duality with both short-wave albedo cooling and long-wave greenhouse warming effects.

On the whole, ice-crystal clouds in the upper troposphere cirrus tend to favor net warming. As difficult as it is to evaluate the influences of current clouds on current climate, it is even more problematic to predict changes in cloud patterns and properties in a future, warmer climate, and the resultant cloud influences on future climate.

In a warmer climate more water would enter the atmosphere by evaporation at the surface; as clouds are formed from water vapor, cloudiness would be expected to increase.

But in a warmer climate, higher temperatures would tend to evaporate clouds. Both of these statements are considered accurate, and both phenomena, known as cloud feedbacks, are found in climate model calculations.

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