, Supplementary cloud formations detached from the main cloud are known as accessory clouds.  The stratocumuliform group is divided into cirrocumulus (high-level), altocumulus (mid-level), and stratocumulus (low-level).
When limited-resolution satellite images of high clouds are analysed without supporting data from direct human observations, distinguishing between individual forms or genus types becomes impossible, and they are then collectively identified as high-type (or informally as cirrus-type, though not all high clouds are of the cirrus form or genus). Differing amounts of these feedbacks are the principal reason for differences in climate sensitivities of current global climate models. Clouds at night are black or dark grey in a moonless sky, or whitish when illuminated by the moon. Cirriform clouds in the troposphere are of the genus cirrus and have the appearance of detached or semimerged filaments. , Yellowish clouds may be seen in the troposphere in the late spring through early fall months during forest fire season. However, if the air becomes sufficiently moist and unstable, orographic showers or thunderstorms may appear. An example of this would be a layer of altocumulus stratiformis arranged in seemingly converging rows separated by small breaks.
These are sometimes known as type 2.
, Noctilucent clouds have four major types based on physical structure and appearance. 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. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical.
First and foremost, they are the source of precipitation, thereby greatly influencing the distribution and amount of precipitation. Howard was a methodical observer with a strong grounding in the Latin language, and used his background to classify the various tropospheric cloud types during 1802.
There are two methods of naming clouds in their respective layers of the homosphere, Latin and common.  These clouds are the product of very strong convection that can penetrate the lower stratosphere. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes.  Cloud droplets tend to scatter light efficiently, so that the intensity of the solar radiation decreases with depth into the gases. , Polar stratospheric clouds (PSC's) form in the lowest part of the stratosphere during the winter, at the altitude and during the season that produces the coldest temperatures and therefore the best chances of triggering condensation caused by adiabatic cooling. The presence of a large-scale high-pressure subtropical ridge on each side of the equator reduces cloudiness at these low latitudes. Terrestrial clouds can be found throughout most of the homosphere, which includes the troposphere, stratosphere, and mesosphere. This results in the formation of embedded cumuliform buildups arising from a common stratiform base. The altitude, form, and thickness of the clouds are the main factors that affect the local heating or cooling of Earth and the atmosphere.
By this process of accumulation, the space between droplets becomes increasingly larger, permitting light to penetrate farther into the cloud.
, A tuba feature is a cloud column that may hang from the bottom of a cumulus or cumulonimbus. Reasonator; PetScan; Scholia; Statistics; Search depicted; Media in category "Morning glory cloud" The following 5 files are in this category, out of 5 total. Opacity-based varieties are not applied to high clouds because they are always translucent, or in the case of cirrus spissatus, always opaque.  In the play, the Clouds change shape to reveal the true nature of whoever is looking at them, turning into centaurs at the sight of a long-haired politician, wolves at the sight of the embezzler Simon, deer at the sight of the coward Cleonymus, and mortal women at the sight of the effeminate informer Cleisthenes. , The luminance or brightness of a cloud is determined by how light is reflected, scattered, and transmitted by the cloud's particles. Coloration such as this does not directly indicate that it is a severe thunderstorm, it only confirms its potential.
, 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.
His system of nomenclature included 12 categories of clouds, with such names as (translated from French) hazy clouds, dappled clouds, and broom-like clouds.
 Meteorologists affiliated with the World Meteorological Organization (WMO) officially classify nimbostratus as mid-level for synoptic purposes while informally characterizing it as multi-level. , Low clouds are found from near the surface up to 2,000 m (6,500 ft).
In general, small cumuliform clouds tend to indicate comparatively weak instability. The best-known is cumulonimbus with mammatus, but the mamma feature is also seen occasionally with cirrus, cirrocumulus, altocumulus, altostratus, and stratocumulus. No embedded cumuliform types have been identified, but broken stratocumuliform wave formations are sometimes seen in the top layer that reveal more continuous layer clouds underneath. Morning Glory, caminos de nubes.jpg 1,184 × 665; 36 KB. —Preceding unsigned comment added by Quaestor23 (talk • contribs) 11:38, 15 December 2009 (UTC), anyone know anything about local Aboriginal stories associated with these clouds? Meteorologica was based on intuition and simple observation, but not on what is now considered the scientific method. 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.  Mid-level altostratus and multi-level nimbostratus always have a flat or diffuse appearance and are therefore not subdivided into species. If these characteristics change over time, the genus tends to change accordingly. 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. Low This article has been rated as Low-importance on the project's importance scale.  In the troposphere, dense, deep clouds exhibit a high reflectance (70% to 95%) throughout the visible spectrum.
, Cloud cover has been seen on most other planets in the Solar System. 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. Русский 1 663 000+ статей. , Some planets outside the Solar System are known to have atmospheric clouds.
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