Altostratus are large mid-level sheets of thin cloud.
They are often spread over a very large area and are usually featureless. Altocumulus is a member of the ten fundamental cloud types (or cloud genera). Along with nimbostratus clouds, these clouds don’t have any species associated with them. Altostratus clouds spread across a huge area in the sky―about hundreds of square kilometers. This middle cloud genus is composed of water droplets, and sometimes ice crystals, In the mid-latitudes, cloud bases are generally found between 15,000 and 20,000 feet. It is a middle-level cloud, thus they usually form between 2 to 7 kilometers (6,500 to 22,000 ft). Sometimes a fibrous and banded aspect may appear, but the intervals between the bands are filled with thinner cloud veil. The sun or moon may shine through an altostratus cloud, but will appear watery or fuzzy.

A mid-altitude cloud that extends in flat, smooth sheets or layers of varying thickness. Description & Characteristics. Altostratus clouds are found in the middle cloud level.

Altostratus clouds can form ice layers on an aircraft’s wings. Altostratus opacus: As op: Sun or moon is completely covered by the clouds. Cirrostratus are darker than cirrus and are always thin enough for the high Sun to cast shadows. Just like stratus clouds they are flat and hazy, but they are not as high as cirrostratus clouds and not as low as stratus clouds. 7. With regards to color, altostratus clouds are darker compared to cirrostratus but lighter than nimbostratus. A light rainy weather can be associated with the formation of altostratus clouds. Altostratus clouds are characterized by their uniform gray cloud layer ranging from thin clouds that let you see the sun, to thick layers of clouds that completely block the sun. Word clouds They become visible during twilight when sunlight from below the horizon illuminates them to reveal their faint ghostly outlines. In the upper troposphere, the terms cirrostratus and cirrus are used. Another type of cloud is called an altostratus cloud. They’re found in the middle layer of the troposphere, lower than cirrocumulus and higher than their cumulus and stratocumulus counterparts. The cirrus cloud type refers to thin, often wispy, cirrostratus clouds. Altostratus clouds generally form between 2,000 and 6,100 m (6,560 and 20,000 ft) and often produce long, steady rain showers. Another type of cloud is called an altocumulus cloud, which looks puffy just like the other cumulus clouds, but it is larger and darker than the cirrocumulus clouds. They look like the wool of sheep or scales of mackerel fish—hence their nicknames "sheep backs" and "mackerel skies." Stratiform clouds that both extend through a large fraction of the troposphere and precipitate are called nimbostratus. The title of highest cloud goes to the rare but beautiful but noctilucent cloud.
Altocumulus cloud usually occur as a layer or patch of more or less separate cloudlets in the form of heaps, rolls, billows or pancakes. Usually composed of a mixture of water droplets and ice crystals, they are thin enough in parts to allow you to see the sun weakly through the cloud. altostratus clouds are flat and hazy and in the middle of the sky, and cirrocumulus clouds are up like small spread out cotton balls. Altocumulus clouds are typically found in groups or heaps clumped together. What are altostratus clouds? See illustration at cloud. An altostratus cloud usually covers the whole sky and has a gray or blue-gray appearance. altostratus From the Latin altum, ‘height’ and stratus, ‘spread out’, the name of a genus of clouds that consists of greyish sheets or layers; the cloud may be striated, fibrous, or uniform. Altocumulus (From Latin Altus, "high", cumulus, "heaped") is a middle-altitude cloud genus that belongs mainly to the stratocumuliform physical category characterized by globular masses or rolls in layers or patches, the individual elements being larger and darker than those of cirrocumulus and smaller than those of stratocumulus. Altocumulus clouds are the most common clouds in the middle atmosphere. They are white and/or gray in colour with generally shadowed parts or undersites and often show a waved … See also cloud classification.

Altostratus are large mid-level sheets of thin cloud. The highest cloud of all. Altostratus. And unlike their altocumulus counterpart, they’re often boring to look at. They hover at around 60,000 m (200,000 feet) and are too faint to be seen in daylight. nimbostratus clouds are big, hazy and dark and are a sign of rain, and cirrostratus clouds are very high up in the sky and flat and hazy. An altostratus cloud usually forms ahead of storms with continuous rain or snow.


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