Altostratus is formed by the lifting of a large mostly stable air mass that causes invisible water vapor to condense into cloud.
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This cloud type normally forms above from altostratus cloud but tends to thicken into the lower levels during the occurrence of precipitation.
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This normally occurs with altostratus opacus, which can produce widespread but usually light precipitation, and with thicker clouds that show significant vertical development.
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If unstable altocumulus castellanus accompanies or takes the place of the main altostratus layer, cumulus congestus or cumulonimbus producing showers or thunderstorms may follow.
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The effect of gravity waves in clouds can look like altostratus undulatus clouds, and are sometimes confused with them, but the formation mechanism is different.
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They also can occur under altostratus cloud preceding a warm or occluded front, when cumulus usually lose vertical development as the sun's heat decreases.
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The best-known is cumulonimbus with mammatus, but the mamma feature is also seen occasionally with cirrus, cirrocumulus, altocumulus, altostratus, and stratocumulus.
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Altostratus most often takes the form of a featureless sheet of cloud but can be wavy ( undulatus ) as a result of wind shear through the cloud.
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Yesterday I saw a roughly 25 deg from the sun rainbowlike halo, and a sundog while the sun was in a cirrus-cirrostratus-altostratus cloud.
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The variety " undulatus " ( having a wavy undulating base ) can occur with any clouds of the species stratiformis or lenticularis, and with altostratus.
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