Stratocumulus cloud
A stratocumulus cloud, occasionally called a cumulostratus, 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 in altocumulus, and the whole being at a lower height, usually below 2,000 metres (6,600 ft). Weak convective currents 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 a twain cloud for being a combination of two types of clouds.
| Stratocumulus clouds | |
|---|---|
Aerial photograph of Stratocumulus perlucidus clouds over the midwestern United States | |
| Abbreviation | Sc |
| Symbol | |
| Genus | Stratocumulus (layer heap) |
| Species |
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| Variety |
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| 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 | Uncommon Rain, Snow or Snow pellets |
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