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Stratocumulus occurs in patches or layers, composed of rounded masses or rolls, at one or more levels. The clouds are grey or whitish and always have dark parts. When in the form of dark rolls (top left photograph), the edges often merge to form a continuous layer. Sometimes the elements lie in parallel bands (top right). Due to perspective these may appear to converge towards the horizon. Sometimes the cloud is not very dense and gaps may appear between the elements (bottom left). In the tropics stratocumulus may occur as a large, single roll cloud. It may also occur in the shape of lenses or almonds, although this is fairly rare. One particular species, called stratocumulus castellanus, has cumulus-like turrets rising from a common horizontal base (bottom right). The turrets may develop into large cumulus (when the coding becomes CL=2 [C=8]) or even cumulonimbus.
Stratus CL6 (C7) may lift to become stratocumulus CL5 (C6). Stratocumulus often forms beneath nimbostratus CM2 (C5).
| Classification | |
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| Description: Stratocumulus not resulting from the spreading out of Cumulus. |
Designation: CH=5 (C6) |
| Latin name: Stratocumulus (Sc) [plus several species and varieties]. |
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Related pages: Cloud classification | CL guide | CM guide | CH guide | Cloud index