Genus Cirrostratus
Abbreviation: Cs
Clouds of the genus cirrostratus consist of mostly continuous, wide sheets of cloud that covers a large area of the sky. It is formed when convectively stable moist air cools to saturation at high altitude, forming ice crystals. Frontal cirrostratus is a precursor to rain or snow if it thickens into mid-level altostratus and eventually nimbostratus as the weather front moves closer to the observer.
WMO species:
- Cirrostratus fibratus
Cirrostratus sheet with a fibrous appearance, but not as detached as cirrus. - Cirrostratus nebulosus
Featureless, uniform sheet.
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- WMO varieties; opacity-based:
- None (always translucent)
- WMO varieties; opacity-based:
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- WMO varieties; fibratus pattern-based:
- Cirrostratus duplicatus
Separate or semi-merged sheets with one layer slightly above the other. - Cirrostratus undulatus
Undulating waves.
- Cirrostratus duplicatus
- WMO varieties; fibratus pattern-based:
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- Varieties are not commonly associated with Cs species nebulosus.
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- WMO supplementary features:
- No supplementary features.
- WMO supplementary features:
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Read more about this topic: Cloud Types, Tropospheric Class: Families, Genera, Species, Varieties, and Supplementary Features, High Cirriform, Stratocumuliform, and Stratiform
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