Cirrocumulus castellanus

Type of cloud
Cirrocumulus castellanus
Cirrocumulus castellanus undulatus (on the center)
AbbreviationCc cas
Symbol
GenusCirro- (curl)
-cumulus (heaped)
SpeciesCastellanus (castle)
AltitudeAbove 6,000 m
(Above 20,000 ft)
ClassificationFamily A (High-level)
Appearancesmall, rounded turrets
PrecipitationVirga only

Cirrocumulus castellanus or Cirrocumulus castellatus[1] is a type of cirrocumulus cloud. Castellanus is from the Latin meaning "of a castle".[2] These clouds appear as round turrets that are rising from either a lowered line or sheet of clouds.[3] Cirrocumulus castellanus is an indicator of atmospheric instability at the level of the cloud.[4] The clouds form when condensation occurs in the base cloud, causing latent heating to occur. This causes air to rise from the base cloud, and if the air ascends into conditionally unstable air, cirrocumulus castellanus will form.[5]

See also

References

  1. ^ "Appendix 3 - History of cloud nomenclature".
  2. ^ Numen - The Latin Lexicon. "Definition of castellanus". Retrieved 13 July 2011.
  3. ^ Dunlop, Storm (2003). The weather identification handbook (1st Lyons Press ed.). Guilford, Conn.: Lyons Press. p. 66. ISBN 1-58574-857-9.
  4. ^ Callanan, Martin. "Cirrocumulus castellanus". International Cloud Atlas. nephology.eu. Archived from the original on 30 December 2020. Retrieved 13 July 2011.
  5. ^ Ahrens, C. Donald (2007). Keith Dodson (ed.). Meteorology Today: An Introduction to Weather, Climate, and the Environment. Belmont, CA: Cengage Learning. p. 158. ISBN 978-0-495-01162-0.

External links

  • International Cloud Atlas – Cirrocumulus castellanus Archived 2020-12-30 at the Wayback Machine
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Cirrocumulus cloud (Cc) types
Species
  • Cirrocumulus castellanus (Cc cas)
  • Cirrocumulus floccus (Cc flo)
  • Cirrocumulus lenticularis (Cc len)
  • Cirrocumulus stratiformis (Cc str)
Varieties
  • Cirrocumulus lacunosus (Cc la)
  • Cirrocumulus undulatus (Cc un)
Variants
  • Cirrocumulus mamma
  • Cirrocumulus virga
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Cloud genera and selected species, supplementary features, and other airborne hydrometeors - WMO Latin terminology except where indicated
Mesospheric
Extreme-level
80–85 km
Noctilucent (NLC)
Polar mesospheric clouds
  • Noctilucent type I veils
  • Noctilucent type II bands
  • Noctilucent type III billows
  • Noctilucent type IV whirls
Stratospheric
Very high-level
15–30 km
Nacreous polar stratospheric clouds (PSC)
  • Cirriform nacreous
  • Lenticular nacreous
Nitric acid and water
polar stratospheric clouds (PSC)
  • No differentiated sub-types; tends to resemble cirrostratus
Tropospheric
High-level
3–18 km
Cirrus (Ci)
Species
Ci-only varieties
Cirrocumulus (Cc)
Species
Cirrostratus (Cs)
Species
High-level-only
mutatus cloud
  • Mutatus non-height specific (see below)
Medium-level
2–8 km
Altocumulus (Ac)
Species
Altostratus (As)
Nimbostratus (Ns)
Multi-level
Varieties
Low-level
0–2 km
Cumulonimbus (Cb)
Towering vertical
Species
Cb-only supplementary features
Cb-only accessories and other
Cumulus (Cu)
Variable vertical extent
Species
Other
Stratus (St)
Species
St-only genitus cloud and other
Stratocumulus (Sc)
Species
Low-level-only
supplementary features
Low-level-only
accessory cloud and other
Non-height
specific
Varieties
Supplementary features
Mother clouds
and human-made clouds
  • (Mother cloud)+genitus (e.g. cumulogenitus (cugen)
  • (Mother cloud)+mutatus (e.g. cumulomutatus (cumut)
  • Homogenitus (hogen)
  • Homomutatus (homut)


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