Fractus cloud

Fractus clouds, also called fractostratus or fractocumulus,[1] are small, ragged cloud fragments that are usually found under an ambient cloud base. They form or have broken off from a larger cloud, and are generally sheared by strong winds, giving them a jagged, shredded appearance. Fractus have irregular patterns, appearing much like torn pieces of cotton candy. They change constantly, often forming and dissipating rapidly. They do not have clearly defined bases. Sometimes they are persistent and form very near the surface. Common kinds include scud and cloud tags.[2]

Fractus cloud
Fractus clouds over the Považský Inovec mountains
AbbreviationCu fr., St fr., Frnb
GenusCumulus or stratus
SpeciesFractus (broken)
AltitudeBelow 1,500 m
(5,000 ft)
ClassificationFamily C (Low-level)
Appearanceirregular, ragged
PrecipitationNo, but may accompany precipitation clouds
Cumulus fractus

Forms
A nimbostratus cloud in the background with a stratus fractus in the middle of the upper half of the image.

Fractus are accessory clouds, named for the type of cloud from which they were sheared. The two principal forms are cumulus fractus (formerly, fractocumulus) and stratus fractus (formerly, fractostratus). Fractus clouds may develop into cumulus if the ground heats enough to start convection. Stratus fractus is distinguishable from cumulus fractus by its smaller vertical extent, darker color, and by the greater dispersion of its particles.

Cumulus fractus clouds actually look like ragged cumulus clouds.[2] They may originate from dissipated cumulus clouds, appearing in this case as white ragged clouds located at significant distances from each other. Cumulus fractus in particular form on the leading and trailing edges of summer storms in warm and humid conditions.[3] Observing fractus gives an indication of wind movements under the parent cloud.

Masses of multiple fractus clouds, located under a main cloud, are called pannus.

Fractonimbus are a form of stratus fractus, developing under precipitation clouds due to turbulent air movement. They are dark-gray and ragged in appearance. Fractonimbus exist only under precipitation clouds (such as nimbostratus, altostratus or cumulonimbus), and don't produce precipitation themselves. Fractonimbus may eventually merge completely with overlying nimbostratus clouds.

Significance in thunderstorms
Scud clouds under a thunderstorm

In rainstorms, scud often form in the updraft area where the air has been cooled by precipitation from the downdraft, thus condensation occurs below the ambient cloud deck. If scud are rising and moving towards the main updraft, sometimes marked by a rain-free base (RFB) or wall cloud, then the thunderstorm is still developing from rising scud.

In addition to forming in inflow, fractus also form in outflow. Scud are very common on the leading edge of a thunderstorm where warm, moist air is lifted by the gust front. Scud are usually found under shelf clouds.[4]

See also

References
Wikimedia Commons has media related to Fractus cloud.
  1. "Appendix 3: History of cloud nomenclature". World Meteorological Organization.
  2. Glickman, Todd S. (June 2000). Glossary of Meteorology. Boston: American Meteorological Society.
  3. NOAA Cloud Types - NOAA Chart of Different Cloud Types.
  4. Marshall, Tim (May 1995). Storm Talk. David Hoadley (illust.). United States.{{cite book}}: CS1 maint: location missing publisher (link)
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.