Kadarsah

Meteorologi dan Sains Atmosfer

List of cloud types

Posted by kadarsah pada Juli 19, 2007

From Wikipedia, the free encyclopedia


 

Clouds (from above)

 

Clouds (from above)

Simply put, clouds form when the dewpoint of water is reached in the presence of condensation nuclei in the troposphere. Atmosphere is a dynamic system, and the local conditions of turbulence, uplift and other parameters give rise to many types of clouds. Various types of clouds occur frequently enough to have acquired a name of their own, often these are further specified with additional descriptive name. Furthermore, some atmospheric processes can make the clouds organize in distinct patterns such as ‘wave cloud‘ or ‘actinoform cloud‘, these are large scale structures and not always readily identifiable from single point of view.

Cont

High-level clouds

Cirrus

 

Cirrus fibratus

 

Cirrus fibratus

 

Cirrus uncinus or Cirrus floccus

 

Cirrus uncinus or Cirrus floccus

 

Cirrus vertebratus

 

Cirrus vertebratus

Cirrus clouds form above 23,000 feet (about 6,000 m), in the cold region of the troposphere. They are denoted by the prefix cirro- or cirrus. At this altitude water almost always freezes so clouds are composed of ice crystals. The clouds tend to be wispy, and are often transparent. Isolated cirrus clouds often indicate a stable situation and do not bring precipitation, however, large amounts of cirrus clouds can indicate an approaching storm system.

There are several variations of cirrus cloud:

A series of dense lumps, or “towers” of cirrus, connected by a thinner base.
Sheets of cirrus at different layers of the atmosphere, which may be connected at one or more points.
Cirrus clouds having the traditional “mare’s tail” appearance. These clouds are long, fibrous, and curved, with no tufts or curls at the ends.
Cirrus with elements which take on a rounded appearance on the top, with the lower part appearing ragged.
Cirrus clouds whose filaments are irregularly curved or tangled.
A slender, horizontal, cirriform spiral, indicative of severe turbulence at that layer of the atmosphere.
Large area of cirrus displaying horizontal banding.
Cirrus thick enough to appear greyish when looking in the direction of the sun.
Akin to cirrus fibratus, only more curled at the ends
Cirrus in curved horizontal strips; cirrus with a “rib cage” appearance.
Cirrus with bubble-like protrusions on the underside.

Cirrocumulus

 

A clump of cirrocumulus clouds.

 

A clump of cirrocumulus clouds.

Abbreviation: Cc

Cirrocumulus clouds occur at 23,000-40,000 feet (about 6,000-12,000 m) above the earth’s surface. They form from cirrus or cirrostratus clouds which are warmed gently from below. The heating process creates convective currents, or pockets of air which rise and sink inside the cloud. If there is no sign of cirrus or cirrostratus clouds nearby, then the cloud is most likely an altocumulus.

Cirrocumulus which feature vertical “clumps”.
Cirrocumulus with elements which take on a rounded appearance on the top, with the lower part appearing ragged.
Thin clouds with large round gaps between them forming mesh structure.
Seed-shaped or lens-shaped cirrocumulus clouds.
Ripple-looking cirrocumulus clouds.
Cirrocumulus with bubble-like protrusions on the underside.

Cirrostratus

Abbreviation: Cs

Cirrostratus clouds are often translucent and do not bring precipitation.

Contrail

Aircraft engines emit water vapour into the atmosphere, and this vapour is then frozen into ice crystals. These are known as condensation trails (contrails).

Medium-level clouds

Altostratus

Abbreviation: As

Altostratus clouds form when a large lifted air mass is condensed, usually from a frontal system, and can bring rain or snow.

Altocumulus

 

Altocumulus mackerel sky

 

Altocumulus mackerel sky

Abbreviation: Ac

Altocumulus clouds are not usually associated with a front but can still bring rain or snow.

Nimbostratus

 

Nimbostratus clouds

 

Nimbostratus clouds

Abbreviation: Ns

Nimbostratus clouds tend to bring constant precipitation and low visibility.

Low-level clouds

Stratocumulus

Abbreviation: Sc

Stratocumulus clouds are lumpy, layered clouds often following a cold front, and they can produce rain or drizzle.

Layer of stratocumulus clouds with tower-like formation protruding upwards.
Stratocumulus with bubble-like protrusions on the underside.
Stratocumulus clouds covering entire sky without break.
Stratocumulus clouds covering entire sky, but having a few small breaks.
Stratocumulus clouds which precipitation reaches ground.
Stratocumulus clouds arranged in parallel waves
Separate masses of stratocumulus clouds with large breaks inbetween.

Stratus

Abbreviation: St

Stratus clouds are layerlike clouds associated with widespread precipitation or ocean air, and often produce drizzle.

Ragged shreds of stratus clouds.
Dark ragged clouds under base of precipitation clouds.
Uniform fog-like low clouds.

Cumulus

Abbreviation: Cu

Cumulus clouds are sometimes called fair weather clouds but can develop into more storm-condition clouds (cumulonimbus, for example), and continued upward growth suggests showers later in the day.

Low, horizontal cloud formation associated with the leading edge of thunderstorm outflow.
Tall and large cumulus clouds
Ragged shreds of cumulus clouds.
“Fair weather clouds” that are wider than taller
Cumulus clouds slightly taller than cumulus humilis
Cumulus clouds with tall tower-like formations protruding upwards.
Cumulus clouds which precipitation reaches ground
Cumulus clouds arranged in parallel lines
Clouds formed by air rising at windward slopes of hills and mountains.
Mass of fractus clouds below cumulus cloud.
Small cap-like cloud over parent cumulonimbus cloud
Column hanging from the bottom of cumulus

Vertically developed clouds

Cumulonimbus

 

Cumulonimbus with NOAA research vessel in foreground

 

Cumulonimbus with NOAA research vessel in foreground

Abbreviation: Cb

Cumulonimbus is the cloud of storms and rain or showers.

Cumulonimbus cloud with cirriform top.
Cumulonimbus with puffy rounded top.
Cumulonimbus with flat anvil-like top
Small cap-like cloud over parent cumulonimbus cloud
Cumulonimbus with bubble-like protrusions on the underside.
Low, horizontal cloud formation associated with the leading edge of thunderstorm outflow.
Cumulonimbus clouds which precipitation reaches ground
Column hanging from the bottom of cumulonimbus cloud
Mass of fractus clouds below cumulonimbus cloud.

Other clouds

A thin cloud seen most often between sunset and sunrise and is between 12 to 18 miles (19 to 29 km) high

A thin cloud seen most often between sunset and sunrise and is 32 to 35 miles (51 to 56 km) high

The meaning of cloud names

Main cloud components

  • Altum – height
  • Cirrus – lock of hair
  • Cumulus – heaped
  • Nimbus – precipitation bearing
  • Stratus – layer

Main cloud types

Main sub-cloud types

  • Castellanus – castle-like with a series of turret shapes – indicates lateral decrease and vertical increase in movement.
  • Congestus – moderate development and heaped into cauliflower shapes – indicates moist ground and upcurrent.
  • Fibratus – thin filament type clouds, can be straight or slightly curved -
  • Floccus – looking like a tuft of wool, small congestus – indicates dry air
  • Fractus – irregular shredded appearance – indicates usually gusts
  • Humilis – small, low, flattened cumulus – indicates relatively dry dry ground
  • Lenticularis – having a lens-like appearance – formed by standing waves of wind passing mountains or hills
  • Mediocris – medium size cumulus with small bulges at the top – indicates moderate updrafts
  • Nebulosus – indistinct cloud without features – indicates stable wind (if any) and static air layers
  • Spissatus – thick cirrus with a grey appearance – indicates upper troposphere vertical movement
  • Stratiformis – horizontal cloud sheet – rains
  • Uncinus – cirrus with a hook shape at the top – indicates a nearby front
  • Uniformis – no notable difference in shapes of clouds (used with cumulus) – indicates stable wind (if any) and static air layers

Other cloud types

 

A translucent wave cloud

 

A translucent wave cloud

  • Arcus – arch or a bow – mostly attached to cumulus, thick with ragged edges
  • Duplicatus – double – partly merged layers of cloud
  • Incus – anvil – top part of Cb cloud, anvil shaped
  • Intortus – twisted – curved and tangled cirrus
  • Mammatus – breast cloud – round pouches on surface of cloud
  • Lacunosus – full of holes – thin cloud distinguished by holes and ragged edges
  • Opacus – thick and shadowy – an opaque sheet of cloud
  • Pannus – shredded cloth – shredded sections attached to main cloud
  • Perlucidus – translucent – sheet of cloud with small spaces among itself
  • Pileus – capped – hood shaped cumulus type cloud
  • Praecipitatio – falling – cloud whose precipitation reaches the ground
  • Radiatus – radiant – parallel lines converging at a central point, often cirrus
  • Tuba – like a trumpet – column hanging from the bottom of cumulus
  • Translucidus – transparent – translucent patch or sheet
  • Undulatus – wavy – cloud displaying an undulating pattern
  • Velum – a ship’s sail – sail-like in appearance
  • Vertebratus – skeletal and bone like – cirrus arranged to look like bones or skeleton

Storm Clouds

Clouds associated with the development and duration of storms:

  • Accessory cloud – cloud that is attached to and develops on body of main cloud
  • Anvil – the top flatter part of a cumulonimbus cloud
  • Anvil dome – the overshooting top on a Cb that is often present on a supercell
  • Anvil rollover – (slang) circular protrusion attached to underside of anvil
  • Arcus cloud – arch or a bow shape, attached to cumulus, thick with ragged edges
  • Backsheared anvil – (slang) anvil that spreads upwind, indicative of extreme weather
  • Clear slot (or dry slot) – an evaporation of clouds as a rear flank downdraft descends and dries out cloud and occludes around a mesocyclone
  • Cloud tags – ragged detached portions of cloud
  • Collar cloud – rare ring shape surrounding upper part of wall cloud
  • Condensation funnel – the cloud of a funnel cloud aloft or a tornado
  • Cumulus – heaped clouds
  • Cumulus congestus – moderate development and heaped into cauliflower shapes
  • Cumulus fractus – ragged detached portions of cumulus cloud
  • Cumulus humilis – small, low, flattened cumulus, early development
  • Cumulus mediocris – medium-sized cumulus with small bulges at the top
  • Cumulus pannus – shredded sections attached to main cumulus cloud
  • Cumulus pileus – capped – hood shaped cumulus cloud
  • Cumulus praecipitatio – cumulus whose precipitation reaches the ground
  • Cumulus radiatus – cumulus arranged in parallel lines
  • Cumulus tuba – column hanging from the bottom of cumulus
  • Cumulus velum – cumulus displaying an undulating pattern
  • Cumulonimbus – heaped towering rain-bearing clouds that stretch to the upper levels
  • Cumulonimbus calvus – cumulonimbus whose upper parts have lost their shape
  • Cumulonimbus capillatus – Cb whose upper parts have taken on a cirrus-like form
  • Cumulonimbus incus – Cb with anvil aloft
  • Cumulonimbus mammutus – pouch-like protrusions that hang from under an anvil
  • Cumulonimbus pannus – shredded sections attached to main Cb cloud
  • Cumulonimbus pileus – capped – hood shaped cumulonimbus cloud
  • Cumulonimbus praecipitatio – Cb whose precipitation reaches the ground
  • Cumulonimbus spissatus – cumulonimbus with a thick grey appearance
  • Cumulonimbus tuba – column hanging from the bottom of cumulonimbus
  • Cumulonimbus velum – cumulonimbus displaying an undulating pattern
  • Debris cloud – rotating ‘cloud’ of debris found at base of tornado
  • Hail fog – a shallow surface layer of fog that sometimes forms in vicinity of deep hail accumulation, can be very dense
  • Inflow band – a laminar band marking inflow to a Cb, can occur at lower or mid levels of tower
  • Inverted cumulus – cumulus which has transferred momentum from an exceptionally intense Cb tower and is convectively growing on the underside of an anvil
  • Fractonimbus – dark ragged clouds under base of precipitation cloud.
  • Funnel cloud – rotating funnel of cloud hanging from under Cb, not making contact with ground
  • Knuckles – lumpy protrusion that hangs from edge or underside of anvil
  • Roll cloud – elongated, low-level, tube shaped, horizontal cloud
  • Rope cloud – (slang) narrow, sometimes twisted funnel type cloud seen after tornado dissipates
  • Scud cloud – ragged detached portions of cloud
  • Shelf cloud – wedge shaped cloud often attached to the underside of Cb
  • Stratus fractus – ragged detached portions of stratus cloud
  • Striations – a groove or band of clouds encircling an updraft tower, indicative of rotation
  • Tail cloud – an area of condensation consisting of laminar band and cloud tags extending from a wall cloud towards a precipitation core
  • Towering cumulus (TCu) – a large cumulus cloud with great vertical development, usually with a cauliflower-like appearance, but lacking the characteristic anvil of a Cb
  • Wall cloud – distinctive fairly large lowering of the rain free base of a Cb, often rotating

See also

 


Weather Portal

External links

  1. Cloud Classification (National Weather Service)
  2. Skywatcher Chart (National Weather Service)
  3. S’COOL Cloud Types Tutorial
  4. Cloud Appreciation Society
  5. Texas A&M Cloud Glossary
  6. Very good cloud-identification site
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