Scud (cloud)

From Wikipedia, the free encyclopedia
Jump to: navigation, search

Scud (Scattered Cumulus Under Deck)[1]

Scud clouds, a type of fractus cloud, are low, detached, irregular clouds found beneath nimbostratus or cumulonimbus clouds. These clouds are often ragged or wispy in appearance. When caught in the outflow (downdraft) beneath a thunderstorm, scud clouds will often move faster than the storm clouds themselves. When in an inflow (updraft) area, scud clouds tend to rise and may exhibit lateral movement ranging from very little to substantial.

Scud clouds are formed as the warmer (and often more moist) updraft of a thunderstorm lifts the relatively warm air near the surface. These clouds condense as the warm, moist air saturates through ascent and is pushed outward from the storm. Scud clouds are very commonly found on the leading edge of a storm front. In this area of a storm, scud are commonly associated with shelf clouds.

Scud clouds may also form when an updraft ingests precipitation-cooled air from the downdraft. Scud forming in this region of the storm, if moving laterally, will tend to move inward towards the dominant updraft. Rising scud may condense and organize into a wall cloud.

Scud clouds can often be mistaken for a developing tornado, landspout, or waterspout. The difference is determinable by identifying if there's any rotation (not just movement) of the scud clouds. If any rotation occurs, a tornado, landspout, or waterspout has a high chance of forming.

Forecast[edit]

Viewing scud clouds means that there is a cumulonimbus parent cloud. Rain, hail, strong wind, and lightning can be expected from the parent cloud.

References[edit]

  1. ^ Storm Talk by Tim Marshall, 1995

See also[edit]