downburst
Sign in to savethumb|right|A downburst seen in Phoenix, Arizona. 325px|thumb|Illustration of a microburst at an airport. The air moves in a downward motion until it hits the surface. It then spreads outward in all directions. The wind regime in a microburst is opposite to that of a tornado.
Article
16 sectionsContents
- Definition
- Dry downbursts
- Wet downbursts
- Formation
- Development stages of downbursts
- Physical processes of dry and wet downbursts
- Basic physical processes using simplified buoyancy equations
- Negative vertical motion associated only with buoyancy
- Heat bursts
- Danger to shipping
- Danger to aviation
- Danger to buildings
- See also
- References
- Bibliography
- External links
thumb|right|A downburst seen in Phoenix, Arizona. 325px|thumb|Illustration of a microburst at an airport. The air moves in a downward motion until it hits the surface. It then spreads outward in all directions. The wind regime in a microburst is opposite to that of a tornado.
In meteorology, a downburst is a strong downward and outward gushing wind system that emanates from a point source above and blows radially, that is, in straight lines in all directions from the area of impact at surface level. It originates under deep, moist convective conditions like cumulus congestus or cumulonimbus. Capable of producing damaging winds, it may sometimes be confused with a tornado, where high-velocity winds circle a central area, and air moves inward and upward. These usually last for seconds to minutes. Downbursts are particularly strong downdrafts within thunderstorms (or deep, moist convection as sometimes downbursts emanate from cumulonimbus or even cumulus congestus clouds that are not producing lightning). Downbursts are most often created by an area of significantly precipitation-cooled air that, after reaching the surface (subsiding), spreads out in all directions producing strong winds.