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Τι (ποιος) είναι outflow$56146$ - ορισμός
![The outflow boundary indicated by the presence of this shelf cloud preceded a [[derecho]] in [[Minnesota]]](https://commons.wikimedia.org/wiki/Special:FilePath/DangerousShelfCloud.jpg?width=200 "The outflow boundary indicated by the presence of this shelf cloud preceded a [[derecho]] in [[Minnesota]]")
![Structure of a tropical cyclone. The upper level outflow is depicted by [[cirrus cloud]]s in the upper part of the schematic](https://commons.wikimedia.org/wiki/Special:FilePath/Hurricane structure graphic.jpg?width=200 "Structure of a tropical cyclone. The upper level outflow is depicted by [[cirrus cloud]]s in the upper part of the schematic")
![Outflow boundary that preceded a strong thunderstorm in [[Oklahoma]]](https://commons.wikimedia.org/wiki/Special:FilePath/Outflow boundary clouds in Oklahoma.jpg?width=200 "Outflow boundary that preceded a strong thunderstorm in [[Oklahoma]]")
Βικιπαίδεια
Outflow, in meteorology, is air that flows outwards from a storm system. It is associated with ridging, or anticyclonic flow. In the low levels of the troposphere, outflow radiates from thunderstorms in the form of a wedge of rain-cooled air, which is visible as a thin rope-like cloud on weather satellite imagery or a fine line on weather radar imagery. For observers on the ground, a thunderstorm outflow boundary often approaches in otherwise clear skies as a low, thick cloud that brings with it a gust front.
Low-level outflow boundaries can disrupt the center of small tropical cyclones. However, outflow aloft is essential for the strengthening of a tropical cyclone. If this outflow is restricted or undercut, the tropical cyclone weakens. If two tropical cyclones are in close proximity, the upper-level outflow from the upwind system can limit the development of the other system.
