Anticyclonic storm

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by ClueBot NG (talk | contribs) at 16:22, 1 February 2016 (Reverting possible vandalism by 155.43.47.247 to version by Blaylockjam10. Report False Positive? Thanks, ClueBot NG. (2527826) (Bot)). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

An anticyclonic storm is a weather storm where winds around the storm flow contrary to the direction dictated by the Coriolis effect about a region of low pressure. In the Northern Hemisphere, anticyclonic storms involve clockwise wind flow; in the Southern Hemisphere, they involve counterclockwise wind flow.

Anticyclonic storms usually form around high-pressure systems. These do not "contradict" the Coriolis effect; it predicts such anticyclonic flow about high-pressure regions. Anticyclonic storms, as high-pressure systems, usually accompany cold weather and are frequently a factor in large snowstorms. Jupiter's Great Red Spot is a well-known extraterrestrial example of an anticyclonic system.

Anticyclonic tornadoes often occur;[1] while tornadoes' vortices are low-pressure regions, this occurs because tornadoes occur on a small enough scale such that the Coriolis effect is negligible.

References

  1. ^ Williams, Jack. The Weather Book. New York: Vintage Books, 1992. Pages 118,122.

External links