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An early version of the Tornado Intercept Vehicle (TIV 1). The SRV "Dominator", featured in the Discovery Channel series, Storm Chasers.. Storm Chasers was filmed each year in the central United States (an area known as Tornado Alley due to the frequency and severity of tornadoes occurring there) primarily during late spring and early summer, the time of the most frequent tornado activity ...
Video shows haboobs, or powerful dust storm, 'brown-out' portions of Texas, New Mexico ... Thunderstorms, strong winds disrupt Mardi Gras in New Orleans as severe weather affects millions.
A back-building thunderstorm, commonly referred to as a training thunderstorm, is a thunderstorm in which new development takes place on the upwind side (usually the west or southwest side in the Northern Hemisphere), such that the storm seems to remain stationary or propagate in a backward direction. Though the storm often appears stationary ...
Hurricane-force winds, caused by individual thunderstorms, thunderstorm complexes, derechos, tornadoes, extratropical cyclones, or tropical cyclones can destroy mobile homes and structurally damage buildings with foundations. Winds of this strength due to downslope winds off terrain have been known to shatter windows and sandblast paint from cars.
Supercell thunderstorms occur more frequently in tornado alley and Dixie Alley than anywhere else in the world. Tornado watches and warnings are frequently necessary in the spring and summer. Most places from the Great Plains to the East Coast of the United States and north as far as the Canadian Prairies , the Great Lakes region , and the St ...
An unexpected and yet increasingly more common result of storm chasers is the data they provide to storm research from their videos, social video posts and documentation of storms they encounter. After the El Reno tornado in 2013, portals were created for chasers to submit their information to help in the research of the deadly storm. [ 70 ]
Rainbands in advance of warm occluded fronts and warm fronts are associated with weak upward motion, [1] and tend to be wide and stratiform in nature. [2] In an atmosphere with rich low level moisture and vertical wind shear, [3] narrow, convective rainbands known as squall lines form generally in the cyclone's warm sector, ahead of strong cold fronts associated with extratropical cyclones. [4]
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