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Although each tornado is unique, most kinds of tornadoes go through a life cycle of formation, maturation, and dissipation. [4] The process by which a tornado dissipates or decays, occasionally conjured as tornadolysis, is of particular interest for study as is tornadogenesis, longevity, and intensity.
Reliably predicting tornado intensity and longevity remains a problem, as do details affecting characteristics of a tornado during its life cycle and tornadolysis. Other rich areas of research are tornadoes associated with mesovortices within linear thunderstorm structures and within tropical cyclones. [141]
An EF4 tornado with wind speeds ranging from 166 to 200 mph can cause devastating damage. Most to all walls on a well-built house will likely collapse, and high-rise buildings can sustain ...
The tornado became the subject of several scientific papers analyzing the life cycle of and wind speed speeds in a tornado. Among the studies was the first-ever photogrammetric analysis of wind speeds in a tornado. The film of the tornado is still regarded as being of exceptionally high quality and sharpness.
Some of the most notorious twisters in U.S. history were wedge tornadoes, including the EF5 that leveled Joplin, Missouri, on May 22, 2011, and the El Reno tornado, which was a jaw-dropping 2.6 ...
A video of the tornado posted to YouTube by storm chaser Scott Peake gained over 1.7 million views, [7] and another video of the tornado during its lifetime posted by the Storm Chasing Channel went viral. [8] Storm chaser Ben Holcomb also took a video of the tornado from the beginning to end of its life. [9]
Video continued to roll as the powerful layers of the tornado approached closer to the vehicle -- debris wrapping around the twister as it made its daunting approach.
Landspout is a term created by atmospheric scientist Howard B. Bluestein in 1985 for a tornado not associated with a mesocyclone. [3] The Glossary of Meteorology defines a landspout: "Colloquial expression describing tornadoes occurring with a parent cloud in its growth stage and with its vorticity originating in the boundary layer.