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The high-end EF3 tornado had a recorded width of 2.2 miles (3.5 km). [14] 2021 South Moravia tornado: F4/IF4 2.2 miles (3.5 km) ESSL, CHMI, CUNI, Meteopress, SHMU, CU, Geosphere, Austrocontrol, BUT: This tornado reached a maximum width of 2.2 miles (3.5 km), setting the record as the widest tornado to ever occur in the Czech Republic and in Europe.
However, tornadoes are capable of both much shorter and much longer damage paths: one tornado was reported to have a damage path only 7 feet (2.1 m) long, while the record-holding tornado for path length—the Tri-State Tornado, which affected parts of Missouri, Illinois, and Indiana on March 18, 1925—was on the ground continuously for 219 ...
Tornadoes of 1912. Tornado outbreak of April 20–22, 1912; Tornado outbreak of April 27–29, 1912; Tornadoes of 1913. 1913 Easter tornado outbreak; Tornadoes of 1916. Tornado outbreak of June 5–6, 1916; Tornadoes of 1917. March 1917 tornado outbreak; Tornado outbreak sequence of May 25 – June 1, 1917; Tornadoes of 1918. 1918 Tyler tornado ...
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 tornado is seen West of Dodge City, Kansas moving North on May 24, 2016 in Dodge City, Kansas.
Houses and stone-walled buildings collapsed. The tornado's maximum width was 850 metres (930 yd) and had a path length of 36 kilometres (22 mi). [8] ESSL: July 17: 1902 Canada: Ontario: Chesterville, Winchester: Several The tornado was 50–60 rods (250–300 m; 820–990 ft) wide and tore dwellings and outbuildings into pieces. [13] [14] [15 ...
Significant tornado – A substantial tornado, one that is rated F2-F5 or EF2-EF5. Grazulis also includes (E)F0-(E)F1 tornadoes that cause a fatality in his definition for The Tornado Project database. Significant tornado parameter (STP) – Model parameter calculated using Shear values, Instability values, and vorticity values.
A tornado is a violently rotating column of air in contact with the surface and a cumuliform cloud base. Tornado formation is caused by the stretching and aggregating/merging of environmental and/or storm-induced vorticity that tightens into an intense vortex. There are various ways this may come about and thus various forms and sub-forms of ...