Amultiple-vortex tornado is atornado that contains several vortices (called subvortices or suction vortices) revolving around,inside of, and as part of the mainvortex. The only times multiple vortices may be visible are when the tornado is first forming or when condensation and debris are balanced such that subvortices are apparent without being obscured. They can add over 100 mph to the ground-relative wind in a tornado circulation and are responsible for most cases where narrow arcs of extreme destruction lie right next to weak damage within tornado paths.^[1]

Suction vortices, also known as suction spots, are substructures found in many tornadoes, though they are not always easily visible. These vortices typically occur at the base of the tornado, where it makes contact with the ground. Sub-vortices tend to form after vortex breakdown reaches the surface, resulting from the interaction of cyclonically incoming and rising air. Although multi-vortex structures are common in tornadoes, they are not unique to them and can occur in other circulations, such as dust devils. This is a natural result of vortex dynamics in physics. Multi-vortex tornadoes should not be confused with cyclically tornadicsupercells. Supercells are large, rotating thunderstorms that can produce multiple, distinct tornadoes, often referred to astornado families. These tornadoes may form at different times or exist simultaneously but are separate from one another.

A phenomenon similar to multiple vortices is thesatellite tornado. Unlike the multiple-vortex tornado, where smaller vortices form inside the main tornado, a satellite tornado develops outside the main tornado's circulation. It forms through a different mechanism, typically as a result of interactions with the parent storm's environment. Despite appearing close to the primary tornado, satellite tornadoes are independent and can have their own rotation.^[1]

In rare instances, multi-vortex tornadoes may display their strength through the uncommon method of "horizontal vorticies" which involves tornadoes appearing to "bend" the multiple vorticies included inside of the tornado, resulting in a tornado appearing to have thin lines stretching out of them. A particularly famous example of horizontal vorticies is the2011 Tuscaloosa EF4.

The largest tornado ever documented was a multiple-vortex tornado. It struckEl Reno, Oklahoma, on May 31, 2013, as a rain-wrapped tornado, taking the lives of tornado researcherTim Samaras, his son Paul, and theirTWISTEX colleague, Carl Young. This storm also took the life of local amateur chaser, Richard Henderson.^[2] It had a maximum width of 2.6 miles (4.2 km) and a maximum recorded windspeed of at least 313 miles per hour (504 km/h). However, because of a lack of intense property damage, the tornado achieved a rating of EF3 on theEnhanced Fujita scale.^[3] Nevertheless, the El Reno tornado is one of the three strongest tornadoes ever recorded in terms of maximum wind speeds, the next being the2024 Greenfield EF4 tornado, reaching a measured windspeed of possibly up to 321 miles per hour (517 km/h), the last being the1999 Bridge Creek–Moore tornado whichdoppler radar measured 321 miles per hour (517 km/h) mph. The Greenfield tornado also displayed multiple vortices.

The1997 Jarrell tornado was another example of a multiple-vortex tornado. The infamous “Dead Man Walking” photo of it was at a juvenile stage of sub-vortices development. The2011 Cullman–Arab tornado is also famous for footage of it "walking" while in its multi-vortex stage.

• Tornadogenesis

• Multiple Vortex Tornado at the Online Tornado FAQ

• Tornado

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