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Mini-tornado – A fallacious term often used in European news media to refer to tornadoes occurring there; even large, strong, and/or long track tornadoes produced by supercells. This is apparently due to the erroneous perception that "real" tornadoes do not occur in Europe (or elsewhere where the term is applied).
A fire whirl, fire devil or fire tornado is a whirlwind induced by a fire and often (at least partially) composed of flame or ash.These start with a whirl of wind, often made visible by smoke, and may occur when intense rising heat and turbulent wind conditions combine to form whirling eddies of air.
The terms fire whirl and fire tornado have often been used interchangeably to describe a vortex of any size or duration occurring in a wildfire. Only in recent years have scientists begun to distinguish types of vortices from one another, in particular highlighting the rare cases of actual pyro-tornadogenesis (or tornado formation during/due to ...
In late July in the midst of the record-breaking wildfire, a powerful spinning vortex emerged that rose 18,000 feet in the air, with wind speeds exceeding 143 mph, and lasted for an hour and a half.
A “fire tornado” swirled as a wildfire raged in British Columbia, Canada, last Thursday (17 August). Dramatic footage captured by overnight ground personnel responding to the Downton Lake ...
Fire whirls or swirls, sometimes called fire devils or fire tornadoes, can be seen during intense fires in combustible building structures or, more commonly, in forest or bush fires. A fire whirl is a vortex-shaped formation of burning gases being released from the combustible material. The genesis of the vortex is probably similar to a dust ...
The tornadoes stemmed from the Park Fire, which started after a 42-year-old man from Chico allegedly pushed a burning car into a ditch. The fire engulfed 164,000 acres in 36 hours. The fire ...
Although the term has been used to describe certain large fires, [1] the phenomenon's determining characteristic is a fire with its own storm-force winds from every point of the compass towards the storm's center, where the air is heated and then ascends.