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A fire whirl, fire devil or fire tornado is a induced by a and often (at least partially) composed of or . These start with a whirl of , often made visible by , and may occur when intense rising heat and turbulent wind conditions combine to form whirling eddies of air. These eddies can contract to a -like that sucks in debris and combustible gases.

The phenomenon is sometimes labeled a fire tornado, firenado, fire swirl, or fire twister, but these terms usually refer to a separate phenomenon where a fire has such intensity that it generates an actual tornado. Fire whirls are not usually classifiable as tornadoes as the vortex in most cases does not extend from the surface to cloud base. Also, even in such cases, those fire whirls very rarely are classic tornadoes, as their derives from surface and heat-induced lifting, rather than from a tornadic aloft.

The phenomenon was first verified in the 2003 Canberra bushfires and has since been verified in the 2018 in California, and the 2020 in California and Nevada.


Formation
A fire whirl consists of a burning core and a rotating pocket of air. A fire whirl can reach up to .Fortofer, Jason (20 September 2012) "New Fire Tornado Spotted in Australia" National Geographic Fire whirls become frequent when a , or especially , creates its own wind, which can spawn large vortices. Even often have whirls on a smaller scale and tiny fire whirls have been generated by very small fires in laboratories.

Most of the largest fire whirls are spawned from wildfires. They form when a warm and convergence from the wildfire are present. They are usually tall, a few meters (several feet) wide, and last only a few minutes. Some, however, can be more than tall, contain over , and persist for more than 20 minutes.

(1993). 9781879362031, The Tornado Project of Environmental Films.

Fire whirls can uproot trees tall or more. These can also aid the 'spotting' ability of wildfires to propagate and start new fires as they lift burning materials such as tree bark. These burning embers can be blown away from the fire-ground by the stronger winds aloft.

Fire whirls can be common within the vicinity of a during a volcanic eruption. These range from small to large and form from a variety of mechanisms, including those akin to typical fire whirl processes, but can result in Cumulonimbus flammagenitus (cloud) spawning and or even to develop mesocyclone-like updraft rotation of the plume itself and/or of the cumulonimbi, which can spawn tornadoes similar to those in . Pyrocumulonimbi generated by large fires on rare occasions also develop in a similar way.


Classification
There are currently three widely recognized types of fire whirls:

  • Type 1: Stable and centered over burning area.
  • Type 2: Stable or transient, downwind of burning area.
  • Type 3: Steady or transient, centered over an open area adjacent to an asymmetric burning area with wind.

There is evidence suggesting that the fire whirl in the Hifukusho-ato area, during the 1923 Great Kantō earthquake, was of type 3. Other mechanism and fire whirl dynamics may exist. A broader classification of fire whirls suggested by Forman A. Williams includes five different categories:

  • Whirls generated by fuel distribution in wind
  • Whirls above fuels in pools or on water
  • Tilted fire whirls
  • Moving fire whirls
  • Whirls modified by vortex breakdown

The meteorological community views some fire-induced phenomena as atmospheric phenomena. Using the pyro- prefix, fire-induced clouds are called and . Larger fire vortices are similarly being viewed. Based on vortex scale, the classification terms of pyronado, "pyrotornado", and "pyromesocyclone" have been proposed.


Notable examples
During the 1871 , the community of Williamsonville, , was burned by a fire whirl; the area where Williamsonville once stood is now Tornado Memorial County Park. Tornadoes of Fire at Williamsonville, Wisconsin, October 8, 1871 by Joseph M. Moran and E. Lee Somerville, 1990, Wisconsin Academy of Sciences, Arts, and Letters, 31 pp. Tornado Memorial Park kiosk historical notes, also see p. 19 of the County C Park and Ride lot panel draft pdf

An extreme example of the phenomenon occurred in the aftermath of the 1923 Great Kantō earthquake in Japan, in which a city-wide in produced the conditions required for a gigantic fire whirl that killed 38,000 people in fifteen minutes in the Hifukusho-Ato region of the city.

(1998). 9780827377325, Thomson Delmar Learning.

Numerous large fire whirls (some tornadic) that developed after struck an oil storage facility near San Luis Obispo, , on 7 April 1926, produced significant structural damage well away from the fire, killing two. Many whirlwinds were produced by the four-day-long firestorm coincident with conditions that produced severe , in which the larger fire whirls carried debris away.

Fire whirls were produced in the and firestorms triggered by of European and Japanese cities during World War II and by the atomic bombings of Hiroshima and Nagasaki. Fire whirls associated with the bombing of Hamburg, particularly those of 27–28 July 1943, were studied.

Throughout the 1960s and 1970s, particularly in 1978–1979, fire whirls ranging from the transient and very small to intense, long-lived tornado-like vortices capable of causing significant damage were spawned by fires generated from the 1000 Météotron, a series of large oil wells located in the plain of used for testing atmospheric motions and thermodynamics.

During the 2003 Canberra bushfires in , , a violent fire whirl was documented. It was calculated to have horizontal winds of and vertical air speed of , causing the of in 0.04 seconds. It was the first known fire whirl in Australia to have EF3 wind speeds on the Enhanced Fujita scale.

On May 22, 2015, a float-equipped Air Tractor AT-802 fighting a fire near Cold Lake, Alberta encountered a fire whirl. The encounter resulted in a loss of control and collision with terrain, killing the pilot on board. A fire whirl, of reportedly uncommon size for New Zealand wildfires, formed on day three of the 2017 Port Hills fires in . Pilots estimated the fire column to be high.

On July 26, 2018, the massive 2018 Carr Fire tornado would hit Redding, California.

On August 15, 2020, for the first time in its history, the U.S. National Weather Service issued a tornado warning for a created by a wildfire near Loyalton, California, capable of producing a fire tornado.

On January 11, 2025, a fire whirl was spotted in the .


Blue whirl
In controlled small-scale experiments, fire whirls are found to transition to a mode of combustion called blue whirls. The name blue whirl was coined because the soot production is negligible, leading to the disappearance of the yellow color typical of a fire whirl. Blue whirls are partially premixed flames that reside elevated in the recirculation region of the vortex-breakdown bubble. The flame length and burning rate of a blue whirl are smaller than those of a fire whirl.


See also


Further reading

External links

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