A fire whirl – also colloquially known as a fire devil, fire tornado, firenado, or fire twister – is a whirlwind induced by a fire and often made up of flame or ash. Fire whirls may occur when intense rising heat and turbulent wind conditions combine to form whirling eddies of air. These eddies can contract into a tornado-like structure that sucks in burning debris and combustible gases. Rarely, however, do fire whirls grow to become actual tornadoes, which are violently rotating vortices connecting the surface to a cumuliform (such as pyrocumulus or pyrocumulonimbus) cloud base.
A fire whirl consists of a core – the part that is actually on fire – and an invisible rotating pocket of air. A fire whirl can reach up to 2,000 °F (1,090 °C) – hot enough to potentially reignite ashes sucked up from the ground. Often, fire whirls are created when a wildfire or firestorm creates its own wind, which can turn into a spinning vortex of flame.
Combustible, carbon-rich gases released by burning vegetation on the ground are fuel for most fire whirls. When sucked up by a whirl of air, this unburned gas travels up the core until it reaches a region where there is enough fresh, heated oxygen to set it ablaze. This causes the tall and skinny appearance of a fire whirl's core.
Real-world fire whirls usually move fairly slowly. Fire whirls can set objects in their paths ablaze and can hurl burning debris out into their surroundings. The winds generated by a fire whirl can also be dangerous. Large fire whirls can create wind speeds of more than 100 mph (160 km/h) – strong enough to knock down trees – and people who get caught by a fire whirl can be burned alive.
Fire whirls can last for an hour or more, and they cannot be extinguished directly.
During the 2003 Canberra bushfires, a fire whirl with a diameter of nearly 500 metres (1,600 ft) with horizontal winds exceeding 250 km/h (160 mph) was documented. Further research into the fires confirmed this in 2012. In Canberra, wind damage consistent with an F2 tornado on the Fujita Scale was observed, in addition to the fire damage. New research released in 2013 showed that the supercell thunderstorm that caused the tornado originated from the converging winds of firestorm itself, one of the first confirmed observations of an intense thunderstorm forming from a Pyrocumulonimbus cloud.
Another extreme example of a fire tornado is the 1923 Great Kantō earthquake in Japan which ignited a large city-sized firestorm and produced a gigantic fire whirl that killed 38,000 people in fifteen minutes in the Hifukusho-Ato region of Tokyo.
Another example is the numerous large fire whirls (some tornadic) that developed after lightning struck an oil storage facility near San Luis Obispo, California on 7 April 1926, several of which 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 thunderstorms, in which the larger fire whirls carried debris 5 kilometers away.
There are currently three known 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 Great Kanto Earthquake of 1923, was of type 3.
A "firecane" refers to a never observed hypothetical confluence of meteorological and man-made disasters, whereby a hurricane crossing an oil-laden expanse of water generates lightning which ignites the flammable fossil fuel, creating a vortex of fire. A fearful imagining born of recent cataclysms in the Gulf of Mexico, the term has gained currency in New Orleans, the city inundated by Hurricane Katrina in 2005, and which in 2010 was near the site of the Deepwater Horizon oil spill. The likelihood of such an occurrence has been dismissed by meteorologist Dr. Jeff Masters of the Weather Underground weather service, who contends that wave action and rain water would quickly douse a fire set by a lightning strike on fresh oil. Lightning strikes from thunderstorms may cause isolated fires, as happened on a drill ship near the spill.
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- Williams, Forman (22 May 2009). "The Occurrence and Mechanisms of Fire Whirls" (PDF). La Lolla, California; Valladolid, Spain: MAE UCSD; Spanish Section of the Combustion Institute.
- Kuwana, Kazunori; Kozo Sekimoto; Kozo Saito; Forman A. Williams (May 2008). "Scaling fire whirls". Fire Safety Journal 43 (4): 252–7. doi:10.1016/j.firesaf.2007.10.006.
- Jacobsen, Mark (June 6, 2010). "New Orleans Residents Are Fearful of a Oil-Spill-Triggered Firecane". New York. Retrieved 19 August 2015.
- Masters, Jeff. "What would a hurricane do to the Deepwater Horizon oil spill?". Weather Underground. Retrieved 19 August 2015.
- Pydynowski, Kristina; et al. (June 25, 2010). "Air Quality Not a Concern, but Lightning Remains a Threat Over Spill Area". AccuWeather. Retrieved 19 August 2015.
- Church, Christopher R.; John T. Snow; Jean Dessens (1980). "Intense Atmospheric Vortices Associated with a 1000 MW Fire". B. Am. Meteorol. Soc. 61 (7): 682–94. Bibcode:1980BAMS...61..682C. doi:10.1175/1520-0477(1980)061<0682:IAVAWA>2.0.CO;2.
- Fire Whirl Simulations
|Wikimedia Commons has media related to Fire whirls.|
- Fire tornado video (whirl) 11 September 2012 Alice Springs Australia
- www.abc.net.au/news Australian researchers document world-first fire tornado.
- Catalyst story: Fire Tornado
- Another photo
- www.youtube.com Video of a Fire whirl (0:30), Brazil.
- "Rare Footage of Fire Tornado". BBC. 25 Aug 2010.
- Video of a Fire Tornado in San Diego country