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.
Fire whirls can last for an hour or more, and they cannot be extinguished directly.
A Firecane refers to a 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 commercial 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.
Another proposed scenario is that oil from the spill would be carried by hurricane winds and deposited over land, where hot weather could subsequently kindle flammable materials that have been strewn over a dry wooded landscape. In addition to being spread by rain and wind, there is concern that oil will be moved inland by a storm surge.
Absent apocalyptic visions of a firestorm, the Deepwater Horizon spill, coupled with the onset of the 2010 hurricane season, generated speculation as to the possibility of increased ecological damage in the event of a powerful tropical storm in the region. Since such an event has not occurred, there is uncertainty as to whether a hurricane would exacerbate the effects of the spill, or as to how the presence of massive volumes of oil would alter the course of a major storm.
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 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.
- Jason Fortofer (20 September 2012) http://news.nationalgeographic.com/news/2012/09/pictures/120920-fire-tornadoes-vortex-firenadoes-devils-science-weather/#/new-fire-tornado-spotted-australia_59442_600x450.jpg
- Firecane! Fear in New Orleans
- What would a hurricane do to the Deepwater Horizon oil spill?
- Air Quality Not a Concern, but Lightning Remains a Threat Over Spill Area
- Will Hurricane Season Mean “Oilmageddon” For The United States?
- Hurricane, Oil Spill Could Be Troubling Mix
- Hurricane vs. Oil Slick
- Jessica Nairn (20 November 2012). "Researchers document world-first fire tornado". Australian Broadcasting Corporation. Retrieved 20 November 2012.
- McRae, >McRae, R et al. (1 October 2012). "An Australian pyro-tornadogenesis event.". Natural Hazards, Springer Netherlands. Retrieved 20 November 2012.
- Anja Taylor (6 June 2013). "Fire Tornado". Australian Broadcasting Corporation. Retrieved 6 June 2013.
- Quintiere, James G. (1998). Principles of Fire Behavior. Thomson Delmar Learning. ISBN 0-8273-7732-0.
- Hissong, J. E. (1926). "Whirlwinds At Oil-Tank Fire, San Luis Obispo, Calif.". Mon. Wea. Rev. 54 (4): 161–3. Bibcode:1926MWRv...54..161H. doi:10.1175/1520-0493(1926)54<161:WAOFSL>2.0.CO;2.
- 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.
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- Fire Whirl Simulations
- 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