On 18 January 2003, fires had a devastating impact on Australia's capital, Canberra. A series of reviews and scientific studies have examined the events of that day and indicate that the worst impacts were due to a series of violent pyro-convective events and resultant pyro-cumulonmibi. These coupled fire-atmosphere events are much more energetic than normal fires. In one instance, an intense pyro-convective cell developed a tornado. We demonstrate that this was indeed a tornado, the first confirmed pyro-tornadogenesis in Australia, and not a fire whirl. Here, we discuss aspects of the formation, evolution and decay of the tornado, which was estimated to have been of at least F2 intensity, highlighting a process that can significantly increase the damage of a wildfire event. © 2012 Springer Science+Business Media Dordrecht.
CITATION STYLE
McRae, R. H. D., Sharples, J. J., Wilkes, S. R., & Walker, A. (2013). An Australian pyro-tornadogenesis event. Natural Hazards, 65(3), 1801–1811. https://doi.org/10.1007/s11069-012-0443-7
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