2017
DOI: 10.22499/3.6702.002
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Meteorological drivers of extreme fire behaviour during the Waroona bushfire, Western Australia, January 2016

Abstract: During the first two days of the fire, there were two pyrocumulonimbus (pyroCb) events and two destructive evening fire runs. Over 160 homes were destroyed and there were two fatalities. This case study examines in detail the links between the meteorological observations and the fire behaviour reconstruction.

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Cited by 15 publications
(28 citation statements)
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“…The fire history of the upper catchment is reasonably well known (Peace et al 2017). Remnant forest areas have not been subject to fire for several decades, with fuel age dating back to the last time broad-scale aerial fuel reduction burning was undertaken in the late 1980s and early 1990s.…”
Section: Study Areamentioning
confidence: 99%
“…The fire history of the upper catchment is reasonably well known (Peace et al 2017). Remnant forest areas have not been subject to fire for several decades, with fuel age dating back to the last time broad-scale aerial fuel reduction burning was undertaken in the late 1980s and early 1990s.…”
Section: Study Areamentioning
confidence: 99%
“…The burn containment line is indicated in pink in the bottom panel. The Waroona fire panels are adapted with permission from Peace et al (), and the Apsey West panels are modified from McCarthy et al ().…”
Section: Observational Case Studiesmentioning
confidence: 99%
“…For example, Fromm et al () and McRae et al () both examine the Canberra (Australia) conflagration and pyroCb of 2003, which inferred a pyrogenic tornado, though the lack of Doppler data prohibited the identification of vortices, limiting the analyses of storm evolution. Peace et al () analyzed the growth and structural aspects of two pyrocumulonimbus events during the Waroona bushfire (Western Australia). Analysis of the evolution with radar included initiation along a sea‐breeze boundary, surface and elevated core formation, downdraft core formation, and vertically aligned vortex imbedded within a pyroCb as shown in Figure .…”
Section: Observational Case Studiesmentioning
confidence: 99%
“…For example, on the high ends of those scales, low humidity and lack of rain for several months can desiccate dead fuel, leading to more large fires and greater area burned [55]. On the low ends of those scales, outflow from a pyrocumulonimbus generated by a fire can, in turn, modify that same fire's immediate environment [56,57]. To be most effective, modeling systems for simulating wildfires and the smoke they generate (see Section 8) must account for these interactions [58][59][60].…”
Section: Ecologymentioning
confidence: 99%