Evolution of a pyrocumulonimbus event associated with an extreme wildfire in Tasmania, Australia
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Published:2020-05-27
Issue:5
Volume:20
Page:1497-1511
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ISSN:1684-9981
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Container-title:Natural Hazards and Earth System Sciences
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language:en
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Short-container-title:Nat. Hazards Earth Syst. Sci.
Author:
Ndalila Mercy N.ORCID, Williamson Grant J.ORCID, Fox-Hughes Paul, Sharples Jason, Bowman David M. J. S.ORCID
Abstract
Abstract. Extreme fires have substantial adverse effects on society and
natural ecosystems. Such events can be associated with the intense coupling of
fire behaviour with the atmosphere, resulting in extreme fire
characteristics such as pyrocumulonimbus cloud (pyroCb) development. Concern
that anthropogenic climate change is increasing the occurrence of pyroCbs
globally is driving more focused research into these meteorological
phenomena. Using 6 min scans from a nearby weather radar, we describe the
development of a pyroCb during the afternoon of 4 January 2013 above the
Forcett–Dunalley fire in south-eastern Tasmania. We relate storm development
to (1) near-surface weather using the McArthur forest fire danger index
(FFDI) and the C-Haines index, the latter of which is a measure of the vertical atmospheric
stability and dryness, both derived from gridded weather reanalysis for
Tasmania (BARRA-TA); and (2) a chronosequence of fire severity derived from
remote sensing. We show that the pyroCb rapidly developed over a 24 min
period on the afternoon of 4 January, with the cloud top reaching a height
of 15 km. The pyroCb was associated with a highly unstable lower atmosphere
(C-Haines value of 10–11) and severe–marginally extreme (FFDI 60–75) near-surface
fire weather, and it formed over an area of forest that was severely burned
(total crown defoliation). We use spatial patterns of elevated fire weather
in Tasmania and fire weather during major runs of large wildfires in
Tasmania for the period from 2007 to 2016 to geographically and historically
contextualise this pyroCb event. Although the Forcett–Dunalley fire is the
only known record of a pyroCb in Tasmania, our results show that eastern and
south-eastern Tasmania are prone to the conjunction of high FFDI and
C-Haines values that have been associated with pyroCb development. Our
findings have implications for fire weather forecasting and wildfire
management, and they highlight the vulnerability of south-east Tasmania to extreme
fire events.
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences
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