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2011 - Cooperative Institute for Research in Environmental Sciences ...

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Roger Pielke, Jr.<br />

Influence of Location, Population and Climate<br />

on Build<strong>in</strong>g Damage and Fatalities Due to<br />

Australian Bushfire: 1925–2009<br />

FUNDING: NATIONAL SCIENCE FOUNDATION<br />

This study (Crompton<br />

et al., 2010), conducted<br />

<strong>in</strong> collaboration with<br />

colleagues at Macquarie<br />

University <strong>in</strong> Sydney,<br />

Australia, reevaluates<br />

the history of build<strong>in</strong>g<br />

damage and loss of life<br />

due to bushfire (wildfire)<br />

<strong>in</strong> Australia s<strong>in</strong>ce 1925<br />

<strong>in</strong> light of the 2009 Black<br />

Saturday fires <strong>in</strong> Victoria<br />

<strong>in</strong> which 173 people lost<br />

their lives and 2,298 homes<br />

were destroyed along with<br />

many other structures. Historical<br />

records are normalized<br />

to estimate build<strong>in</strong>g<br />

damage and fatalities had<br />

events occurred under the<br />

societal conditions of 2008/09. There are relationships between<br />

normalized build<strong>in</strong>g damage and the El Niño–Southern<br />

Oscillation and Indian Ocean dipole phenomena, but there is<br />

no discernable evidence that the normalized data are be<strong>in</strong>g<br />

Aerial view of northern Sydney show<strong>in</strong>g the highly dissected and complex<br />

<strong>in</strong>terface (red l<strong>in</strong>e) between brushland (dark green) and urban areas.<br />

<strong>in</strong>fluenced by climatic change due to the emission of greenhouse<br />

gases.<br />

Our result—that there is no discernable evidence that<br />

normalized build<strong>in</strong>g damage is be<strong>in</strong>g <strong>in</strong>fluenced by climate<br />

change due to the emission of greenhouse gases—is not surpris<strong>in</strong>g<br />

when you consider that bushfire damage is not solely<br />

a function of bushfire weather; far from it, <strong>in</strong> fact. Even given<br />

a gradual aggravation of bushfire weather due to anthropogenic<br />

climate change or other factors, a bushfire still has to<br />

be ignited. Once ignited, a bushfire then has to traverse the<br />

landscape and impact a populated area, where outcomes <strong>in</strong><br />

terms of damage will be a function of the spatial disposition of<br />

dwell<strong>in</strong>gs with respect to the fire front, and especially distance<br />

of properties from the bushland boundary (McAneney et al.,<br />

2009). These factors all contribute a large degree of stochasticity<br />

to eventual event-loss outcomes.<br />

Annual Aggregated Bushfire HE/Fatalities and Correspond<strong>in</strong>g Normalized Values <strong>for</strong> Bushfire Years 192-2008<br />

Figure 1: (a) Annual aggregate house equivalents (HE)<strong>for</strong><br />

bushfire events <strong>in</strong> Peril, Australia, <strong>for</strong> years beg<strong>in</strong>n<strong>in</strong>g July 1; (b)<br />

as <strong>in</strong> (a) but with HE normalized to 2008 brushfire year values.<br />

Figure 2: (a) Annual aggregate fatalities <strong>for</strong> brushfire events <strong>in</strong> the<br />

Haynes et al. (2010) database <strong>for</strong> years beg<strong>in</strong>n<strong>in</strong>g July 1; (b) as <strong>in</strong><br />

(a) but with fatalities normalized to 2008 brushfire year values.<br />

CIRES Annual Report <strong>2011</strong> 45

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