BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT

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BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT
BE PREPARED:
CLIMATE
CHANGE AND
THE VICTORIAN
BUSHFIRE
THREAT

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providing quality information on climate change to the Australian public.

CLIMATECOUNCIL.ORG.AU
BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT
Authorship:
Professor Lesley Hughes
Published by the Climate Council of Australia Limited
ISBN:    978-0-9941866-5-2 (print)
         978-0-9941866-4-5 (web)
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Be Prepared: Climate Change and the Victorian bushfire threat
by Professor Lesley Hughes (Climate Council of Australia).

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Professor Lesley Hughes Climate Councillor

                  Professor Lesley Hughes
                  Climate Councillor
BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT
Introduction
Residents of Victoria have experienced      This report first describes the
the serious consequences of bushfires.      background context of fire and its
Although Victoria comprises only            history in Victoria. We then outline the
3% of Australia’s land mass, more           link between bushfires and climate
than half of all known fatalities due       change, before considering how bushfire
to bushfires have occurred in Victoria,     danger weather is increasing in Victoria
and the state has sustained around          and what this means for the immediate
50% of the economic damage.                 future. We explore the impacts of fire
Australians have always lived with          on people, property, water supply and
fire and its consequences, but climate      biodiversity, before considering the
change is increasing fire danger weather    future influence of climate change
and thus the risk of fires. It is time to   on bushfires, and the implications
think very seriously about the risks        for Victorian fire managers, planners
that future fires will pose.                and emergency services.

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                Key Findings
                1. Climate change is increasing                 ›› Victoria’s 2014–15 bushfire season
                   the risk of bushfires in Victoria               outlook has been upgraded
                   and lengthening the fire                        from an “above normal” fire
                   season.                                         season to a “major” fire season
                                                                   following record October warmth
                   ›› Extreme fire weather has increased
                                                                   and expected ongoing hot, dry
                      over the last 30 years in Victoria.
                                                                   conditions.
                      The fire season in Victoria is
                      starting earlier and lasting longer.   3. Recent severe fires in Victoria
                      Fire weather has been extending           have been influenced by
                      into October and into March.              record hot, dry conditions.
                   ›› Australia is a fire prone country         ›› The 2009 Black Saturday fires in
                      and Victoria has always                      Victoria were preceded by a record
                      experienced bushfires. Today                 breaking decade-long drought
                      climate change is making hot days            with a string of record hot years,
                      hotter, and heatwaves longer and             coupled with a severe heatwave
                      more frequent, with increasing               in the preceding week.
                      drought conditions in Australia’s
                                                                ›› In the lead up to the bushfires
                      southeast.
                                                                   on Saturday 7th 2009, maximum
                   ›› Record breaking heat and hotter              temperatures were up to 23°C
                      weather over the long term in                above the February average
                      Victoria has worsened fire weather           in Victoria and record high
                      and contributed to an increase               temperatures for February were
                      in the frequency and severity                set in over 87% of the state.
                      of bushfires.
                                                             4. In Victoria the economic
                2. Victoria is the state most                   cost of bushfires, including
                   affected by bushfires and is                 loss of life, livelihoods,
                   on the frontline of increasing               property damage and
                   bushfire risk.                               emergency services
                   ›› Over half of known fatalities due         responses, is very high.
                      to bushfires in Australia have
                                                                ›› The total economic costs of
                      occurred in Victoria.
                                                                   bushfires in Victoria in 2014
                   ›› Victoria has sustained around                are projected to be more than
                      50% of the economic damage from              $172 million. By around the middle
                      bushfires despite covering only              of the century these costs will
                      3% of Australia.                             more than double.

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BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT
›› These projections do not              ›› Increasing severity, frequency and
     incorporate increased bushfire           the lengthening fire season will
     incident rates due to climate            strain Victoria’s existing resources
     change and so could potentially          for fighting and managing fires.
     be much higher.
                                           ›› By 2030, it has been estimated
  ›› Livestock losses were estimated          that the number of professional
     at 13,000 in the 2003 Alpine fires       firefighters in Victoria will need to
     in Victoria, 65,000 in the 2005–6        approximately double (compared to
     Grampians fire and more than             2010) to keep pace with increased
     11,000 in the Black Saturday fires.      population, asset value, and fire
                                              danger weather.
5. In the future, Victoria is
   very likely to experience an            ›› Australia must cut its emissions
   increased number of days                   rapidly and deeply to join global
   with extreme fire danger.                  efforts to stabilise the world’s
   Communities, emergency                     climate and to reduce the risk
   services and health services               of even more extreme events,
   across Victoria must prepare.              including bushfires.
  ›› Fire severity and intensity is
     expected to increase substantially
     in coming decades in Victoria.
     The fire season will continue to
     lengthen, further reducing the
     opportunities for safe hazard
     reduction burning.

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    1. The nature of bushfires
                  Fire has been a feature of the Australian      The unprecedented ferocity of the
                  environment for at least 65 million years      2009 Black Saturday bushfires in Victoria
                  (Cary et al. 2012). Human management of        saw a new ‘catastrophic’ category added
                  fires also has a long history, starting with   to the FFDI for events exceeding the
                  fire use by indigenous Australians (“fire-     existing scale.
                  stick farming”) up to 60,000 years ago.
                                                                 The concept of “fire regimes” is
                  Between 3% and 10% of Australia’s land
                                                                 important for understanding the
                  area burns every year (Western Australian
                                                                 nature of bushfires in Australia, and
                  Land Information Authority 2013).
                                                                 for assessing changes in fire behaviour
                  In Australia, the Forest Fire Danger           caused by both human and climatic
                  Index (FFDI) is used to measure the            factors (Figure 2). A fire regime describes
                  degree of risk of fire in our forests          a recurrent pattern of fire, with the most
                  (Luke and Macarthur 1978). The                 important characteristics being the
                  Bureau of Meteorology (BoM) and fire           frequency, intensity, and seasonality
                  management agencies use the FFDI               of the fire. Significant changes in any
                  to assess fire risk and issue warnings.        of these features of a fire regime can
                  The index was originally designed on a         have a very important influence on
                  scale from 0 to 100, with fires between        its ecological and economic impacts
                  75 and 100 considered ‘extreme’.               (Williams et al. 2009).

    Figure 1: Trees burn in Bullumwaal, Victoria

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BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT
01
                                             THE NATURE OF BUSHFIRES IN AUSTRALIA

                                                                Figure 4. Main factors affecting bushfires

       Main factors                                                               3 | People
                                                         Fires may be deliberately started
                                                         (arson) or be started by accident

       affecting                                         (e.g. by powerline fault). Human
                                                            activities can also reduce fire,
                                                              either by direct suppression

       bushfires                                                or by reducing fuel load by
                                                                        prescribed burning

       1 | Ignition
       Fires can be started
       by lightning or
       people, either
       deliberately or
       accidentally

       2 | Fuel
       Fires need fuel of
       sufficient quantity &
       dryness. A wet year creates
       favourable conditions
       for vegetation growth. If                                               4 | Weather
       this is followed by a dry               Fires are more likely to spread on hot, dry,
       season or year, fires are              windy days. Hot weather also dries out fuel,
       more likely to spread and                       favouring fire spread and intensity
       become intense

Figure 2: Main factors affecting bushfires
       CLIMATECOUNCIL.ORG.AU                                                               Page 6

CLIMATECOUNCIL.ORG.AU                                                                                 Page 5
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                Fire is a complex process that is very         between rainfall and fuel is complex.
                variable in space and time. A fire             Wet seasons can lead to increased
                needs to be started (ignition), it needs       plant growth and therefore increase
                something to burn (fuel) and it needs          fuel buildup in the months or years
                conditions that are conducive to its           before a fire is ignited (Bradstock et
                spread (weather and topography)                al. 2009). Warmer temperatures and
                (see Figure 2). Fire activity is strongly      low rainfall in the period immediately
                influenced by weather, fuel, terrain,          preceding an ignition, however,
                ignition agents and people. The most           can lead to drier vegetation and
                important aspects of weather that              soil, making the existing fuel more
                affect fire and fuels are temperature,         flammable. Warmer temperatures
                precipitation, wind and humidity. Once         can also be associated with a higher
                a fire is ignited, very hot days with low      incidence of lightning activity (Jayaratne
                humidity and high winds are conducive          and Kuleshov, 2006), increasing the
                to its spread. The type, amount, and           risk of ignition. In many regions
                moisture level of fuel available are also      local weather conditions are the most
                critical determinants of fire behaviour,       important influence on fire activity
                extent and intensity. The relationship         (Climate Council 2014a).

    “The most important aspects of weather
    that affect fire and fuels are temperature,
    precipitation, wind and humidity”.
                As fire weather conditions become more         People are also a very important
                severe, fuel moisture content declines,        component of the fire equation. Many
                making the fuel more flammable. By             fires are either deliberately or accidentally
                contrast, in arid regions, vegetation          lit, and in places where population
                and thus fuel in most years is sparsely        density is high, the probability of a
                distributed and fires, if ignited, rarely      fire igniting increases close to roads
                spread far. In Australia’s southeast, fires    and settlements (Willis 2005; Penman
                are common in the heathlands and dry           et al. 2013). Some of Australia’s most
                sclerophyll forests, such as the mountain      catastrophic bushfires have been ignited
                ash forests in Victoria, typically occurring   by powerline faults. But people also play
                about every 5 to 30 years, with spring and     an important role in reducing fire risk,
                summer being peak fire season (Clarke et       by vegetation management including
                al. 2011; Bradstock et al. 2012).              prescribed burning to reduce fuel

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BE PREPARED: CLIMATE CHANGE AND THE VICTORIAN BUSHFIRE THREAT
Mildura

                                                                Swan Hill

                                                                                   Gannawarra                                                                            Wodonga

                                                                Buloke
                                    Hindmarsh                                                                                       Moira                 Indigo
                                                                                                              Campaspe
                                                                                       Loddon                                 Greater
                                                                                                                            Shepparton                                             Towong
                                                                                                                                                       Wangaratta
                           West                                  Northern                                                                    Benalla
                          Wimmera                               Grampians

CLIMATECOUNCIL.ORG.AU
                                          Horsham                                                   Bendigo                    Strathbogie                              Alpine

                                                                      Pyrenees       Central        Mount                                    Mansfield
                                                                                    Goldfields     Alexander        Mitchell
                           Goroke

                                        Southern                                                             Macedon                                                                  East Gippsland
                                        Grampians          Ararat                                            Ranges
                                                                                      Ballarat
                                                                                                  Gisborne
                                          Grampians                                               Moorabool                                                          Wellington
                           Glenelg
                                           Ranges
                                                                                   Golden Plains                                                Baw Baw
                               Hamilton
                                                Dunkled Moyne            Skipton                                                                                     Erica
                                                                                                                               Beaumaris
                                                                                                 Surf    Geelong                                         Traralgon
                                                                 Derrinallum
                                                                                                 Coast                                                               Morwell
                                                                            Colac-Otway
                                                                                                                                              South
                                                                                                                                             Gippsland
                                                                                                                Melbourne
                                                      Warrnambool
                                                                                           Birregurra                                                          Yallourn
                                                                               Otway Ranges

                                     1939 Widespread across Victoria including;                                                                                                         2003 North East and Gippsland
                                     Warburton, Erica, Rubicon, Dromana, Manfield,
                                     the Otway ranges and the Grampian Ranges.                                                                                                          2006 Grampian ranges

                                     1944 Central and western districts, Morwell, Yallourn                                                                                              2006–07 Great divide complex

                                     1977 Western Districts                                                                                                                             January 2009 Delburn

                                     1983 Victoria and South Australia including;                                                                                                       February 2009 Churchill, Kilmore and Murrundindi,
                                     Dandenong Ranges east of Melbourne,                                                                                                                Vectis (Horsham), Coleraine, Weerite, Redesdale,
                                     Macedon areas northwest of Melbourne                                                                                                               Harkaway, Upper Ferntree Gully, Maiden Gully /
                                                                                                                                                                                        Eaglehawk, Lynbrook / Narre Warren, Beechworth
                                     1997 Dandenong ranges, Creswick, Heathcote,
                                     Teddywaddy, Gough’s Bay
                                                                                                                                                                                                                          Source: CFA 2012

                        Figure 3: Ten major bushfires in VIC that have damaged homes, property, land and resulted in loss of life since 1939

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                load and conducting fire suppression        state (Haynes et al. 2010). Significant
                activities. Interventions such as total     bushfires in Victoria’s recent history
                fire ban days also play a pivotal role in   that have damaged property and
                reducing ignitions under dangerous fire     resulted in loss of life include the
                conditions (Climate Council 2014a).         Ash Wednesday and Black Saturday
                Victoria is no stranger to bushfires. The   fires (see Figure 3 and Table 2).
                state has been affected by bushfires        Ash Wednesday occurred in February
                throughout its history (see Figure 3). A    1983 in Victoria and South Australia.
                study of significant Australian bushfires   The fires claimed a total of 75 lives
                from 1900–2008 found that over half         (47 in Victoria, 28 in South Australia)
                of all known fatalities due to bushfires    and over 2,300 homes were destroyed
                in Australia have occurred in Victoria      (BoM 2011). The Black Saturday bushfires
                (296 deaths). Extreme fires have also       occurred in February 2009, killing
                destroyed and damaged property more         173 people and destroying over 2000
                frequently in Victoria than in any other    homes (CFA 2012).

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2. What is the link
between bushfires
and climate change?

Figure 4: Aftermath of the Black Saturday bushfires, Victoria

              A fire needs to be started (ignition),       The role of climate change in ignition
              it needs something to burn (fuel) and        is likely to be relatively small compared
              it needs conditions that are conducive       to the fuel and weather, but may still
              to its spread (weather) (Section 1).         be significant. For example, lightning
              Climate change can affect all of these       accounts for about 25% of the ignitions
              factors in both straightforward and          in Victoria (Attiwill and Adams 2011) and
              more complex ways.                           the incidence of lightning is sensitive

CLIMATECOUNCIL.ORG.AU                                                                             Page 9
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     to weather conditions, including            atmosphere – and the incidence of very
     temperature (Jayaratne and Kuleshov         hot days. Put simply, climate change is
     2006). Climate change can also affect       increasing the frequency and severity
     fuel. For example, a lack of rainfall can   of very hot days (IPCC 2012; 2013), and
     dry out the soil and vegetation, making     is driving up the likelihood of very high
     existing fuel more combustible. But         fire danger weather (see Section 3). The
     whilst climate change can affect ignition   Black Saturday fires in Victoria were
     and fuel, it is the impact of climate       preceded by a decade-long drought with
     change on weather that has the most         a string of record hot years, coupled
     significant influence on fire activity      with a severe heatwave in the preceding
     (Climate Council 2014a).                    week. The weather conditions on
     Very hot, dry and windy days create         February 7th broke temperature records,
     very high bushfire risk. The most direct    with maximum temperatures up to
     link between bushfires and climate          23°C above the February average in
     change therefore comes from the             Victoria and record high temperatures
     relationship between the long-term          for February set in over 87% of the state
     trend towards a warmer climate due to       (BoM 2009a; BoM 2009b). In addition the
     increasing greenhouse gas emissions         FFDI ranged from 120 to 190, the highest
     – the increasing amount of heat in the      vales ever recorded (Karoly 2009).

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Figure 5: Climate change and the bushfire threat in Victoria

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     It is important to note that climate        climate change is the wrong question.
     change is already increasing the            All extreme weather events are now
     intensity and frequency of many             being influenced by climate change
     extreme events such as very hot days        because they are occurring in a climate
     and droughts. The strength of trends        system that is hotter and moister than
     and the confidence in their attribution,    it was 50 years ago (Trenberth 2012).
     however, varies between regions and         The latest IPCC report confirms with
     between different types of event (IPCC      high confidence (95% likelihood) that
     2012; 2013; 2014). Extreme weather          climate change is expected to increase
     events, like bushfires, are influenced by   the number of days with very high and
     a number of different factors. That’s why   extreme fire weather, particularly in
     asking if a weather event is “caused” by    southern Australia (IPCC 2014).

    “Climate change is expected to increase
    the number of days with very high and
    extreme fire weather, particularly in
    southern Australia”.

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3. Observations of
changing bushfire danger
weather in Victoria
          Increasing hot days, heatwaves and          For example, in Melbourne from
          rainfall deficiencies in Victoria are       1951–2011, the average intensity of
          driving up the likelihood of very high      heatwaves has increased by 1.5°C
          fire danger weather in the state.           and the average intensity of the peak
          While hot weather has always occurred       day during a heatwave has increased
          in Australia’s southeast, it has become     by 2°C (Climate Council 2014c). This
          more common and severe over the past        has implications for bushfire danger
          few decades, including in Victoria (see     weather; for example the heatwave
          Figure 7). The southeast of Australia       prior to the 2009 Black Saturday
          has experienced significant warming         bushfires was notable both for its
          during the last 50 years (Timbal et         peak intensity and duration, with
          al. 2012). 2013 was the hottest year        maximum temperatures up to 23°C
          on record and during the summer of          above the February average in Victoria
          2013–14 Victoria experienced its hottest    (BoM 2009a; BoM 2009b). The IPCC
          four days on record from the 14–17th        projects with virtual certainty that
          of January. Melbourne set a record for      warming in Australia will continue
          four consecutive days at 41°C and above,    throughout the 21st century and
          and two nights in a row at 27°C or above    predicts with high confidence that
          (BoM 2014a; Climate Council 2014b).         bushfire danger weather will increase
          Heatwaves in Victoria are increasing        in most of southern Australia,
          in frequency, intensity and duration.       including Victoria (IPCC 2014).

          Figure 6: Cars destroyed in the Black Saturday bushfires, Victoria

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    Figure 7: Victoria’s increasing heat (Australian Bureau of Meteorology). Blue bars indicate
    years where annual temperatures were below average, and red bars indicate years of above
    average temperatures.

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“Rainfall has declined in southeast
Australia over the last 20 years”.
          Much of eastern Australia has become         25 percent decline in average rainfall in
          drier since the 1970s, with the southeast    April and May (CSIRO & BoM 2014). It is
          experiencing a drying trend due to           very likely that an increased incidence
          declines in rainfall combined with           of drought in the southeast-coupled
          increased temperatures (BoM 2013;            with consecutive hot and dry days –
          Climate Commission 2013). Since the          will in turn result in longer fire seasons
          mid-1990s, southeast Australia has           and an ever larger number of days of
          experienced a 15 percent decline in late     extreme fire danger in coming decades
          autumn and early winter rainfall and a       (e.g. Clarke et al. 2011; 2013).

“Bushfires continue to increase in
number, burn for longer and affect
larger areas of land”.
          The concept of a ‘normal’ bushfire           extreme fire weather since the 1970s,
          season is rapidly changing as bushfires      as indicated by changes in the FFDI.
          continue to increase in number, burn         The FFDI increased significantly at
          for longer and affect larger areas of land   16 of 38 weather stations across
          (Bushfire and Natural Hazards CRC            Australia between 1973 and 2010,
          2014a). The influence of hotter, drier       with none of the stations recording a
          weather conditions on the likelihood         significant decrease (Clarke et al. 2013).
          of bushfire spread in Victoria is            These changes have been most marked
          captured by changes in the Forest Fire       in spring, indicating a lengthening fire
          Danger Index (FFDI), an indicator of         season across southern Australia, with
          extreme fire weather. Some regions of        fire weather extending into October
          Australia, especially in the south and       and March. The lengthening fire
          southeast (Victoria, South Australia         season means that opportunities for
          and New South Wales) have already            fuel reduction burning are decreasing
          experienced a significant increase in        (Matthews et al. 2012).

CLIMATECOUNCIL.ORG.AU                                                                          Page 15
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     Victoria is currently experiencing           season in different states. For the first
     persistent rainfall deficiencies, with       time this outlook has been reissued
     severe deficiencies (lowest 5% of records)   (November 2014) due to unseasonably
     emerging in parts of Victoria over the       hot, dry weather in Australia’s southeast
     last 11-months. Below average October        (See Figure 8). Victoria’s 2014–15 bushfire
     rainfall across much of eastern Australia    season outlook has been upgraded
     has also worsened rainfall deficiencies      from an above normal fire season
     over the last four months in northern        to a major fire season. All Victorian
     Victoria (BoM 2014b).                        districts, except the Mallee and East
     The Australia Seasonal Bushfire Outlook      Gippsland, may expect above normal
     for 2014–15, issued in September 2014,       fire potential (Bushfire and Natural
     anticipates the severity of the bushfire     Hazards CRC 2014b).

    Figure 8: The Updated Australia Seasonal Bushfire Outlook (Bushfire and Natural Hazards
    CRC 2014b)

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4. Future projections of
fire activity in southeast
Australia
          Research aimed at understanding future       actual fire activity in southeast and
          fire activity in Australia’s southeast       central Australia (Williams and Karoly
          has a long history (Table 1). While the      1999; Verdon et al. 2004; Lucas 2005;
          detailed results of these studies vary due   Harris et al. 2013). Significant changes
          to the use of different global circulation   have occurred in the nature of ENSO
          models (GCMs) and different emission         since the 1970s, with the phenomenon
          scenarios, their collective conclusion is    being more active and intense during
          clear – weather conditions conducive         the 1979–2009 period than at any other
          to fire in the southeast and southwest of    time in the past 600 years (Aiken et al.
          the continent are becoming increasingly      2013). It is likely that climate change is
          frequent and this trend will continue.       and will continue to influence ENSO
          From the 1980s scientist’s projections       behaviour, although there is currently
          have demonstrated that bushfire              no consensus on the nature, extent
          conditions would be elevated as global       or direction of this influence. Recent
          temperatures increased from rising           projections suggest increases in El
          greenhouse gases.                            Niño-driven drying in the western
          Future changes in the El Niño-Southern       Pacific Ocean by mid-to late 21st century
          Oscillation (ENSO) phenomenon are            (Power et al. 2013); such a change would
          also likely to have an influence on          increase the incidence of heat and
          fire activity. El Niño events worsen         drought, and potentially increase fire
          fire weather conditions and increase         activity in eastern Australia.

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    SUMMARY OF PROJECTIONS FROM MODELLING STUDIES INVESTIGATING CHANGES
    IN FIRE RISK IN SOUTHEAST AUSTRALIA.

     Study                        Projections

     Beer et al. (1988)           10%–20% increase in FFDI in southeast Australia
     Beer and Williams (1995)     Increase in FFDI with doubling of atmospheric CO2, commonly >10%
                                  across most of continent, especially in the southeast, with a few small areas
                                  showing decreases
     Williams et al. (2001)       General trend towards decreasing frequency of low and moderate fire danger
                                  rating days, but an increasing frequency of very high and in some cases
                                  extreme fire danger days
     Hennessy (2007)              Potential increase of very high and extreme FFDI days 4%–25% by 2020,
                                  15%–70% by 2050
     Lucas et al. (2007)          Increases in annual FFDI of up to 30% by 2050 over historical levels in
                                  southeast Australia and up to a trebling in the number of days per year
                                  where the uppermost values of the index are exceeded. The largest changes
                                  projected to occur in the arid and semi-arid interior of NSW and northern
                                  Victoria.
     Hasson et al. (2009)         Analysed likelihood of increase in incidence of synoptic weather pattern
                                  in southeast Australia known to be associated with extreme fire events.
                                  Projected potential frequency of extreme events to increase from around
                                  1 event every 2 years during the late 20th century to around 1 event per year
                                  in the middle of the 21st century, and to around 1 to 2 events per year by the
                                  end of the 21st century
     Clarke et al. (2011)         FFDI projected to decrease or show little change in the tropical northeast.
                                  In the southeast, FFDI projected to increase strongly by end of the 21 st
                                  century, with the fire season extending in length and starting earlier
     Matthews et al. (2012)       Warming and drying climate projected to produce drier, more flammable
                                  fuel, and to increase rate of fire spread
     Jones et al. (2013)          Projected increases in FFDI for Melbourne area

    Table 1: Summary of projections from modelling studies investigating changes in fire risk
    in southeast Australia.

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5. Impacts of Bushfires
in Victoria
          Bushfires have had a very                  (296 deaths) (Haynes et al. 2010). The
          wide range of human and                    Black Saturday bushfires in Victoria in
          environmental impacts, including           February 2009 accounted for 173 deaths,
          loss of life and severe health             ranking as one of the world’s ten most
          effects, damage to property,               deadly recorded bushfires (Teague
          devastation of communities                 et al. 2010). A large proportion of the
          and effects on water and natural           fatalities (44%) were children younger
          ecosystems (Stephenson 2010).              than 12 years old, people over 70 years
                                                     and those with either chronic or acute
                                                     disabilities (O’Neill and Handmer 2012).

5.1 Health Impacts                                   In addition to fatalities, bushfire
                                                     smoke can seriously affect health.
                                                     Smoke contains not only respiratory
“From 1900–2008                                      irritants, but also inflammatory
                                                     and cancer‑causing chemicals
over half of all known                               (Bernstein and Rice 2013). Smoke can
                                                     be transported in the atmosphere

bushfire fatalities in                               for hundreds or even thousands of
                                                     kilometres from the fire front, exposing

Australia occurred                                   large populations to its impacts
                                                     (Spracklen et al. 2009; Dennekamp

in Victoria”.                                        and Abramson 2011; Bernstein and
                                                     Rice 2013). For example in Melbourne,
                                                     cardiac arrests outside hospitals increase
                                                     by almost 50% on bushfire smoke-
          Populations in Victoria are at risk from
                                                     affected days (Dennekamp et al. 2011).
          the health impacts of bushfires, which
                                                     Firefighters are also faced with higher
          have contributed to physical and mental
                                                     risks to their long-term health with an
          illness as well as death.
                                                     elevated chance of developing a variety
          Tragically, in Australia bushfires have    of cancers (Youakim 2006). The impacts
          accounted for more than 800 deaths         of bushfire smoke in the community are
          since 1850 (Cameron et al. 2009; King      also uneven, with the elderly, infants and
          et al. 2013), with more than half of the   those with chronic heart or lung diseases
          deaths (1900–2008) occurring in Victoria   at higher risk (Morgan et al. 2010).

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    In addition to physical health impacts,    major depressive episodes and increased
    the trauma and stress of experiencing a    alcohol use (Bryant et al. 2014). A study
    bushfire can also increase depression,     of over 1500 people who experienced
    anxiety, and other mental health issues,   losses in the 1983 Ash Wednesday
    both in the immediate aftermath of         bushfires found that after 12 months,
    the trauma and for months or years         42% were suffering a decline in mental
    afterwards (McFarlane and Raphael 1984;    health (“psychiatric morbidity”)
    Sim 2002; Whittaker et al. 2012). For      (McFarlane et al. 1997). PTSD, major
    example, a study conducted 3–4 years       depression, anxiety and suicide can also
    after the Black Saturday bushfires in      manifest among firefighters, sometimes
    Victoria found that some members of        only becoming evident many months
    the affected community developed           after an extreme event (McFarlane 1988;
    Post Traumatic Stress Disorder (PTSD),     Cook et al. 2013).

    Figure 9: Bushfire smoke blankets Melbourne in 2006

 Page 20                                                                  CLIMATECOUNCIL.ORG.AU
5.2 Economic Costs
          The economic cost of bushfires –              reaching $378 million (Deloitte Access
          including loss of life, livelihoods,          Economics 2014). These estimates take
          property damage and emergency                 into account increases in the number
          services responses – is very high.            of households, growth in the value
          The total economic cost of bushfires, a       of housing stock, population growth
          measure that includes insured losses as       and increasing infrastructure density.
          well as broader social costs, is estimated    These estimates do not, however,
          to be $337 million per year in Australia      include the potential for climate
          (2011$), a figure that is expected to reach   change to increase bushfire frequency
          $800 million by around 2050 (Deloitte         or intensity, so must be considered
          Access Economics 2014). The total             conservative. Even though Victoria
          economic costs of bushfires in Victoria       comprises only 3% of the country’s
          for 2014 are projected to be $172 million     landmass, it has sustained around
          (2011$). By about mid century these           50% of the economic damage from
          costs will more than double, potentially      bushfires (Buxton et al. 2011).

“Even though Victoria comprises only
3% of the country’s landmass, it has
sustained around 50% of the economic
damage from bushfires”.

CLIMATECOUNCIL.ORG.AU                                                                        Page 21
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    RECORDED LOSSES FROM MAJOR BUSHFIRE EVENTS IN VICTORIA SINCE 1939

     Date     FIRE            Location              LOSSES (including            Deaths               SIGNIFICANT
              EVENT                                 residential property,                             INSURED
                                                    stock)                                            LOSSES
                                                                                                      (normalised to
                                                                                                      2011 values)1
     1939     Black Friday    Widespread across        1000+ homes                       71                    n/a
                              Victoria including;
                                                      (ABS 2004; AIC 2004)          (AIC 2004;
                              Warburton,
                                                                                   Reuters 2009)
                              Erica, Rubicon,
                              Dromana,
                              Manfield, the
                              Otway ranges and
                              the Grampian
                              Ranges.
     1977                     Victoria, Western         >100 homes                       4             $ 101 million
                              Districts
                                                           (CFA 2012)                (CFA 2012)            (ICA 2013)
     1983     Ash             Victoria and            >2,300 homes                      75             $1.796 billion
                              South Australia
              Wednesday       including;
                                                     (Ramsay et al. 1996; AIC       (AIC 2004;             (ICA 2013)
                                                    2004; McAeney et al 2009)      Reuters 2009)
                              Dandenong
                              Ranges east
                              of Melbourne,          >200,000 stock
                              Macedon areas          (Ramsay et al. 1996; AIC
                              northwest of                   2004)
                              Melbourne
     2003     Gippsland       Victoria, North           >41 homes                        0              $24 million
                              East and
              Fires                                                                  (CFA 2012)            (ICA 2013)
                              Gippsland fires       >10,000 livestock
                                                           (CFA 2012)

     2006     Grampians       Victoria,                 > 40 homes                       2              $28 million
                              Grampian ranges
              Fires                                                                  (CFA 2012)            (ICA 2013)
                                                      >65,000 stock
                                                           (CFA 2012)
     2009     Black           Churchill, Kilmore      >2000 houses                      173                $ 1.266
              Saturday
                              and Murrundindi,
                                                    (CFA 2012; Stephenson et       (Teague et al.          billion
                              Vectis (Horsham),
                                                            al. 2013)            2010; Stephenson          (ICA 2013)
                              Coleraine, Weerite,
                                                                                     et al 2013)
                              Redesdale,
                              Harkaway, Upper          8000–11,800
                              Ferntree Gully,             stock
                              Maiden Gully             (Teague et al 2010;
                              / Eaglehawk,           Stephenson et al. 2013)
                              Lynbrook /
                              Narre Warren,
                              Beechworth

    Table 2: Recorded losses from major             1. I nsured losses shown have been normalized to 2011 values
    bushfire events in Victoria since 1939.            (taking inflation and wealth changes into account).

 Page 22                                                                              CLIMATECOUNCIL.ORG.AU
Bushfires can cause direct damage           A study by Keating and Handmer
          to properties; for example, the Black       (2013) provides one of the few full
          Saturday bushfires destroyed over 2000      economic assessments of bushfire
          homes (see Table 2). Infrastructure         impacts on primary industry. This
          such as powerlines and roads can            study conservatively estimated that
          also be damaged. In the 2003 alpine         bushfires directly cost the Victorian
          fires in Victoria, for example, about       agricultural industry around $42 million
          4,500 km of roads were damaged and          per year. When business disruption
          local businesses reported a 50–100%         was included more broadly, the costs
          economic downturn in the fire               to the entire Victorian economy
          aftermath (Stephenson 2010).                from this impact were estimated to
          Bushfires have significant impacts in       be $92 million per year. A similar
          farming areas. For example, livestock       analysis for the Victorian timber
          losses were estimated at 13,000 in the      industry estimated direct costs at
          2003 Alpine fires in Victoria, 65,000 in    $74 million per year, and state-wide
          the 2005–6 Grampians fire and more          costs at $185 million (Keating and
          than 11,000 in the Black Saturday fires     Handmer 2013). In the future, with no
          (Stephenson 2010; Teague et al. 2010).      adaptive change, increased damage
          Stock that survives the initial bushfires   to the agricultural industry in Victoria
          can face starvation in the post-fire        by 2050 could add $1.4 billion (or
          period, as well as threats from predators   $46.6 million per year) to the existing
          due to the destruction of fences around     costs of $92 million per year (Keating
          properties (Stephenson 2010). Over          and Handmer 2013). Similarly, the
          8,000 km of fences were lost in the Black   additional cost of bushfires to the
          Saturday fires (Stephenson 2010). Smoke     Victorian timber industry is estimated
          damage can also taint fruit and vegetable   to be $2.85 billion ($96.2 million per year),
          crops, with wine grapes particularly        over and above the present day estimate
          susceptible (Stephenson 2010).              of $185 million per year.

“Bushfires directly cost the Victorian
agricultural industry around $42 million
per year”.

CLIMATECOUNCIL.ORG.AU                                                                         Page 23
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VICTORIAN BUSHFIRE THREAT

    It is important to note that these          costs for volunteer fire fighters,
    economic losses do not account for          fixed costs for bushfire fighting
    the full range of costs associated with     services, government contributions
    bushfires – few attempts have been          for rebuilding and compensation,
    made to account for loss of life, social    impacts on health, and ecosystem
    disruption and trauma, opportunity          services (King et al. 2013).

    Figure 10: A firefighter observes the wreckage of a home in Kinglake, Victoria

 Page 24                                                                    CLIMATECOUNCIL.ORG.AU
5.3 Environmental Impacts
          Fire can affect the quality and quantity of water in catchments and have
          significant impacts on ecosystems.

                                                        usually uses more water than the mature
          5.3.1 IMPACT ON WATER
          QUALITY AND QUANTITY                          trees they have replaced (Langford 1976,
                                                        Feikema et al. 2013). Seven years after
          Large-scale high intensity fires that
                                                        the 2003 fires in the mountain ash
          remove vegetation expose topsoils
                                                        forests of Victoria, the regrowth was still
          to erosion and increased runoff after
                                                        using twice the water of adjacent mature
          subsequent rainfall (Shakesby et al.
                                                        forest (Buckley et al. 2012). This pattern,
          2007). This can increase sediment
                                                        known as the “Kuczera effect”, can last
          and nutrient concentrations in nearby
                                                        for several decades after a fire, with water
          waterways, potentially making water
          supplies unfit for human consumption          yields from forested catchments being
          (Smith et al. 2011; IPCC 2014). During the    reduced by up to 50% (Kuczera 1985;
          Black Saturday fires 10 billion litres of     Brookhouse et al. 2013). Fires can also
          Melbourne’s drinking water was pumped         affect water infrastructure; the Black
          to safer storage locations because of fears   Saturday bushfires in 2009 affected
          it would be contaminated (Johnston            about 30% of the catchments that
          2009). Fire also has longer-term affects      supply Melbourne’s drinking water.
          on water flow in forested catchments.         Melbourne Water estimated the
          Immediately after the fire there may          post‑fire recovery costs, including
          be an increase in water flow. But as          water‑monitoring programs, to be
          the forests regenerate, the new growth        over $2 billion (WRF 2013).

CLIMATECOUNCIL.ORG.AU                                                                           Page 25
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    Figure 11: Bushfire smoke at the Upper Yarra Dam, Victoria.

                                                 and disadvantage others. If fires are
    5.3.2 IMPACTS ON ECOSYSTEMS
                                                 too frequent, plant species can become
    Fire is a regular occurrence in many
                                                 vulnerable to local extinction as the
    Australian ecosystems, and many
                                                 supply of seeds in the soil declines.
    species have evolved strategies over
                                                 Conversely, if the interval between fires
    millions of years to not only withstand
                                                 is too long, plant species that rely on fire
    fire, but to benefit from it (Crisp et al.
                                                 for reproduction may be eliminated from
    2011; Bowman et al. 2012). Fire does not
    “destroy” bushland, as is often reported;    an ecological community. Animals are
    rather, it acts as a major disturbance       also affected by bushfires, for example
    with a range of complex impacts on           if they are restricted to localised habitats
    different species and communities.           and cannot move quickly, and/or
    Particular fire regimes (especially          reproduce slowly, they may be at risk
    specific combinations of fire frequency      from intense large-scale fires that occur
    and intensity) can favour some species       at short intervals (Yates et al. 2008).

 Page 26                                                                      CLIMATECOUNCIL.ORG.AU
Ecosystems in which the natural fire        et al. 2011; Bowman et al. 2013). This
              interval is very long (>100 years) can      change in vegetation has important
              undergo substantial change if the fire      flow-on effects for other species,
              frequency increases. After successive       especially the ~40 vertebrate species that
              fires in 2003 and 2006–7 in Victoria,       rely on the hollows of 120–150 year old
              Acacia shrublands have replaced             mountain ash trees for habitat, such as
              some mountain and alpine ash forests        the endangered Leadbeater’s possum;
              because there was insufficient time         an estimated 42% of the possum’s
              between fires for the ash trees to become   habitat was burned in the 2009 bushfires
              reproductively mature (Lindenmayer          (Lindenmayer 2013) (Figure 12).

Figure 12: The Black Saturday 2009 bushfires affected much of the habitat of the already
endangered Leadbeater’s possum.

CLIMATECOUNCIL.ORG.AU                                                                            Page 27
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VICTORIAN BUSHFIRE THREAT

    6. Implications of
    increasing fire activity
    “Melbourne’s rural-urban fringe is among
    the most vulnerable in the world to the
    bushfire hazard”.
    The risk that bushfires pose to people are   The increasing population and built
    particularly acute in southern Australia,    assets, coupled with increasing fire
    where large populations live close to        danger weather, present significant
    highly flammable native vegetation           and growing challenges for the state.
    that is exposed to frequent severe fire      Already fire prone regions are becoming
    weather. The population of Victoria          more fire prone and risks to lives and
    could potentially grow to 10 million         property continue to increase in parts
    by 2051, with 2.2 million in Victoria’s      of Victoria. Hard decisions will have to
    regions and 7.8 million in Greater           be made about the on-going livability
    Melbourne (Victorian Government              of those regions, as they become
    2014). Melbourne’s rural-urban fringe        increasingly dangerous to live in.
    is among the most vulnerable in the
    world to the bushfire hazard (Buxton et      The economic, social and environmental
    al. 2011). The population of Melbourne       costs of increasing bushfire activity
    is continuing to spread, encroaching         in Victoria are potentially immense.
    into surrounding bushland, increasing        As noted in Section 5.2, an analyses
    risk to life and property from bushfires.    of projected costs of bushfires in
    For example, many of the homes               Victoria by Deloitte Access Economics
    destroyed in Marysville and Kingslake,       (2014) forecast that bushfires in Victoria
    two communities devastated by the            could cost $378 million by about
    2009 Victorian bushfires, were either        mid‑century (2011$), based only on
    surrounded by or located less than           population and asset increases, but
    10 metres from bushland (Chen and            not including increased risk due to
    McAneney 2010; Crompton et al. 2010).        climate change.

 Page 28                                                                     CLIMATECOUNCIL.ORG.AU
“The economic, social and environmental
costs of increasing bushfire activity in
Victoria are potentially immense”.
          There is increasing interest in               Adams 2013; Altangerel and Kull 2013). In
          how adaptation to an increasingly             the wake of the Black Saturday bushfires,
          bushfire‑prone world may reduce               the Royal Commission recommended
          vulnerability. Current initiatives centre     treating at least 5% of Victorian
          on planning and regulations, building         public land per year (and up to 8%) by
          designs to reduce flammability, burying       prescribed burning (Teague et al. 2010).
          powerlines in high risk areas, retrofitting   The “5% solution” is being imported
          electricity systems, fuel management,         to some other states, even though fire
          fire detection and suppression, improved      ecologists stress that the frequency and
          early warning systems, and community          amount of prescribed burning required
          education (Preston et al. 2009; Buxton        to reduce risk varies greatly between
          et al. 2011; O’Neill and Handmer 2012;        different landscapes (Penman et al.
          King et al. 2013). Responses to bushfires     2011; Williams and Bowman 2012). The
          can be controversial, particularly the        Tasmania Bushfire Inquiry noted that a
          practice of prescribed burning, where         strategic approach to prescribed burning
          fires are lit in cool weather to reduce       was “preferable to a quantitative target”
          the volume of fuel. Fire managers are         (TBI 2013). The prospect of increasing
          constantly faced with the challenge of        fire risk as the climate warms brings
          balancing the need to reduce risk to          the prescribed burning issue into even
          life and property whilst simultaneously       sharper focus. The increasing length of
          conserving biodiversity and                   the fire season will reduce the window
          environmental amenity, and controlling        of opportunity for hazard reduction at
          air pollution near urban areas (Penman        the same time as the need for hazard
          et al. 2011; Williams and Bowman 2012;        reduction becomes greater.

CLIMATECOUNCIL.ORG.AU                                                                        Page 29
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VICTORIAN BUSHFIRE THREAT

    “Australia’s fire and emergency
    services agencies have recognised
    the implications of climate change for
    bushfire risk and fire-fighting resources
    for some time”.
    Australia’s fire and emergency              increase in the number of both
    services agencies have recognised           professional and volunteer firefighters
    the implications of climate change for      will be needed. To keep pace with
    bushfire risk and fire-fighting resources   asset growth and population, it has
    for some time (AFAC 2009; 2010).            been estimated that the number of
    Longer fire seasons have implications       professional firefighters in Victoria
    for the availability and costs of fire-     will need to increase from approximately
    fighting equipment that is leased from      2,400 in 2010 to 3,000 by 2020 and
    fire fighting agencies in the Northern      3,700 by 2030. When the increased
    Hemisphere. As fire seasons in the two      incidence of extreme fire weather
    hemispheres increasingly overlap, such      under a realistic warming scenario is
    arrangements may become increasingly        also taken into account, a further 500
    impractical (Handmer et al. 2012).          firefighters will be needed by 2020, and
    Substantially increased resources for       900 by 2030 – this represents an overall
    fire suppression and control will be        doubling of numbers compared to 2010
    required. Most importantly, a significant   (NIEIR 2013).

 Page 30                                                                   CLIMATECOUNCIL.ORG.AU
“In Victoria the number of professional
firefighters will need to double by 2030,
to keep pace with increased population,
asset growth, and fire risk from
climate change”.

Figure 13: The Victorian Country Fire Authority on patrol

CLIMATECOUNCIL.ORG.AU                                       Page 31
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VICTORIAN BUSHFIRE THREAT

    7. This is the Critical
    Decade
    The impacts of climate change are            impacts as the temperature rises. For
    already being observed. Sea levels           Victoria, these impacts include increased
    are rising, oceans are becoming              fire danger weather and longer bushfire
    more acidic, and heatwaves                   seasons. Ensuring that this guardrail is
    have become longer and hotter.               not exceeded will prevent even worse
    Greenhouse gases from human                  impacts from occurring.
    activities, particularly the burning         The evidence is clear and compelling.
    of fossil fuels, is the primary cause        The trend of increasing global emissions
    for the changes in climate over the          must be halted within the next few
    past half-century (IPCC 2013; 2014).         years and emissions must be trending
                                                 downwards by 2020. Investment in
    Projections of future climate change
                                                 renewable, clean energy must therefore
    and its impacts have convinced nations
                                                 increase rapidly. And, critically, most
    that the global average temperature, now
                                                 of the known fossil fuel reserves must
    at 0.9°C above the pre-industrial level,
                                                 remain in the ground.
    must not be allowed to rise beyond 2°C
    – the so-called ‘2°C guardrail’. Societies   This is the critical decade to get on
    will have to adapt to even more serious      with the job.

 Page 32                                                                      CLIMATECOUNCIL.ORG.AU
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