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QUANTIFYING THE FLAMMABILITY
OF FIRE-SENSITIVE RAINFORESTS
Ross Peacock
› How flammable are rainforests
compared to Eucalyptus forests
› What are their fuel characteristics
› Is the fuel micro-climate different
› Is climate change relevant
› How will fires behave in rainforests
› How will species respond after fire
› Can we improve our predictive
capabilities and risk planning using
this information
Study objectives
Ecotone forests are utilised by a range of
threatened fauna – Tiger Quoll.
The Nothofagus rainforest estate
Is the climate changing?
500
1000
1500
2000
2500
3000
3500
1962
1963
1964
1965
1966
1967
2009
2010
2011
2012
2013
2014
2015
2016
rainfall (mm/year)
litterfall (kg/ha/year)
Rainforest litter inputs are
correlated with annual
rainfall
Rainforest fires in northern NSW
Hazard reduction burn wet sclerophyll – rainforest
interface northern NSW. Photograph Dale McLean
› Frequency of 1-2 per century per
stand;
› Significant wildfires burnt
rainforest in 1915, 1918, 1956,
1968, 1996, 2012 and 2013
› Conglomerate Coffs Harbour
wildfire of 1968 ‘Even rainforests
were burning’ (Humphreys 2012)
› Do we need to be become more
proactive in managing risk?
Macleay River wildfire Oct 2012
burnt significant area of dry rainforest
in Oxley Wild Rivers NP
Are the north coast wildfire seasons changing?
0
100
200
300
400
500
600
700
800
Total number of fires per month
1951 - 1961 (n=2905)
2002 - 2016 (n=2911)
0
5
10
15
20
25
30
35
40
45
50
% of region burnt per month
1951 - 1961
2002 - 2016
150012009006003000
18
16
14
12
10
8
6
4
2
0
g/m2/month
Percent
75604530150
40
30
20
10
0
diameter of largest piece (mm)
Percent
2.52.01.51.00.50.0-0.5
30
25
20
15
10
5
0
diameter (m)
Percent
Fine fuels input 498 kg/yr-1/ha-1 Coarse fuels input 590 kg/yr-
1/ha-1
CWD mass 407 t/ha-1
Fuel characteristics
Fuel fraction Rainforest Eucalyptus
forest
Fine fuel input (< 6mm) kg/yr-1/ha-1 498 3010
Coarse fuel input (>6 mm) kg/yr-1/ha-1 590 470
Coarse woody fuels mean diameter (m) 0.54 0.31
Coarse woody fuels mean volume (t/ha-1) 207 403
Total fine fuel mass < 6 mm (t/ha-1) 9-11 16-23
RainforestEucalyptus forest
Profile fuel characteristics differ in density and moisture
Profile fuel characteristics differ in depth and mass
Rainforest Eucalyptus forest
Fine fuel mass varies across vegetation boundaries
Fuel type Profile mass
(g/m-2)
Rainforest 982
Ecotone 1125
Eucalyptus forest 1363
Fuel decay stage is important
R² = 0.9402
0
10
20
30
40
50
60
70
80
90
100
0 100 200 300 400
%ofinitialmasscombustedafterignition
days of litter burial
Fuel decay proportions differed
None of the forest type
comparisons were
significantly different
(p>0.05)
Fuel decay impacts a range of flammability metrics
Fine fuel inputs in rainforest are strongly seasonalJanuaryFebruary
M
arch
April
M
ay
June
July
AugustSeptem
ber
O
ctoberN
ovem
berD
ecem
ber
litterfallkg/ha-1
/month-1
0
20
40
60
80
100
120
› Spring is the peak season for
litter fall
› Spring is the peak season for
wildfire ignitions
› In spring fuels are generally at
their lowest seasonal fuel
moisture content
› In spring ambient humidity is
low.
Fine and coarse rainforest fuel inputs increase in wetter
years
350030002500200015001000
2800
2600
2400
2200
2000
1800
1600
1400
1200
rainfall (mm/year)
litterfall(kg/ha/year)
Fine fuels < 6mm
R² = 0.9779
0
100
200
300
400
500
600
700
800
900
1000 1500 2000 2500 3000
kg/ha-1/yr-1
sampling period annual rainfall (mm)
Coarse fuels > 6mm
Landscape scale relationship of rainfall and fine fuel
biomass
mean annual rainfall (mm)
1100 1200 1300 1400 1500 1600 1700 1800
littermassg/m2
500
1000
1500
2000
2500
3000
mean annual rainfall (mm)
1600 1800 2000 2200 2400 2600
littermassg/m2
400
600
800
1000
1200
1400
1600
1800
WSF Shrubby forests Cool Temperate Rainforests
Are instantaneous fuel moisture conditions different?
0
20
40
60
80
100
120
140
160
180
200
rainforest
0
20
40
60
80
100
120
140
160
180
200
Eucalyptus forest
Is fuel moisture correlated with ambient conditions
Eucalyptus forest RainforestEcotone
Rainforest understoreys are more sensitive to
variation in relative humidity compared to Eucalyptus
0
10
20
30
40
50
60
70
80
90
100 0:00
1:30
3:00
4:30
6:00
7:30
9:00
10:30
12:00
13:30
15:00
16:30
18:00
19:30
21:00
22:30
0:00
relativehumidity(%)
litter layer
1.5 m
0
10
20
30
40
50
60
70
80
90
100
0:00
1:30
3:00
4:30
6:00
7:30
9:00
10:30
12:00
13:30
15:00
16:30
18:00
19:30
21:00
22:30
0:00
litter layer
1.5 m
Eucalyptus forestRainforest
Rainforest fuels are slower to
ignite, release less heat and burn
more slowly
Heat output is greater from Eucalyptus forest fuels
0
100
200
300
400
500
600
700
800
Eucalyptus forest Rainforest
maximumtemperature0C
Litter bed combustion experiment
Fine fuels drive the rate of spread
Wind 1.5m/s
Temp 250 C
RH 30%
FMC 8%
0
200
400
600
800
1000
0.0 1.0 2.0 3.0 4.0
time(sec) distance of flame front spread (m)
Rainforest
Eucalyptus
Ecotone
Rainforest hazard reduction burn
Low intensity
burn applied
to rainforest
experimental
area
Large tree size class most likely to ignite
Large tree size class most
likely to ignite and fall
tree DBH (cm)
10-19.9 20-29.9 30-39.9 40-49.9 50-59.9 60-69.9 70-79.9 80-89.9 90 +
proportionoftreesburnt
-0.2
0.0
0.2
0.4
0.6
0.8
1.0
Changes in fine fuel
biomass following HRB,
wildfire and canopy
scorch
WSF Shrubby forests
Cool Temperate Rainforests
Brushy Mountain Complex wildfire November 2013
Wildfires burning rainforest follow antecedent soil drying
13,000 ha burnt
Photograph (right) Andrew Marshall
Rainforests can
form natural
containment
lines however
patches will
contract
Photograph Andrew Marshall
Rainforest
was only
vegetation
type not
to
propagate
the
ground
and crown
wildfire
Photographs
Andrew Marshall
Outcomes
› How flammable are rainforests compared
to Eucalyptus forests
› What are rainforest fuel characteristics
› Is climate change relevant
› Is the fuel micro-climate different
› How will fires behave in rainforests
› How will species respond after fire
› Can we improve our predictive capabilities
and risk planning using this information
› Lower ROS, heat output, ignitability, mass loss
etc
› Less mass, depth, elevated fuels, increased
FMC and bulk density
› Wildfire seasons are earlier than 50 years
ago, rainforest fuel mass increases in wet and
cool years and is at seasonal max. in spring.
› Rainforest fuels less sensitive to diurnal RH
variation than Eucalyptus forests. Importance
of antecedent soil drying.
› Rainforests are anti-flammable. Large tree
mortality and dieback, understorey re-
sprouting
› Yes if we strategically address risks to
environmental assets through BFRMP’s
Outreach outcomes
› A sustainable model for citizen science
volunteering in fuel and climate
monitoring has been established
Acknowledgements
All photographic credits Ross Peacock unless
annotated otherwise

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BushfireConf2017 – 11. Quantifying the flammability of fire-sensitive rainforest habitats.

  • 1. QUANTIFYING THE FLAMMABILITY OF FIRE-SENSITIVE RAINFORESTS Ross Peacock
  • 2. › How flammable are rainforests compared to Eucalyptus forests › What are their fuel characteristics › Is the fuel micro-climate different › Is climate change relevant › How will fires behave in rainforests › How will species respond after fire › Can we improve our predictive capabilities and risk planning using this information Study objectives Ecotone forests are utilised by a range of threatened fauna – Tiger Quoll.
  • 4. Is the climate changing? 500 1000 1500 2000 2500 3000 3500 1962 1963 1964 1965 1966 1967 2009 2010 2011 2012 2013 2014 2015 2016 rainfall (mm/year) litterfall (kg/ha/year) Rainforest litter inputs are correlated with annual rainfall
  • 5. Rainforest fires in northern NSW Hazard reduction burn wet sclerophyll – rainforest interface northern NSW. Photograph Dale McLean › Frequency of 1-2 per century per stand; › Significant wildfires burnt rainforest in 1915, 1918, 1956, 1968, 1996, 2012 and 2013 › Conglomerate Coffs Harbour wildfire of 1968 ‘Even rainforests were burning’ (Humphreys 2012) › Do we need to be become more proactive in managing risk?
  • 6. Macleay River wildfire Oct 2012 burnt significant area of dry rainforest in Oxley Wild Rivers NP
  • 7. Are the north coast wildfire seasons changing? 0 100 200 300 400 500 600 700 800 Total number of fires per month 1951 - 1961 (n=2905) 2002 - 2016 (n=2911) 0 5 10 15 20 25 30 35 40 45 50 % of region burnt per month 1951 - 1961 2002 - 2016
  • 8. 150012009006003000 18 16 14 12 10 8 6 4 2 0 g/m2/month Percent 75604530150 40 30 20 10 0 diameter of largest piece (mm) Percent 2.52.01.51.00.50.0-0.5 30 25 20 15 10 5 0 diameter (m) Percent Fine fuels input 498 kg/yr-1/ha-1 Coarse fuels input 590 kg/yr- 1/ha-1 CWD mass 407 t/ha-1
  • 9. Fuel characteristics Fuel fraction Rainforest Eucalyptus forest Fine fuel input (< 6mm) kg/yr-1/ha-1 498 3010 Coarse fuel input (>6 mm) kg/yr-1/ha-1 590 470 Coarse woody fuels mean diameter (m) 0.54 0.31 Coarse woody fuels mean volume (t/ha-1) 207 403 Total fine fuel mass < 6 mm (t/ha-1) 9-11 16-23
  • 10. RainforestEucalyptus forest Profile fuel characteristics differ in density and moisture
  • 11. Profile fuel characteristics differ in depth and mass Rainforest Eucalyptus forest
  • 12. Fine fuel mass varies across vegetation boundaries Fuel type Profile mass (g/m-2) Rainforest 982 Ecotone 1125 Eucalyptus forest 1363
  • 13. Fuel decay stage is important R² = 0.9402 0 10 20 30 40 50 60 70 80 90 100 0 100 200 300 400 %ofinitialmasscombustedafterignition days of litter burial
  • 14. Fuel decay proportions differed None of the forest type comparisons were significantly different (p>0.05)
  • 15. Fuel decay impacts a range of flammability metrics
  • 16. Fine fuel inputs in rainforest are strongly seasonalJanuaryFebruary M arch April M ay June July AugustSeptem ber O ctoberN ovem berD ecem ber litterfallkg/ha-1 /month-1 0 20 40 60 80 100 120 › Spring is the peak season for litter fall › Spring is the peak season for wildfire ignitions › In spring fuels are generally at their lowest seasonal fuel moisture content › In spring ambient humidity is low.
  • 17. Fine and coarse rainforest fuel inputs increase in wetter years 350030002500200015001000 2800 2600 2400 2200 2000 1800 1600 1400 1200 rainfall (mm/year) litterfall(kg/ha/year) Fine fuels < 6mm R² = 0.9779 0 100 200 300 400 500 600 700 800 900 1000 1500 2000 2500 3000 kg/ha-1/yr-1 sampling period annual rainfall (mm) Coarse fuels > 6mm
  • 18. Landscape scale relationship of rainfall and fine fuel biomass mean annual rainfall (mm) 1100 1200 1300 1400 1500 1600 1700 1800 littermassg/m2 500 1000 1500 2000 2500 3000 mean annual rainfall (mm) 1600 1800 2000 2200 2400 2600 littermassg/m2 400 600 800 1000 1200 1400 1600 1800 WSF Shrubby forests Cool Temperate Rainforests
  • 19. Are instantaneous fuel moisture conditions different? 0 20 40 60 80 100 120 140 160 180 200 rainforest 0 20 40 60 80 100 120 140 160 180 200 Eucalyptus forest
  • 20. Is fuel moisture correlated with ambient conditions Eucalyptus forest RainforestEcotone
  • 21. Rainforest understoreys are more sensitive to variation in relative humidity compared to Eucalyptus 0 10 20 30 40 50 60 70 80 90 100 0:00 1:30 3:00 4:30 6:00 7:30 9:00 10:30 12:00 13:30 15:00 16:30 18:00 19:30 21:00 22:30 0:00 relativehumidity(%) litter layer 1.5 m 0 10 20 30 40 50 60 70 80 90 100 0:00 1:30 3:00 4:30 6:00 7:30 9:00 10:30 12:00 13:30 15:00 16:30 18:00 19:30 21:00 22:30 0:00 litter layer 1.5 m Eucalyptus forestRainforest
  • 22. Rainforest fuels are slower to ignite, release less heat and burn more slowly
  • 23. Heat output is greater from Eucalyptus forest fuels 0 100 200 300 400 500 600 700 800 Eucalyptus forest Rainforest maximumtemperature0C
  • 24. Litter bed combustion experiment
  • 25. Fine fuels drive the rate of spread Wind 1.5m/s Temp 250 C RH 30% FMC 8% 0 200 400 600 800 1000 0.0 1.0 2.0 3.0 4.0 time(sec) distance of flame front spread (m) Rainforest Eucalyptus Ecotone
  • 27. Low intensity burn applied to rainforest experimental area
  • 28. Large tree size class most likely to ignite
  • 29. Large tree size class most likely to ignite and fall tree DBH (cm) 10-19.9 20-29.9 30-39.9 40-49.9 50-59.9 60-69.9 70-79.9 80-89.9 90 + proportionoftreesburnt -0.2 0.0 0.2 0.4 0.6 0.8 1.0
  • 30. Changes in fine fuel biomass following HRB, wildfire and canopy scorch WSF Shrubby forests Cool Temperate Rainforests
  • 31. Brushy Mountain Complex wildfire November 2013
  • 32. Wildfires burning rainforest follow antecedent soil drying
  • 33. 13,000 ha burnt Photograph (right) Andrew Marshall
  • 34. Rainforests can form natural containment lines however patches will contract Photograph Andrew Marshall
  • 35. Rainforest was only vegetation type not to propagate the ground and crown wildfire Photographs Andrew Marshall
  • 36. Outcomes › How flammable are rainforests compared to Eucalyptus forests › What are rainforest fuel characteristics › Is climate change relevant › Is the fuel micro-climate different › How will fires behave in rainforests › How will species respond after fire › Can we improve our predictive capabilities and risk planning using this information › Lower ROS, heat output, ignitability, mass loss etc › Less mass, depth, elevated fuels, increased FMC and bulk density › Wildfire seasons are earlier than 50 years ago, rainforest fuel mass increases in wet and cool years and is at seasonal max. in spring. › Rainforest fuels less sensitive to diurnal RH variation than Eucalyptus forests. Importance of antecedent soil drying. › Rainforests are anti-flammable. Large tree mortality and dieback, understorey re- sprouting › Yes if we strategically address risks to environmental assets through BFRMP’s
  • 37. Outreach outcomes › A sustainable model for citizen science volunteering in fuel and climate monitoring has been established
  • 38. Acknowledgements All photographic credits Ross Peacock unless annotated otherwise