Comparison of Current and Future Boreal Fire Regimes in Canada and Russia

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Comparison of Current and Future Boreal Fire Regimes in Canada and Russia WJ de Groot MD Flannigan BJ Stocks DR Cahoon AJ Soja E Kukavskaya G Ivanova AS Cantin N Jurko SG Conard 1

Outline General fuel, weather and fire statistics Comparison of North American and Eurasian boreal forest fire regimes Future trends in boreal fire regimes under climate change

General Fire Regime Characteristics Canada Russia Area burned (M ha/yr) 0.3-7.5 12-20 Crown Fire 97% 20% Fire intensity High Lo-Mod

Forest Composition Thuja & other conifers 4% Abies sp. 6% Unclassified 6% Pinus sp. 9% Tree Proportions in Canada by Area Tsuga sp. Other hardwoods 2% 2% Betula sp. 4% Fir Pine Acer sp. 2% Aspen Populus sp. 11% Larix sp. 1% Pseudotsuga menziesii 1% Spruce Canada Picea sp. 52% Abies sp. 4% Picea sp. 15% Populus tremula 5% Betula sp. 13% Tree Proportions in Russia by Volume Quercus sp. 1% Birch Fir Spruce Other trees 1% Bushes 2% Pine Larch Larix sp. 31% Russia Pinus sibirica 9% Pinus sylvestris 19%

Historical Fire Weather

Canadian Fuels Data C1 Spruce-lichen woodland C2 Boreal spruce C3 Immature jack/lodgepole pine C4 Mature jack/lodgepole pine C5 Red and white pine C6 Pine plantation C7 Ponderosa pine-douglas fir D1 Deciduous (leafless) M1/M2 Boreal mixedwood O1 Grass

Russian Fuels Data Fuel Types: Larix Pinus sylvestris Pinus sibirica Betula Picea Abies Populus tremula

Modelled Fire Behaviour and Effects Using the Canadian Fire Effects Model (CanFIRE), simulated every large fire: satellite determined fire perimeters simulated each fire as a one-day fire event interpolated fire weather using the date with most MODIS hotspots using standard fuel types/loads (e.g., mature stand, average biomass data) Calculated: Head fire intensity Type of fire (surface, crown) Fuel consumption and carbon emissions

Large (>200 ha) Fire Occurrence 9

Mean Fire Return Interval 10

Mean Fire Return Interval 11

Average National Fire Statistics (Canada 2001-2010; Russia 2001-2007) Canada Russia Number of large fires per year 295 10,923 Large Fire Frequency (#/yr/100m ha forest) 64 1732 Total area burned (M ha) 1.6 12.4 Area Burned (M ha/yr/100m ha forest) 0.34 1.96 Large Fire Size (ha) 5342 1132 Fire Freq. (MFRI, yrs) 294 51

Average National Fire Statistics (Canada 2001-2010; Russia 2001-2007) Canada Russia Crowning Fires (%) 54.7 1.2 Fire Intensity (kw/m) 7042 1996 Carbon emission rate (t/ha) 27.1 11.1 Total carbon emissions (Mt/yr) 43 138

Average National Fire Statistics (Canada 2001-2010; Russia 2001-2007) Canada Russia Crowning Fires (%) 54.7 1.2 Fire Intensity (kw/m) 7042 1996 Carbon emission rate (t/ha) 27.1 11.1 Total carbon emissions (Mt/yr) 43 138

Boreal Fire Regimes Russia is characterised by very many large surface fires of low-moderate intensity Canada is characterised by a small number of very large crown fires having very high intensity Why? Forest composition (genus) Tree morphology and fire ecology (species) Human-caused fire?

Boreal Fire Regimes Forest Composition Crown-fire promoting: Picea Abies Pinus Carbon Emissions Non-crowning: Larix Betula Populus

Forest Composition Thuja & other conifers 4% Abies sp. 6% Unclassified 6% Pinus sp. 9% Tree Proportions in Canada by Area Tsuga sp. Other hardwoods 2% 2% Betula sp. 4% Fir Pine Acer sp. 2% Aspen Populus sp. 11% Larix sp. 1% Pseudotsuga menziesii 1% Spruce Canada Picea sp. 52% Abies sp. 4% Picea sp. 15% Populus tremula 5% Betula sp. 13% Tree Proportions in Russia by Volume Quercus sp. 1% Birch Fir Spruce Other trees 1% Bushes 2% Pine Larch Larix sp. 31% Russia Pinus sibirica 9% Pinus sylvestris 19%

Boreal Fire Regimes Tree morphology and fire ecology Carbon Emissions Pinus banksiana Pinus sylvestris

Future Change in Fire Weather Severity Cumulative Severity Rating (CSR) for 2091-2100 using HadCM3 and A2

Future Change in Fire Danger Severity Results and implications: Fire weather severity increased in both countries for all GCM and CC scenarios Head fire intensity and daily severity rating (indicators of fire control difficulty) substantially increased in both countries; Peak extreme HFI and DSR values in mid-summer in both countries, but Russia also had a secondary peak in late spring/early summer Generally, Canada will experience greater increases than Russia, resulting in more crown fire and increased C emissions Increases in HFI and DSR are so great (up to 3X current) that it could push current suppression capacity beyond a tipping point, resulting in many more larger fires Note: Effects of increased numbers of fires, area burned, and changing fuel type were not studied

References de Groot, Cantin, Flannigan, Soja, Gowman, Newbery. 2013. A comparison of Canadian and Russian boreal forest fire regimes. For. Ecol. Manage. 294: 23-34. de Groot, Flannigan, Cantin. 2013. Climate change impacts on future boreal fire regimes. For. Ecol. Manage. 294: 35-44. Flannigan, Cantin, de Groot, Wotton, Newbery, Gowman. 2013. Global wildland fire season severity in the 21 st century. For. Ecol. Manage. 294: 54-61.

IUFRO XXIV World Congress 5-11 Oct 2014, Salt Lake City, Utah Session 138: Forests, fire and climate change dynamics Presentations in this session will focus on the latest scientific understanding of climate change and future global fire regimes, feedback to the global carbon balance, expected human and environmental impacts, and potential management strategies to mitigate negative impacts. 22 VI ICFFR Coimbra, Portugal 15-18 November 2010