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GLOBAL CHANGE EFFECTS ON FIRE AND FUEL MANAGEMENT IN NORTHERN FORESTS. Brian Amiro, Brian Stocks, Marty Alexander, Mike Flannigan, and Mike Wotton Canadian Forest Service. Outline. The recent past: fire history The present fire occurrence magnitude of boreal fires
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GLOBAL CHANGE EFFECTS ON FIRE AND FUEL MANAGEMENT IN NORTHERN FORESTS Brian Amiro, Brian Stocks, Marty Alexander, Mike Flannigan, and Mike Wotton Canadian Forest Service
Outline • The recent past: fire history • The present • fire occurrence • magnitude of boreal fires • Fuel management at the landscape scale • The future • global change • the carbon issue
Circumpolar Boreal Forest • Huge size • Fire dominated (short fire cycle) • Crown fires common • Relatively sparse settlement Ecologically, this forest needs fire!
Fire History: • 1 to 3 million ha burned annually • ~8,000 fires annually • large variability • general trend upwards • uncertainty in older data • direct suppression costs ~$0.5 billion
Large-Fire Database fires > 200 ha 1980 - 1994
Lichen woodland Coniferous Deciduous Mixed Wood Grassland/Agriculture Non-fuel Water FUEL TYPES
Fires are most common in “coniferous” fuel types in the boreal forest Fires 1980-94 Fuel Types An increasing deciduous component reduces the rate of spread and resists crowning
~ 400 x 400 km • Coniferous fuels • - Jack pine • - Black spruce • Small deciduous • component Example Area: Boreal Shield Saskatchewan 1980-1994
1988-91, 1980-82, 1983-87, 1992-94, 1995 Fuel Types lakes deciduous coniferous Scale: about 400 x 400 km
Fuel Management at the Landscape/National Scale • Assume that localized fuel management can protect valued areas (e.g., communities) • But: Can proactive fuel management decrease area burned in northern forests? • Basic Options • fuel reduction (mechanical, burning) • fuel conversion (deciduous) • fuel isolation (mechanical, burning, tie into strategic fuelbreaks)
Fuel Reduction • Fuel continuity & build-up greatest in areas of most fire exclusion • Wildfires are reducing fuel, but these are mostly stand-replacing crown fires • Mechanical or prescribed-fire treatments not normally used on huge scales • Prescribed fire has a narrow window • Chemical (herbicide) treatments have ecological concerns
Fuel Conversion spruce • Species are limited (essentially aspen in the west) • Economic impact on species shift • Ecological/ Biodiversity impacts aspen
For a 400 x 400 km area (16 million ha), to limit fire size to 1000 ha with 200m wide “breaks” would require treating about 1 million ha! Even if a “perfect” fuel treatment can limit fire size, the area required to be treated is huge! Fuel Isolation
Fuel Management Summary • At large scales, the greatest potential for fuel management is in areas where a “natural” fire regime has been in place. • The greatest problems will be in areas where fire suppression has been effective, and fuel continuity and amount are above historical norms. • Without a major change in settlement and land-use, it is unlikely that fuels can be managed to reduce area burned in Canada over the next few decades.
“Global” Change • Changing fire weather • Climate effects on vegetation • Human changes to the landscape • Human effects on fire
Precipitation: 2xCO2/1xCO2 ratio REGIONAL CLIMATE MODEL May to Aug means Temperature: 2xCO2-1xCO2 (oC)
Regional Climate Model Fire Weather Index Ratio: 2xCO2/1xCO2 Interpretation: Fire danger will increase through much of western Canada
Future climate? (Hogg and Hurdle 1995 Water Air Soil Pollut.) Climate Effects on the West-Central Forest Present climate (isolines are a moisture index)
aspen lowland black spruce The Carbon Issue How much carbon is lost: - during the fire? - after the fire through decomposition? When does the forest turn from a source of carbon to a sink following a fire? Regeneration same year as fire:
Models estimate that Canadian forests have changed from net carbon sinks to sources, because of enhanced disturbance
Modelled Carbon Losses from Fire • Direct fire carbon losses are approximated from fuel combustion • The post-fire fluxes are largely unknown • The post-fire net carbon balance needs to be quantified, to include decomposition and succession kg carbon / m2 Wong 78 Kurz & Apps Kasischke et al. 95a Seiler & Crutzen 80 Auclair & Carter 93 Kasischke et al. 95b Dixon & Krankina 93
Mature jack pine Fort Providence, NWT One-year-old burn
Mature pine/aspen/spruce Prince Albert National Park, SK 10-year-old burn
1989 fires At the landscape scale, it appears to take close to 30 years before the forest returns to its “pre-burn” sink condition. Daytime carbon dioxide fluxes were measured along a 500 km transect during BOREAS 1995 fires
NPP in 1994. North-central Saskatchewan. (~ 130 km x 120 km area) Cree Lake
Estimates of NPP following fire for 10 ecoregions
Conclusions • Fire is the dominant stand-renewing agent in most of the boreal forest: ecologically, this forest needs fire. • Fuel management is unlikely to be successful at decreasing area burned, although the threat to small, valued areas (e.g., communities) can be reduced. • Landscape fragmentation is increasing, and although of ecological concern, it has had little impact on area burned to date. • A changing climate is likely to affect fire weather and vegetation types: The impact is to increase fire through much of the area: In mixed-wood areas, younger forests will burn less.