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Fire Research » Fire & Climate Change » National & International Activities

Assessing Past, Current, and Future Fire Occurrence and Fire Severity in British Columbia

Fire is a critical process in British Columbia's forests in terms of their composition, structure, and function. Climate change will result in an altered fire regime that has the potential to overshadow the importance of the direct effects of climate warming on species distribution, migration, substitution, and extinction. Understanding the changes in fire activity, number of fire starts, and area burned that British Columbia can expect under climate change is extremely important to the general public from both timber loss and community protection standpoints. It is also important in the context of improving our understanding of how fire disturbances will influence forest succession and migration under future climate conditions.

1955 Aug 1-15 FFMC map of BC
1961 Aug 1-15 FFMC map of BC

Historic data of 90th percentile Fine Fuel Moisture Code for 1–15 August for 1955 (top) and 1961 (bottom)

Fire weather represents unique short periods of weather involving temperature, humidity, and wind speed. If global circulation model (GCM) and regional climate model (RCM) projections of climate change are to be considered for use in assessing future fire weather conditions, it is imperative that they be able to recreate current weather conditions. To date, the resolution of the GCM is inadequate to reliably predict events for British Columbia, and more sophisticated analysis is required to predict the impact of climate change for British Columbia's complex terrain and vegetation conditions at a regional level.

RCM 1xCO2 SSR Map of BC

In this current work, the potential of the RCM to generate realistic fire weather, danger, occurrence, and area burned estimates for projections of current climate conditions in British Columbia will be evaluated. The intent is to provide feedback to the RCM modeling community on the ability of current models to simulate current fire weather conditions. Recommendations will be made on where improvements are needed to reduce uncertainty and improve confidence in using the RCM for assessing the implications of climate change on future fire regimes.

Moreover, there is some evidence to suggest that severe fire seasons, fire occurrence, and drought in British Columbia are associated with sea surface temperature anomalies (El Niño and La Niña). The second component of this project is designed to establish whether any trends exist between fire season severity and the occurrence of El Niño and La Niña. This work should establish predictive relationships that could be used to support long-term seasonal fire management planning in British Columbia, by identifying the epicentre location and strength of past anomalies and the lag time associated with fire occurrence and drought. The frequency of problematic synoptic patterns such as omega blocks, cold fronts, and severe lightning associated with El Niño and La Niña will also be evaluated.

RCM projection of mean 90th percentile Daily Severity Rating for 1 x CO2 scenario (1975–1985).

RCM 2xCO2 SSR Map of BC

RCM projection of mean 90th percentile Daily Severity Rating for 2 x CO2 scenario (2041–2049).

RCM 3xCO2 SSR Map of BC

RCM projection of mean 90th percentile Daily Severity Rating for 3 x CO2 scenario (2080–2089).

For more information, contact:

M.D. (Mike) Flannigan

 

Canadian Forest Service
Great Lakes Forestry Centre
1219 Queen Street East
Sault Ste. Marie, ON P6A 2E5

Phone: (705) 541-5541
Fax: (705) 541-5701
e-mail: Mike.Flannigan@nrcan.gc.ca

J.B. (Bernie) Todd

 

Canadian Forest Service
Northern Forestry Centre
5320-122 Street
Edmonton, AB T6H 3S5

Phone: (780) 435-7398
Fax: (780)435-7359
e-mail: Bernie.Todd@NRCan.gc.ca

B.M. (Mike) Wotton

 

Canadian Forest Service
Great Lakes Forestry Centre
1219 Queen Street East
Sault Ste. Marie, ON P6A 2E5

Phone: (705) 541-5740
Fax: (705) 541-5701
e-mail: Mike.Wotton@nrcan.gc.ca

 

 

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