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International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Fire weather index system components for large fires in the Canadian boreal forest

B. D. Amiro A D , K. A. Logan B , B. M. Wotton B C , M. D. Flannigan B , J. B. Todd A , B. J. Stocks B and D. L. Martell C
+ Author Affiliations
- Author Affiliations

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

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

C Faculty of Forestry, University of Toronto, 33 Willcocks Street, Toronto, ON, M5S 3B3, Canada.

D Corresponding author. Present address: Department of Soil Science, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada. Telephone: +1 204 474 9155; email: brian_amiro@umanitoba.ca

International Journal of Wildland Fire 13(4) 391-400 https://doi.org/10.1071/WF03066
Submitted: 16 September 2003  Accepted: 27 July 2004   Published: 15 December 2004

Abstract

Canadian Fire Weather Index (FWI) System components and head fire intensities were calculated for fires greater than 2 km2 in size for the boreal and taiga ecozones of Canada from 1959 to 1999. The highest noon-hour values were analysed that occurred during the first 21 days of each of 9333 fires. Depending on ecozone, the means of the FWI System parameters ranged from: fine fuel moisture code (FFMC), 90 to 92 (82 to 96 for individual fires); duff moisture code (DMC), 38 to 78 (10 to 140 for individual fires); drought code (DC), 210 to 372 (50 to 600 for individual fires); and fire weather index, 20 to 33 (5 to 60 for individual fires). Fine fuel moisture code decreased, DMC had a mid-season peak, and DC increased through the fire season. Mean head fire intensities ranged from 10 to 28 MW m−1 in the boreal spruce fuel type, showing that most large fires exhibit crown fire behaviour. Intensities of individual fires can exceed 60 MW m−1. Most FWI System parameters did not show trends over the 41-year period because of large inter-annual variability. A changing climate is expected to create future weather conditions more conducive to fire throughout much of Canada but clear changes have not yet occurred.

Additional keywords: drought; duff moisture; fire intensity; forest fire; seasonality; taiga; trends.


References


Alexander ME (1980) Calculating and interpreting forest fire intensities. Canadian Journal of Botany  60, 349–357.
Alexander ME, deGroot WJ (1989) ‘A decision aid for characterizing fire behavior and determining fire suppression needs.’ Technical Transfer Note A-008. (Canadian Forest Service: Edmonton)

Amiro BD, Todd JB, Wotton BM, Logan KA, Flannigan MD, Stocks BJ, Mason JA, Martell DL , Hirsch KG (2001) Direct carbon emissions from Canadian forest fires, 1959–1999. Canadian Journal of Forest Research  31, 512–525.
Crossref | GoogleScholarGoogle Scholar | Byram GM (1959) Combustion of forest fuels. In ‘Forest fire: control and use’. (Ed. KP Davis) pp. 61–89. (McGraw-Hill: New York)

Ecological Stratification Working Group (1996) ‘A national ecological framework for Canada.’ (Agriculture and Agri-Food Canada and Environment Canada: Ottawa)

Flannigan MD , Wotton BM (1989) A study of interpolation methods for forest fire danger rating in Canada. Canadian Journal of Forest Research  19, 1059–1066.
Flannigan MD, Logan K, Stocks BJ, Wotton BM, Amiro BD, Todd JB (2002) Projections of future fire activity and area burned in Canada. In ‘Forest fire research and wildland fire safety’. (Ed. DX Viegas) p. 14. (Millpress: Rotterdam)

Flannigan MD, Logan KA, Amiro BD, Skinner WR , Stocks BJ (2004) Future area burned in Canada. Climatic Change ,
Forestry Canada (1992) ‘Development and structure of the Canadian forest fire behavior prediction system.’ ST-X-3. (Science and Sustainable Development Directorate: Ottawa)

Girardin M-P, Tardif J, Flannigan MD, Wotton BM , Bergeron Y (2004) Trends and periodicities in the Canadian drought code and their relationships with atmospheric circulation for the southern Canadian boreal forest. Canadian Journal of Forest Research  34, 103–119.
Crossref | GoogleScholarGoogle Scholar | Harrington JB (1982) ‘A statistical study of area burned by wildfire in Canada 1953–1980.’ PI-X-16. (Petawawa National Forestry Institute, Canadian Forestry Service: Petawawa)

Harrington JB, Flannigan MD, Van Wagner CE (1983) ‘A study of the relation of components of the fire weather index to monthly provincial area burned by wildfire in Canada 1953–80.’ PI-X-25. (Petawawa National Forestry Institute, Canadian Forestry Service: Petawawa)

Hirsch KG, Corey PN , Martell DL (1998) Using expert judgement to model initial attack fire crew effectiveness. Forest Science  44, 539–549.
Kafka V, Tymstra C, Hirsch K, Flannigan M (2000) Assessing fire behavior potential: a comparative analysis of two spatial techniques. In ‘Crossing the millenium: integrating spatial technologies and ecological principles for a new age in fire management’. Vol. 1. (Eds LF Neuenschwander, KC Ryan) pp. 113–122. (University of Idaho: Moscow, ID)

Podur J, Martell DL , Knight K (2002) Statistical quality control analysis of forest fire activity in Canada. Canadian Journal of Forest Research  32, 195–205.
Crossref | GoogleScholarGoogle Scholar | SAS (2000) ‘OnlineDoc®, Version 8. SAS Institute Inc.’ (SAS Institute Inc.: Cary, NC)

Simard AJ, Valenzuela J (1972) ‘A climatological summary of the Canadian Forest Fire Weather Index.’ FF-X-34. (Canadian Forestry Service: Ottawa)

Skinner WR, Flannigan MD, Stocks BJ, Martell DL, Wotton BM, Todd JB, Mason JA, Logan KA , Bosch EM (2002) A 500 hPa synoptic wildland fire climatology for large Canadian forest fires, 1959–1996. Theoretical and Applied Climatology  71, 157–169.
Crossref | GoogleScholarGoogle Scholar | SYSTAT (1997) ‘SYSTAT software.’ (SPSS Inc.: Chicago)

Van Wagner CE (1987) ‘Development and structure of the Canadian forest fire weather index system.’ Forest Technology Report 35. (Canadian Forestry Service: Ottawa)

Woodward WA, Bottone S , Gray HL (1997) Improved tests for trend in time series data. Journal of Agricultural Biological & Environmental Statistics  2, 403–416.


Zhang XB, Vincent LA, Hogg WD , Niitsoo A (2000) Temperature and precipitation trends in Canada during the 20th century. Atmosphere-Ocean  38, 395–429.