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Table 2 Selected fire history studies for areas within fire weather index (FWI) zones of Canada (see Figure 3). Where detailed fire history studies are unavailable, research from areas in adjacent United States was used. If researchers assigned climate change as a primary factor causal to a fire frequency change at the end of a period, this is indicated by an asterisk.

From: Burning at the Edge: Integrating Biophysical and Eco-Cultural Fire Processes in Canada’s Parks and Protected Areas

FWI zone

Ecozonea-vegetation cover

Reference

Estimated mean fire interval or fire cycleb in years (time period, year AD)

Potential causal covariates analyzedc

Early period

Middle period

Late period

Minimal

PM-conifer

Lertzman et al. 2002 Gavin et al. 2003

>1000 (<2000)

  

TE, FT, C

PM-conifer

Daniels and Gray 2006

>500

 

>fire

LU

MC-conifer

Hawkes 1997, Kopra and Feller 2007

>500(<1940)

  

TE, RC

PM-conifer

Hallett et al. 2003

174–272 (800–2000)

  

RC, C

Very low

TP-boreal conifer

Johnson 1979

102 (<1975)

  

RC

BSE-conifer

Bergeron et al. 2001

69*(<1850)

123* (1850–1920)

273 (1920–1999)

C, RC

BSE-conifer

Bouchard et al. 2008

>500 (1800–2000)

  

RC

Low

TP-boreal conifer

Johnson 1979

70 (<1975)

  

RC

BSE-conifer

Bergeron et al. 2001

 

86* (1850–1920)

195 (1920–1999)

C, RC

BSE-conifer

Le Goff et al. 2007

99* (1720–1940)

 

282 (1940–1998)

C, RC

BSE-conifer

Lauzon et al. 2007

89* (1600–1850)

 

176 (1850–2003)

IW, IT

BSE-conifer

Bouchard et al. 2008

250 (1800–2000)

  

RC

Moderate

MC-conifer

Van Wagner 1978

50 (1680–1915)

 

>80 (1915–1960)

LU

TP-boreal conifer

Johnson 1979

50 (<1975)

  

RC

MC-conifer

Johnson et al. 1990

80* (1520–1760)

 

110 (1760–1988)

TE, LU

BSE-conifer

Bergeron et al. 2001

131* (<1850)

234* (1850–1920)

521 (1920–1999)

C, RC

BSE-conifer

Bergeron et al. 2001

83*(<1850)

146* (1850–1920)

325 (1920–1999)

C, RC

BSE-mixedwood

Lefort 2003, Bergeron et al. 2004b

83*(<1850)

111* (1850–1920)

326 (1920–1990)

C, FT, IW, RC, IT, FT, LU, LF

BC-conifer

Bothwell et al. 2004

28 (1813–1974)

  

RC

TP-boreal conifer

Bothwell et al. 2004

27 (1765–1977)

  

RC

High

BSW-mixedwood

Heinselman 1973, Van Wagner 1978

47 (1542–1911)

 

1000 (1911–1970)

IW, FT, IT, S, FS, LU

AM-mixedwood

Wein and Moore 1977

  

>650 (1920–1975)

FT, IT, S, RC

MC-conifer

Tande 1979

74 (1675–1913)

 

Few fires (1913–1975)

TE, FT

TP-boreal conifer

Johnson 1979

37 (<1975)

  

RC

BP-conifer

Larsen 1997

25–49 (1750–1859)

 

59–89 (1860–1989

FT

BP-conifer

Weir et al. 2000

15* (<1890)

75* (1890–1945)

1745 (1945–1996)

RC, LU

MP-mixedwood

Dey and Guyette 2000, Cwyner 1977

29 (1643–1814)

6 (1814–1954)

Few fires

RC, IT, TK, LU

BP-mixedwood

Tardif 2004

35 (1700–1880)

278 (1900–1960)

>15 000 (1960–2002)

C, LU, FS

Very high

MC-conifer grassland

Tande 1979

21* (1675–1913)

 

Few fires (1913–1975)

TE, FT

MC-conifer

Masters 1990

60* (1508–1778)

130* (1778–1928)

>2700 (1928–1988)

TE

MC-conifer

Johnson and Larsen 1991

50* (1600–1730)

 

90 (1730–1990)

TE

BP-mixedwood

Weir et al. 2000

25* (1795–1945)

 

645 (1945–1996)

FT, LU, IT

MC-conifer westslope

Van Wagner et al. 2006

99 (1332–1840)

 

352 (1841–1999)

RC, C, LF

MC-conifer eastslope

Van Wagner et al. 2006, and others

72 (1285–1760)

174 (1760–1940)

6855 (1941–1999)

RC, C, IW, TE, IT, FS, LU, TK, LF

MC-conifer grass

Heyerdahl et al. 2006

37 (1700–1860)

 

Few fires (1860–2005)

LU, C, TE

Extreme

MC-conifer

Gray et al. 2004

19 (1694–1883)

 

>115 (1884–1998)

TE

MC-conifer grass

Heyerdahl et al. 2005

16 (1750–1950)

 

Few fires (1950–2004)

TE, S

MC-conifer grass

Daniels et al. 2009

10–26 (1509–1944)

 

Few fires (1944–2006)

C, LU

P-conifer grass

Fisher et al. 1987

27 (1600–1770)

14 (1770–1900)

42 (1900–1987)

LU, FS

P-conifer grass

Brown and Seig 1999

10–12 (1564–1912)

 

Few fires (1912–1996)

S, LU, RC

  1. a See Figure 1.
  2. b As defined by Johnson and Van Wagner (1985), the mean fire interval is the average time between known dates of fires across a point, whereas the fire cycle is the time required to burn an area equal to the study area.
  3. c Covariates are coded as proxy climate data, usually derived from tree-ring studies (C), fire suppression (FS), fuel or vegetation type (FT), ignition type (IT), instrumental weather data (IW), lightning frequency (LF), land-use changes (LU), regional comparisons between areas (RC), local topography effects (TE), seasonality (S), and First Nations’ occupation patterns and traditional knowledge (TK).