The potential and realized spread of wildfires across Canada

被引:58
作者
Wang, Xianli [1 ]
Parisien, Marc-Andre [2 ]
Flannigan, Mike D. [1 ,2 ]
Parks, Sean A. [3 ]
Anderson, Kerry R. [2 ]
Little, John M. [2 ]
Taylor, Steve W. [4 ]
机构
[1] Univ Alberta, Dept Renewable Resources, Edmonton, AB T6G 2H1, Canada
[2] Nat Resources Canada, Canadian Forest Serv, No Forestry Ctr, Edmonton, AB T6H 3S5, Canada
[3] US Forest Serv, USDA, Aldo Leopold Wilderness Res Inst, Rocky Mt Res Stn, Missoula, MT 59801 USA
[4] Nat Resources Canada, Canadian Forest Serv, Pacific Forestry Ctr, Victoria, BC V8Z 1M5, Canada
关键词
boreal forests; Canada; fire spread; MODIS fire detections; temperate forests; weather; FIRE REGIME ZONATION; FOREST-FIRES; UNITED-STATES; CLIMATE; WEATHER; COMPONENTS; GROWTH; PROBABILITY; VARIABILITY; SIMULATION;
D O I
10.1111/gcb.12590
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Given that they can burn for weeks or months, wildfires in temperate and boreal forests may become immense (eg., 10(0)-10(4) km(2)). However, during the period within which a large fire is 'active', not all days experience weather that is conducive to fire spread; indeed most of the spread occurs on a small proportion (e. g., 1 - 15 days) of not necessarily consecutive days during the active period. This study examines and compares the Canada-wide patterns in fire-conducive weather ('potential' spread) and the spread that occurs on the ground ('realized' spread). Results show substantial variability in distributions of potential and realized spread days across Canada. Both potential and realized spread are higher in western than in eastern Canada; however, whereas potential spread generally decreases from south to north, there is no such pattern with realized spread. The realized-to-potential fire-spread ratio is considerably higher in northern Canada than in the south, indicating that proportionally more fire-conducive days translate into fire progression. An exploration of environmental correlates to spread show that there may be a few factors compensating for the lower potential spread in northern Canada: a greater proportion of coniferous (i.e., more flammable) vegetation, lesser human impacts (i.e., less fragmented landscapes), sufficient fire ignitions, and intense droughts. Because a linear relationship exists between the frequency distributions of potential spread days and realized spread days in a fire zone, it is possible to obtain one from the other using a simple conversion factor. Our methodology thus provides a means to estimate realized fire spread from weather-based data in regions where fire databases are poor, which may improve our ability to predict future fire activity.
引用
收藏
页码:2518 / 2530
页数:13
相关论文
共 71 条
[21]   A simulation of probabilistic wildfire risk components for the continental United States [J].
Finney, Mark A. ;
McHugh, Charles W. ;
Grenfell, Isaac C. ;
Riley, Karin L. ;
Short, Karen C. .
STOCHASTIC ENVIRONMENTAL RESEARCH AND RISK ASSESSMENT, 2011, 25 (07) :973-1000
[22]   Future area burned in Canada [J].
Flannigan, MD ;
Logan, KA ;
Amiro, BD ;
Skinner, WR ;
Stocks, BJ .
CLIMATIC CHANGE, 2005, 72 (1-2) :1-16
[23]  
FLANNIGAN MD, 1988, J APPL METEOROL, V27, P441, DOI 10.1175/1520-0450(1988)027<0441:ASOTRO>2.0.CO
[24]  
2
[25]   THE HISTORY AND PATTERN OF FIRE IN THE BOREAL FOREST OF SOUTHEASTERN LABRADOR [J].
FOSTER, DR .
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE, 1983, 61 (09) :2459-2471
[26]  
Gavin DG, 2006, ECOLOGY, V87, P1722, DOI 10.1890/0012-9658(2006)87[1722:WCCOSF]2.0.CO
[27]  
2
[28]   Atmospheric, climatic, and ecological controls on extreme wildfire years in the northwestern United States [J].
Gedalof, Z ;
Peterson, DL ;
Mantua, NJ .
ECOLOGICAL APPLICATIONS, 2005, 15 (01) :154-174
[29]   Three centuries of annual area burned variability in northwestern North America inferred from tree rings [J].
Girardin, Martin P. ;
Sauchyn, Dave .
HOLOCENE, 2008, 18 (02) :205-214
[30]   Temporal variability in area burned for the province of Ontario, Canada, during the past 200 years inferred from tree rings [J].
Girardin, Martin P. ;
Tardif, Jacques ;
Flannigan, Mike D. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D17)