Recent changes in the fire regime across the North American boreal region-Spatial and temporal patterns of burning across Canada and Alaska

We used historic records from 1959–99 to explore fire regime characteristics at ecozone scales across the entire North American boreal region (NABR). Shifts in the NABR fire regime between the 1960s/70s and the 1980s/90s were characterized by a doubling of annual burned area and more than a doubling...

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Published inGeophysical research letters Vol. 33; no. 9
Main Authors Kasischke, Eric S., Turetsky, Merritt R.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.05.2006
American Geophysical Union
Subjects
Online AccessGet full text
ISSN0094-8276
1944-8007
DOI10.1029/2006GL025677

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Abstract We used historic records from 1959–99 to explore fire regime characteristics at ecozone scales across the entire North American boreal region (NABR). Shifts in the NABR fire regime between the 1960s/70s and the 1980s/90s were characterized by a doubling of annual burned area and more than a doubling of the frequency of larger fire years because of more large fire events (>1,000 km2). The proportion of total burned area from human‐ignited fires decreased over this same time period, while the proportion of burning during the early and late‐ growing‐seasons increased. Trends in increased burned area were consistent across the NABR ecozones, though the western ecozones experienced greater increases in larger fire years compared to the eastern ecozones. Seasonal patterns of burning differed among ecozones. Along with the climate warming, changes in the fire regime characteristics may be an important driver of future ecosystem processes in the NABR.
AbstractList We used historic records from 1959–99 to explore fire regime characteristics at ecozone scales across the entire North American boreal region (NABR). Shifts in the NABR fire regime between the 1960s/70s and the 1980s/90s were characterized by a doubling of annual burned area and more than a doubling of the frequency of larger fire years because of more large fire events (>1,000 km 2 ). The proportion of total burned area from human‐ignited fires decreased over this same time period, while the proportion of burning during the early and late‐ growing‐seasons increased. Trends in increased burned area were consistent across the NABR ecozones, though the western ecozones experienced greater increases in larger fire years compared to the eastern ecozones. Seasonal patterns of burning differed among ecozones. Along with the climate warming, changes in the fire regime characteristics may be an important driver of future ecosystem processes in the NABR.
We used historic records from 1959-99 to explore fire regime characteristics at ecozone scales across the entire North American boreal region (NABR). Shifts in the NABR fire regime between the 1960s/70s and the 1980s/90s were characterized by a doubling of annual burned area and more than a doubling of the frequency of larger fire years because of more large fire events ( > 1,000 km2). The proportion of total burned area from human-ignited fires decreased over this same time period, while the proportion of burning during the early and late-growing-seasons increased. Trends in increased burned area were consistent across the NABR ecozones, though the western ecozones experienced greater increases in larger fire years compared to the eastern ecozones. Seasonal patterns of burning differed among ecozones. Along with the climate warming, changes in the fire regime characteristics may be an important driver of future ecosystem processes in the NABR.
Author Turetsky, Merritt R.
Kasischke, Eric S.
Author_xml – sequence: 1
  givenname: Eric S.
  surname: Kasischke
  fullname: Kasischke, Eric S.
  email: ekasisch@geog.umd.edu
  organization: Department of Geography, University of Maryland, Maryland, College Park, USA
– sequence: 2
  givenname: Merritt R.
  surname: Turetsky
  fullname: Turetsky, Merritt R.
  organization: Department of Plant Biology and Wildlife, Michigan State University, Michigan, East Lansing, USA
BackLink http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17847445$$DView record in Pascal Francis
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10.1029/2004GB002300
10.1007/s007040050095
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Keywords trend-surface analysis
fires
ecosystems
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climate warming
Boreal
North America
frequency
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References Kasischke, E. S., and J. F. Johnstone (2005), Variation in post-fire organic layer thickness in a black spruce forest complex in Interior Alaska and its effects on soil temperature and moisture, Can. J. For. Res., 35, 2164-2177.
Liu, H., J. T. Randerson, J. Lindfors, and F. S. Chapin III (2005), Changes in the surface energy budget after fire in boreal ecosystems of interior Alaska: An annual perspective, J. Geophys. Res., 110, D13101, doi:10.1029/2004JD005158.
Stocks, B. J., et al. (2002), Large forest fires in Canada, 1959-1997, J. Geophys. Res., 108(D1), 8149, doi:10.1029/2001JD000484.
Kasischke, E. S., E. J. Hyer, P. C. Novelli, L. P. Bruhwiler, N. H. F. French, A. I. Sukhinin, J. H. Hewson, and B. J. Stocks (2005), Influences of boreal fire emissions on Northern Hemisphere atmospheric carbon and carbon monoxide, Global Biogeochem. Cycles, 19, GB1012, doi:10.1029/2004GB002300.
Kasischke, E. S., D. Williams, and D. Barry (2002), Analysis of the patterns of large fires in the boreal forest region of Alaska, Int. J. Wildland Fire, 11, 131-144.
Kurz, W. A., and M. J. Apps (1999), A 70-year retrospective analysis of carbon fluxes in the Canadian forest sector, Ecol. Appl., 9, 526-547.
Wein, R. W., and D. A. MacLean (1983), The Role of Fire in Northern Circumpolar Ecosystems, 322 pp., John Wiley, Hoboken, N. J.
Hess, J. C., C. A. Scott, G. L. Hufford, and M. D. Fleming (2001), El Nino and its impact on fire weather conditions in Alaska, Int. J. Wildland Fire, 10, 1-13.
Gillett, N. P., A. J. Weaver, F. W. Zwiers, and M. D. Flannigan (2004), Detecting the effect of climate change on Canadian forest fires, Geophys. Res. Lett., 31, L18211, doi:10.1029/2004GL020876.
Landhaeusser, S. M., and R. W. Wein (1993), Postfire vegetation recovery and tree establishment at the Arctic treeline: Climactic-change-vegetation-response hypothesis, J. Ecol., 81, 665-672.
Turetsky, M., K. Wieder, L. Halsey, and D. Vitt (2002), Current disturbance and the diminishing peatland carbon sink, Geophys. Res. Lett., 29(11), 1526, doi:10.1029/2001GL014000.
Duffy, P. A., J. E. Walsh, J. M. Graham, D. H. Mann, and T. S. Rupp (2005), Impacts of large-scale atmospheric-ocean variability on Alaskan fire season severity, Ecol. Appl., 15, 1317-1330.
Harden, J. W., S. E. Trumbore, B. J. Stocks, A. Hirsch, S. T. Gower, K. P. O'Neill, and E. S. Kasischke (2000), The role of fire in the boreal carbon budget, Global Change Biol., 6, 174-184.
Skinner, W. R., B. J. Stocks, D. L. Martell, B. Bonsal, and A. Shabbar (1999), The association between circulation anomalies in the mid-troposphere and area burned by wildland fire in Canada, Theor. Appl. Climatol., 63, 89-105.
Bergner, B., J. Johnstone, and K. K. Treseder (2004), Experimental warming and burn severity alter CO2 flux and soil functional groups in recently burned boreal forest, Global Change Biol., 10, 1996-2004.
Flannigan, M. D., K. A. Logan, B. D. Amiro, W. R. Skinner, and B. J. Stocks (2005), Future area burned in Canada, Clim. Change, 72, 1-16.
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References_xml – reference: Harden, J. W., S. E. Trumbore, B. J. Stocks, A. Hirsch, S. T. Gower, K. P. O'Neill, and E. S. Kasischke (2000), The role of fire in the boreal carbon budget, Global Change Biol., 6, 174-184.
– reference: Kasischke, E. S., and J. F. Johnstone (2005), Variation in post-fire organic layer thickness in a black spruce forest complex in Interior Alaska and its effects on soil temperature and moisture, Can. J. For. Res., 35, 2164-2177.
– reference: Skinner, W. R., B. J. Stocks, D. L. Martell, B. Bonsal, and A. Shabbar (1999), The association between circulation anomalies in the mid-troposphere and area burned by wildland fire in Canada, Theor. Appl. Climatol., 63, 89-105.
– reference: Stocks, B. J., et al. (2002), Large forest fires in Canada, 1959-1997, J. Geophys. Res., 108(D1), 8149, doi:10.1029/2001JD000484.
– reference: Kasischke, E. S., D. Williams, and D. Barry (2002), Analysis of the patterns of large fires in the boreal forest region of Alaska, Int. J. Wildland Fire, 11, 131-144.
– reference: Turetsky, M., K. Wieder, L. Halsey, and D. Vitt (2002), Current disturbance and the diminishing peatland carbon sink, Geophys. Res. Lett., 29(11), 1526, doi:10.1029/2001GL014000.
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– reference: Hess, J. C., C. A. Scott, G. L. Hufford, and M. D. Fleming (2001), El Nino and its impact on fire weather conditions in Alaska, Int. J. Wildland Fire, 10, 1-13.
– reference: Landhaeusser, S. M., and R. W. Wein (1993), Postfire vegetation recovery and tree establishment at the Arctic treeline: Climactic-change-vegetation-response hypothesis, J. Ecol., 81, 665-672.
– reference: Wein, R. W., and D. A. MacLean (1983), The Role of Fire in Northern Circumpolar Ecosystems, 322 pp., John Wiley, Hoboken, N. J.
– reference: Liu, H., J. T. Randerson, J. Lindfors, and F. S. Chapin III (2005), Changes in the surface energy budget after fire in boreal ecosystems of interior Alaska: An annual perspective, J. Geophys. Res., 110, D13101, doi:10.1029/2004JD005158.
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Snippet We used historic records from 1959–99 to explore fire regime characteristics at ecozone scales across the entire North American boreal region (NABR). Shifts in...
We used historic records from 1959-99 to explore fire regime characteristics at ecozone scales across the entire North American boreal region (NABR). Shifts in...
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SubjectTerms Earth sciences
Earth, ocean, space
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Title Recent changes in the fire regime across the North American boreal region-Spatial and temporal patterns of burning across Canada and Alaska
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