Abstract

We report measurements and analysis of a boreal forest fire, integrating the effects of greenhouse gases, aerosols, black carbon deposition on snow and sea ice, and postfire changes in surface albedo. The net effect of all agents was to increase radiative forcing during the first year (34 ± 31 Watts per square meter of burned area), but to decrease radiative forcing when averaged over an 80-year fire cycle (–2.3 ± 2.2 Watts per square meter) because multidecadal increases in surface albedo had a larger impact than fire-emitted greenhouse gases. This result implies that future increases in boreal fire may not accelerate climate warming.

Keywords

Radiative forcingEnvironmental scienceAlbedo (alchemy)BorealTaigaAtmospheric sciencesGreenhouse gasSnowBlack spruceForcing (mathematics)ClimatologyGlobal warmingClimate changeMeteorologyOceanographyGeographyGeologyForestry

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Publication Info

Year
2006
Type
article
Volume
314
Issue
5802
Pages
1130-1132
Citations
931
Access
Closed

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James T. Randerson, H. Liu, M. Flanner et al. (2006). The Impact of Boreal Forest Fire on Climate Warming. Science , 314 (5802) , 1130-1132. https://doi.org/10.1126/science.1132075

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DOI
10.1126/science.1132075