Fire-induced carbon emissions and regrowth uptake in western U.S. forests: Documenting variation across forest types, fire severity, and climate regions

The forest area in the western United States that burns annually is increasing with warmer temperatures, more frequent droughts, and higher fuel densities. Studies that examine fire effects for regional carbon balances have tended to either focus on individual fires as examples or adopt generalizati...

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Bibliographic Details
Published in:Journal of Geophysical Research: Biogeosciences Vol. 117; no. G3
Main Authors: Ghimire, Bardan, Williams, Christopher A., Collatz, G. James, Vanderhoof, Melanie
Format: Journal Article
Language:English
Published: Washington, DC Blackwell Publishing Ltd 01-09-2012
American Geophysical Union
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Summary:The forest area in the western United States that burns annually is increasing with warmer temperatures, more frequent droughts, and higher fuel densities. Studies that examine fire effects for regional carbon balances have tended to either focus on individual fires as examples or adopt generalizations without considering how forest type, fire severity, and regional climate influence carbon legacies. This study provides a more detailed characterization of fire effects and quantifies the full carbon impacts in relation to direct emissions, slow release of fire‐killed biomass, and net carbon uptake from forest regrowth. We find important variations in fire‐induced mortality and combustion across carbon pools (leaf, live wood, dead wood, litter, and duff) and across low‐ to high‐severity classes. This corresponds to fire‐induced direct emissions from 1984 to 2008 averaging 4 TgC yr−1 and biomass killed averaging 10.5 TgC yr−1, with average burn area of 2723 km2 yr−1across the western United States. These direct emission and biomass killed rates were 1.4 and 3.7 times higher, respectively, for high‐severity fires than those for low‐severity fires. The results show that forest regrowth varies greatly by forest type and with severity and that these factors impose a sustained carbon uptake legacy. The western U.S. fires between 1984 and 2008 imposed a net source of 12.3 TgC yr−1 in 2008, accounting for both direct fire emissions (9.5 TgC yr−1) and heterotrophic decomposition of fire‐killed biomass (6.1 TgC yr−1) as well as contemporary regrowth sinks (3.3 TgC yr−1). A sizeable trend exists toward increasing emissions as a larger area burns annually. Key Points Comprehensive review of fire‐induced plant combustion and mortality Introduces detailed post‐fire carbon flux trajectories for western U.S. forests Assesses interannual variation in regional carbon emissions and uptake from fire
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ark:/67375/WNG-PH7N12SR-1
ArticleID:2011JG001935
istex:3CE8B4417BFA7CD4D49CAC9513F290A640514F11
ISSN:0148-0227
2169-8953
2156-2202
2169-8961
DOI:10.1029/2011JG001935