How does increased fire frequency affect carbon loss from fire? A case study in the northern boreal forest

被引:45
作者
Brown, C. D. [1 ]
Johnstone, J. F. [1 ]
机构
[1] Univ Saskatchewan, Dept Biol, Saskatoon, SK S7N 5E2, Canada
关键词
adventitious root method; biomass; fire return interval; soil organic layer; Yukon; CLIMATE-CHANGE; SOIL-TEMPERATURE; CHANGING CLIMATE; DISTURBANCE; FEEDBACKS; SEVERITY; DYNAMICS; EXCHANGE; WILDFIRE; STORAGE;
D O I
10.1071/WF10113
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Fire frequency is expected to increase due to climate warming in many areas, particularly the boreal forests. An increase in fire frequency may have important effects on the global carbon cycle by decreasing the size of boreal carbon stores. Our objective was to quantify and compare the amount of carbon consumed during and the amount of carbon remaining following fire in black spruce (Picea mariana (Mill.) BSP) forests burned after long v. short intervals. We hypothesised that stands with a shortened fire return interval would have a higher carbon consumption than those experiencing a historically typical fire return interval. Using field measurements of forest canopy, soil organic horizons and adventitious roots, we reconstructed pre-fire stand conditions to estimate the biomass lost in each fire and the effects on post-fire residual carbon stores. We found evidence of a higher loss of carbon following two fire events that recurred after a short interval, resulting in a much greater total reduction in carbon relative to pre-fire or mature stand conditions. Consequently, carbon storage across disturbance intervals was dramatically reduced following short-interval burns. Recovery of these stores would require a subsequent lengthening of the fire cycle, which appears unlikely under future climate scenarios.
引用
收藏
页码:829 / 837
页数:9
相关论文
共 65 条
[1]   Post-fire carbon dioxide fluxes in the western Canadian boreal forest: evidence from towers, aircraft and remote sensing [J].
Amiro, BD ;
MacPherson, JI ;
Desjardins, RL ;
Chen, JM ;
Liu, J .
AGRICULTURAL AND FOREST METEOROLOGY, 2003, 115 (1-2) :91-107
[2]  
[Anonymous], 1992, FIRE VEGETATION DYNA, DOI DOI 10.1017/CBO9780511623516
[3]  
Auerbach NA, 1997, ECOL APPL, V7, P218, DOI 10.1890/1051-0761(1997)007[0218:EORDOS]2.0.CO
[4]  
2
[5]   Assessing the response of area burned to changing climate in western boreal North America using a Multivariate Adaptive Regression Splines (MARS) approach [J].
Balshi, Michael S. ;
McGuirez, A. David ;
Duffy, Paul ;
Flannigan, Mike ;
Walsh, John ;
Melillo, Jerry .
GLOBAL CHANGE BIOLOGY, 2009, 15 (03) :578-600
[6]   THE RELATIVE IMPORTANCE OF FUELS AND WEATHER ON FIRE BEHAVIOR IN SUB-ALPINE FORESTS [J].
BESSIE, WC ;
JOHNSON, EA .
ECOLOGY, 1995, 76 (03) :747-762
[7]   REPRODUCTIVE ECOLOGY OF PICEA-MARIANA (MILL) BSP, AT TREE LINE NEAR INUVIK, NORTHWEST TERRITORIES, CANADA [J].
BLACK, RA ;
BLISS, LC .
ECOLOGICAL MONOGRAPHS, 1980, 50 (03) :331-354
[8]   Quantifying fire severity, carbon, and nitrogen emissions in Alaska's boreal forest [J].
Boby, Leslie A. ;
Schuur, Edward A. G. ;
Mack, Michelle C. ;
Verbyla, David ;
Johnstone, Jill F. .
ECOLOGICAL APPLICATIONS, 2010, 20 (06) :1633-1647
[9]   Net primary production and net ecosystem production of a boreal black spruce wildfire chronosequence [J].
Bond-Lamberty, B ;
Wang, CK ;
Gower, ST .
GLOBAL CHANGE BIOLOGY, 2004, 10 (04) :473-487
[10]   Urgent preservation of boreal carbon stocks and biodiversity [J].
Bradshaw, Corey J. A. ;
Warkentin, Ian G. ;
Sodhi, Navjot S. .
TRENDS IN ECOLOGY & EVOLUTION, 2009, 24 (10) :541-548