The influence of vegetation, fire spread and fire behaviour on biomass burning and trace gas emissions: results from a process-based model

被引:308
作者
Thonicke, K. [1 ,2 ,3 ,9 ]
Spessa, A. [1 ,4 ,5 ,9 ]
Prentice, I. C. [1 ,6 ,7 ,9 ]
Harrison, S. P. [2 ,6 ]
Dong, L.
Carmona-Moreno, C. [8 ]
机构
[1] Max Planck Inst Biogeochem, D-07701 Jena, Germany
[2] Univ Bristol, Sch Geog Sci, Bristol BS8 1SS, Avon, England
[3] Macquarie Univ, Dept Biol Sci, N Ryde, NSW 2109, Australia
[4] Univ London Imperial Coll Sci Technol & Med, Grantham Inst Climate Change, Ascot SL5 7PY, Berks, England
[5] Univ London Imperial Coll Sci Technol & Med, Div Biol, Ascot SL5 7PY, Berks, England
[6] Univ Reading, NCAS Climate, Natl Ctr Atmospher Sci, Reading RG6 6BB, Berks, England
[7] Univ Bristol, QUEST, Dept Earth Sci, Bristol BS8 1RJ, Avon, England
[8] Joint Res Ctr Ispra, Global Vegetat Monitoring Unit, Ispra, Italy
[9] Potsdam Inst Climate Impact Res PIK eV, D-14473 Potsdam, Germany
关键词
DYNAMIC GLOBAL VEGETATION; CLIMATE-CHANGE; TROPICAL SAVANNA; TREE MORTALITY; WATER-BALANCE; CARBON; FOREST; REGIMES; AREA; SIMULATIONS;
D O I
10.5194/bg-7-1991-2010
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A process-based fire regime model (SPITFIRE) has been developed, coupled with ecosystem dynamics in the LPJ Dynamic Global Vegetation Model, and used to explore fire regimes and the current impact of fire on the terrestrial carbon cycle and associated emissions of trace atmospheric constituents. The model estimates an average release of 2.24 Pg C yr(-1) as CO2 from biomass burning during the 1980s and 1990s. Comparison with observed active fire counts shows that the model reproduces where fire occurs and can mimic broad geographic patterns in the peak fire season, although the predicted peak is 1-2 months late in some regions. Modelled fire season length is generally overestimated by about one month, but shows a realistic pattern of differences among biomes. Comparisons with remotely sensed burnt-area products indicate that the model reproduces broad geographic patterns of annual fractional burnt area over most regions, including the boreal forest, although interannual variability in the boreal zone is underestimated.
引用
收藏
页码:1991 / 2011
页数:21
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