TY - JOUR
T1 - Variability of fire carbon emissions in equatorial Asia and its nonlinear sensitivity to El Niño
AU - Yin, Yi
AU - Ciais, Philippe
AU - Chevallier, Frederic
AU - van der Werf, Guido R.
AU - Fanin, Thierry
AU - Broquet, Gregoire
AU - Boesch, Hartmut
AU - Cozic, Anne
AU - Hauglustaine, Didier
AU - Szopa, Sophie
AU - Wang, Yilong
PY - 2016/10/16
Y1 - 2016/10/16
N2 - The large peatland carbon stocks in the land use change-affected areas of equatorial Asia are vulnerable to fire. Combining satellite observations of active fire, burned area, and atmospheric concentrations of combustion tracers with a Bayesian inversion, we estimated the amount and variability of fire carbon emissions in equatorial Asia over the period 1997–2015. Emissions in 2015 were of 0.51 ± 0.17 Pg carbon—less than half of the emissions from the previous 1997 extreme El Niño, explained by a less acute water deficit. Fire severity could be empirically hindcasted from the cumulative water deficit with a lead time of 1 to 2 months. Based on CMIP5 climate projections and an exponential empirical relationship found between fire carbon emissions and water deficit, we infer a total fire carbon loss ranging from 12 to 25 Pg by 2100 which is a significant positive feedback to climate warming.
AB - The large peatland carbon stocks in the land use change-affected areas of equatorial Asia are vulnerable to fire. Combining satellite observations of active fire, burned area, and atmospheric concentrations of combustion tracers with a Bayesian inversion, we estimated the amount and variability of fire carbon emissions in equatorial Asia over the period 1997–2015. Emissions in 2015 were of 0.51 ± 0.17 Pg carbon—less than half of the emissions from the previous 1997 extreme El Niño, explained by a less acute water deficit. Fire severity could be empirically hindcasted from the cumulative water deficit with a lead time of 1 to 2 months. Based on CMIP5 climate projections and an exponential empirical relationship found between fire carbon emissions and water deficit, we infer a total fire carbon loss ranging from 12 to 25 Pg by 2100 which is a significant positive feedback to climate warming.
KW - atmospheric inversion
KW - carbon cycle
KW - carbon emissions
KW - carbon monoxide
KW - MOPITT
KW - peat fire
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U2 - 10.1002/2016GL070971
DO - 10.1002/2016GL070971
M3 - Article
AN - SCOPUS:84990943364
SN - 0094-8276
VL - 43
SP - 10,472-10,479
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 19
ER -