Improved quantification of Chinese carbon fluxes using CO2/CO correlations in Asian outflow -: art. no. D18S18

被引:119
作者
Suntharalingam, P
Jacob, DJ
Palmer, PI
Logan, JA
Yantosca, RM
Xiao, YP
Evans, MJ
Streets, DG
Vay, SL
Sachse, GW
机构
[1] Harvard Univ, Div Engn & Appl Sci, Cambridge, MA 02138 USA
[2] Argonne Natl Lab, Argonne, IL 60439 USA
[3] NASA, Langley Res Ctr, Hampton, VA 23681 USA
基金
英国自然环境研究理事会;
关键词
regional carbon fluxes; multiple-species correlations; atmospheric; CO2; modeling;
D O I
10.1029/2003JD004362
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] We use observed CO2: CO correlations in Asian outflow from the TRACE-P aircraft campaign ( February - April 2001), together with a three-dimensional global chemical transport model (GEOS-CHEM), to constrain specific components of the east Asian CO2 budget including, in particular, Chinese emissions. The CO2/CO emission ratio varies with the source of CO2 ( different combustion types versus the terrestrial biosphere) and provides a characteristic signature of source regions and source type. Observed CO2/CO correlation slopes in east Asian boundary layer outflow display distinct regional signatures ranging from 10 - 20 mol/mol ( outflow from northeast China) to 80 mol/mol ( over Japan). Model simulations using best a priori estimates of regional CO2 and CO sources from Streets et al. [ 2003] ( anthropogenic), the CASA model (biospheric), and Duncan et al. [ 2003] (biomass burning) overestimate CO2 concentrations and CO2/CO slopes in the boundary layer outflow. Constraints from the CO2/CO slopes indicate that this must arise from an overestimate of the modeled regional net biospheric CO2 flux. Our corrected best estimate of the net biospheric source of CO2 from China for March - April 2001 is 3200 Gg C/d, which represents a 45% reduction of the net flux from the CASA model. Previous analyses of the TRACE-P data had found that anthropogenic Chinese CO emissions must be similar to 50% higher than in Streets et al.' s [ 2003] inventory. We find that such an adjustment improves the simulation of the CO2/CO slopes and that it likely represents both an underreporting of sector activity ( domestic and industrial combustion) and an underestimate of CO emission factors. Increases in sector activity would imply increases in Chinese anthropogenic CO2 emissions and would also imply a further reduction of the Chinese biospheric CO2 source to reconcile simulated and observed CO2 concentrations.
引用
收藏
页码:D18S181 / 13
页数:13
相关论文
共 57 条
[1]   Airborne observations of spatial and temporal variability of tropospheric carbon dioxide [J].
Anderson, BE ;
Gregory, GL ;
Collins, JE ;
Sachse, GW ;
Conway, TJ ;
Whiting, GP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D1) :1985-1997
[2]   Emission of trace gases and aerosols from biomass burning [J].
Andreae, MO ;
Merlet, P .
GLOBAL BIOGEOCHEMICAL CYCLES, 2001, 15 (04) :955-966
[3]   Large-scale distribution of CH4 in the western North Pacific:: Sources and transport from the Asian continent -: art. no. 8807 [J].
Bartlett, KB ;
Sachse, GW ;
Slate, T ;
Harward, C ;
Blake, DR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D20)
[4]   Variability in the O-2/N-2 ratio of southern hemisphere air, 1991-1994: Implications for the carbon cycle [J].
Bender, M ;
Ellis, T ;
Tans, P ;
Francey, R ;
Lowe, D .
GLOBAL BIOGEOCHEMICAL CYCLES, 1996, 10 (01) :9-21
[5]   Asian chemical outflow to the Pacific in spring: Origins, pathways, and budgets [J].
Bey, I ;
Jacob, DJ ;
Logan, JA ;
Yantosca, RM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D19) :23097-23113
[6]   NMHCs and halocarbons in Asian continental outflow during the Transport and Chemical Evolution over the Pacific (TRACE-P) Field Campaign: Comparison with PEM-West B [J].
Blake, NJ ;
Blake, DR ;
Simpson, IJ ;
Meinardi, S ;
Swanson, AL ;
Lopez, JP ;
Katzenstein, AS ;
Barletta, B ;
Shirai, T ;
Atlas, E ;
Sachse, G ;
Avery, M ;
Vay, S ;
Fuelberg, HE ;
Kiley, CM ;
Kita, K ;
Rowland, FS .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D20)
[7]   Regional changes in carbon dioxide fluxes of land and oceans since 1980 [J].
Bousquet, P ;
Peylin, P ;
Ciais, P ;
Le Quéré, C ;
Friedlingstein, P ;
Tans, PP .
SCIENCE, 2000, 290 (5495) :1342-1346
[8]   Inverse modeling of annual atmospheric CO2 sources and sinks 1.: Method and control inversion [J].
Bousquet, P ;
Ciais, P ;
Peylin, P ;
Ramonet, M ;
Monfray, P .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D21) :26161-26178
[9]  
BRADSHER K, 2003, NY TIMES 1022
[10]   Evaluating regional emission estimates using the TRACE-P observations [J].
Carmichael, GR ;
Tang, Y ;
Kurata, G ;
Uno, I ;
Streets, DG ;
Thongboonchoo, N ;
Woo, JH ;
Guttikunda, S ;
White, A ;
Wang, T ;
Blake, DR ;
Atlas, E ;
Fried, A ;
Potter, B ;
Avery, MA ;
Sachse, GW ;
Sandholm, ST ;
Kondo, Y ;
Talbot, RW ;
Bandy, A ;
Thorton, D ;
Clarke, AD .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D21)