An ensemble data assimilation system to estimate CO2 surface fluxes from atmospheric trace gas observations -: art. no. D24304

被引:164
作者
Peters, W
Miller, JB
Whitaker, J
Denning, AS
Hirsch, A
Krol, MC
Zupanski, D
Bruhwiler, L
Tans, PP
机构
[1] NOAA, Global Monitoring Div, Earth Syst Res Lab, Boulder, CO 80302 USA
[2] Cooperat Inst Res Environm Sci, Boulder, CO USA
[3] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[4] SRON Netherlands Inst Space Res, NL-3584 CA Utrecht, Netherlands
关键词
D O I
10.1029/2005JD006157
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] We present a data assimilation system to estimate surface fluxes of CO2 and other trace gases from observations of their atmospheric abundances. The system is based on ensemble data assimilation methods under development for Numerical Weather Prediction (NWP) and is the first of its kind to be used for CO2 flux estimation. The system was developed to overcome computational limitations encountered when a large number of observations are used to estimate a large number of unknown surface fluxes. The ensemble data assimilation approach is attractive because it returns an approximation of the covariance, does not need an adjoint model or other linearization of the observation operator, and offers the possibility to optimize fluxes of chemically active trace gases (e.g., CH4, CO) in the same framework. We assess the performance of this new system in a pseudodata experiment that resembles the real problem we will apply this system to. The sensitivity of the method to the choice of several parameters such as the assimilation window size and the number of ensemble members is investigated. We conclude that the system is able to provide satisfactory flux estimates for the relatively large scales resolved by our current observing network and that the loss of information in the approximated covariances is an acceptable price to pay for the efficient computation of a large number of surface fluxes. The full potential of this data assimilation system will be used for near - real time operational estimates of North American CO2 fluxes. This will take advantage of the large amounts of atmospheric data that will be collected by NOAA-CMDL in conjunction with the implementation of the North American Carbon Program (NACP).
引用
收藏
页码:1 / 18
页数:21
相关论文
共 58 条
[1]   A 1 degrees x1 degrees distribution of carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1950-1990 [J].
Andres, RJ ;
Marland, G ;
Fung, I ;
Matthews, E .
GLOBAL BIOGEOCHEMICAL CYCLES, 1996, 10 (03) :419-429
[2]  
[Anonymous], [No title captured]
[3]  
[Anonymous], ATMOSPHERIC CHEM PHY
[4]   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
[5]  
Brenkert A. L., 1998, CARBON DIOXIDE EMISS
[6]  
BRUHWILER L, 2005, ATMOS CHEM PHYS DISC, V5, P1891
[7]   PARTITIONING OF OCEAN AND LAND UPTAKE OF CO2 AS INFERRED BY DELTA-C-13 MEASUREMENTS FROM THE NOAA CLIMATE MONITORING AND DIAGNOSTICS LABORATORY GLOBAL AIR SAMPLING NETWORK [J].
CIAIS, P ;
TANS, PP ;
WHITE, JWC ;
TROLIER, M ;
FRANCEY, RJ ;
BERRY, JA ;
RANDALL, DR ;
SELLERS, PJ ;
COLLATZ, JG ;
SCHIMEL, DS .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D3) :5051-5070
[8]  
COHN SE, 1994, MON WEATHER REV, V122, P2838, DOI 10.1175/1520-0493(1994)122<2838:AFLKSF>2.0.CO
[9]  
2
[10]   EVIDENCE FOR INTERANNUAL VARIABILITY OF THE CARBON-CYCLE FROM THE NATIONAL-OCEANIC-AND-ATMOSPHERIC-ADMINISTRATION CLIMATE-MONITORING-AND-DIAGNOSTICS-LABORATORY GLOBAL-AIR-SAMPLING-NETWORK [J].
CONWAY, TJ ;
TANS, PP ;
WATERMAN, LS ;
THONING, KW .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D11) :22831-22855