Sensitivity analysis of methane emissions derived from SCIAMACHY observations through inverse modelling

被引:62
作者
Meirink, JF [1 ]
Eskes, HJ [1 ]
Goede, APH [1 ]
机构
[1] Royal Netherlands Meteorol Inst KNMI, Climate Res & Seismol Dept, De Bilt, Netherlands
关键词
D O I
10.5194/acp-6-1275-2006
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
offer a promising method for global verification of emissions and improvement of global emission inventories. Here, an inverse modelling approach based on four-dimensional variational (4D-var) data assimilation is presented and applied to synthetic measurements of atmospheric methane. In this approach, emissions and initial concentrations are optimised simultaneously, thus allowing inversions to be carried out on time scales of weeks to months, short compared with the lifetime of methane. Observing System Simulation Experiments (OSSEs) have been performed to demonstrate the feasibility of the method and to investigate the utility of SCIAMACHY observations for methane source estimation. The impact of a number of parameters on the error in the methane emission field retrieved has been analysed. These parameters include the measurement error, the error introduced by the presence of clouds, and the spatial resolution of the emission field. It is shown that 4D-var is an efficient method to deal with large amounts of satellite data and to retrieve emissions at high resolution. Some important conclusions regarding the SCIAMACHY measurements can be drawn. (i) The observations at their estimated precision of 1.5 to 2% will contribute considerably to uncertainty reduction in monthly, subcontinental (similar to 500 km) methane source strengths. (ii) Systematic measurement errors well below 1% have a dramatic impact on the quality of the derived emission fields. Hence, every effort should be made to identify and remove such systematic errors. (iii) It is essential to take partly cloudy pixels into account in order to achieve sufficient spatial coverage. (iv) The uncertainty in measured cloud parameters may at some point become the limiting factor for methane emission retrieval, rather than the uncertainty in measured methane itself.
引用
收藏
页码:1275 / 1292
页数:18
相关论文
共 52 条
[1]  
ATLAS R, 1997, IMPACT VARIOUS OBSER, P155
[2]   Inverse modelling of national and European CH4 emissions using the atmospheric zoom model TM5 [J].
Bergamaschi, P ;
Krol, M ;
Dentener, F ;
Vermeulen, A ;
Meinhardt, F ;
Graul, R ;
Ramonet, M ;
Peters, W ;
Dlugokencky, EJ .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :2431-2460
[3]  
Bovensmann H, 1999, J ATMOS SCI, V56, P127, DOI 10.1175/1520-0469(1999)056<0127:SMOAMM>2.0.CO
[4]  
2
[5]   On the use of mass-conserving wind fields in chemistry-transport models [J].
Bregman, B ;
Segers, A ;
Krol, M ;
Meijer, E ;
van Velthoven, P .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2003, 3 :447-457
[6]   Atmospheric methane and carbon dioxide from SCIAMACHY satellite data:: initial comparison with chemistry and transport models [J].
Buchwitz, M ;
de Beek, R ;
Burrows, JP ;
Bovensmann, H ;
Warneke, T ;
Notholt, J ;
Meirink, JF ;
Goede, APH ;
Bergamaschi, P ;
Körner, S ;
Heimann, M ;
Schulz, A .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :941-962
[7]   Mass balance inverse modelling of methane in the 1990s using a Chemistry Transport Model [J].
Butler, TM ;
Simmonds, I ;
Rayner, PJ .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2004, 4 :2561-2580
[8]  
Chen Y.-H., 2003, THESIS MIT CAMBRIDGE
[9]   Trace gas measurements from infrared satellite for chemistry and climate applications [J].
Clerbaux, C ;
Hadji-Lazaro, J ;
Turquety, S ;
Mégie, G ;
Coheur, PF .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2003, 3 :1495-1508
[10]   A STRATEGY FOR OPERATIONAL IMPLEMENTATION OF 4D-VAR, USING AN INCREMENTAL APPROACH [J].
COURTIER, P ;
THEPAUT, JN ;
HOLLINGSWORTH, A .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1994, 120 (519) :1367-1387