Inverse modeling of European CH4 emissions 2001-2006

被引:95
作者
Bergamaschi, P. [1 ]
Krol, M. [4 ,10 ,11 ]
Meirink, J. F. [6 ]
Dentener, F. [1 ]
Segers, A. [1 ]
van Aardenne, J. [1 ]
Monni, S. [1 ]
Vermeulen, A. T. [9 ]
Schmidt, M. [8 ]
Ramonet, M. [8 ]
Yver, C. [8 ]
Meinhardt, F. [5 ]
Nisbet, E. G. [3 ]
Fisher, R. E. [3 ]
O'Doherty, S. [7 ]
Dlugokencky, E. J. [2 ]
机构
[1] European Commiss, Inst Environm & Sustainabil, Joint Res Ctr, I-21027 Ispra, Italy
[2] NOAA, Global Monitoring Div, Earth Syst Res Lab, Boulder, CO 80305 USA
[3] Univ London, Dept Earth Sci, Egham TW20 0EX, Surrey, England
[4] SRON Netherlands Inst Space Res, NL-3584 Utrecht, Netherlands
[5] Umweltbundesamt, D-79199 Kirchzarten, Germany
[6] Royal Netherlands Meteorol Inst, Climate & Seismol Dept, NL-3732 GK De Bilt, Netherlands
[7] Univ Bristol, Sch Chem, Bristol BS8 1TS, Avon, England
[8] Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France
[9] Energy Res Ctr Netherlands, Dept Biomass Coal & Environm, NL-1755 ZG Petten, Netherlands
[10] Univ Wageningen & Res Ctr, Wageningen, Netherlands
[11] Inst Marine & Atmospher Res Utrecht, Utrecht, Netherlands
关键词
ATMOSPHERIC METHANE; GREENHOUSE GASES; HISTORY; AREAS;
D O I
10.1029/2010JD014180
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
European CH4 emissions are estimated for the period 2001-2006 using a four-dimensional variational (4DVAR) inverse modeling system, based on the atmospheric zoom model TM5. Continuous observations are used from various European monitoring stations, complemented by European and global flask samples from the NOAA/ESRL network. The available observations mainly provide information on the emissions from northwest Europe (NWE), including the UK, Ireland, the BENELUX countries, France and Germany. The inverse modeling estimates for the total anthropogenic emissions from NWE are 21% higher compared to the EDGARv4.0 emission inventory and 40% higher than values reported to U.N. Framework Convention on Climate Change. Assuming overall uncertainties on the order of 30% for both bottom-up and top-down estimates, all three estimates can be still considered to be consistent with each other. However, the uncertainties in the uncertainty estimates prevent us from verifying (or falsifying) the bottom-up inventories in a strict sense. Sensitivity studies show some dependence of the derived spatial emission patterns on the set of atmospheric monitoring stations used, but the total emissions for the NWE countries appear to be relatively robust. While the standard inversions include a priori information on the spatial and temporal emission patterns from bottom-up inventories, a further sensitivity inversion without this a priori information results in very similar NWE country totals, demonstrating that the available observations provide significant constraints on the emissions from the NWE countries independent from bottom-up inventories.
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页数:18
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