An evaluation of the performance of chemistry transport models -: Part 2:: Detailed comparison with two selected campaigns

被引:40
作者
Brunner, D [1 ]
Staehelin, J
Rogers, HL
Köhler, MO
Pyle, JA
Hauglustaine, DA
Jourdain, L
Berntsen, TK
Gauss, M
Isaksen, ISA
Meijer, E
van Velthoven, P
Pitari, G
Mancini, E
Grewe, V
Sausen, R
机构
[1] ETH, Inst Atmospher & Climate Sci, Zurich, Switzerland
[2] Univ Cambridge, Ctr Atmospher Sci, Cambridge CB2 1TN, England
[3] Lab Sci Climat & Environm, Gif Sur Yvette, France
[4] Serv Aeron, Paris, France
[5] Univ Oslo, Dept Geosci, Oslo, Norway
[6] Royal Netherlands Meteorol Inst, Sect Atmospher Composit, NL-3730 AE De Bilt, Netherlands
[7] Univ Aquila, Dipartimento Fis, I-67100 Laquila, Italy
[8] DLR, Inst Phys Atmosphare, Wessling, Germany
关键词
D O I
10.5194/acp-5-107-2005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This is the second part of a rigorous model evaluation study involving five global Chemistry-Transport and two Chemistry-Climate Models operated by different groups in Europe. Simulated trace gas fields were interpolated to the exact times and positions of the observations to account for the actual weather conditions and hence for the specific histories of the sampled air masses. In this part of the study we focus on a detailed comparison with two selected campaigns, PEM-Tropics A and SONEX, contrasting the clean environment of the tropical Pacific with the more polluted North Atlantic region. The study highlights the different strengths and weaknesses of the models in accurately simulating key processes in the UT/LS region including stratosphere-troposphere-exchange, rapid convective transport, lightning emissions, radical chemistry and ozone production. Model simulated Radon, which was used as an idealized tracer for continental influence, was occasionally much better correlated with measured CO than simulated CO pointing towards deficiencies in the used biomass burning emission fields. The abundance and variability of HOx radicals is in general well represented in the models as inferred directly from the comparison with measured OH and HO2 and indirectly from the comparison with hydrogen peroxide concentrations. Components of the NOy family such as PAN, HNO3 and NO were found to compare less favorably. Interestingly, models showing good agreement with observations in the case of PEM-Tropics A often failed in the case of SONEX and vice versa. A better description of NOx and NOy emissions, chemistry and sinks is thought to be key to future model improvements with respect to the representation of chemistry in the UT/LS region.
引用
收藏
页码:107 / 129
页数:23
相关论文
共 60 条
[1]  
[Anonymous], 2001, IPCC 3 ASSESSMENT RE
[2]   Time evolution of tropospheric ozone and its radiative forcing [J].
Berntsen, TK ;
Myhre, G ;
Stordal, F ;
Isaksen, ISA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D7) :8915-8930
[3]   Global modeling of tropospheric chemistry with assimilated meteorology: Model description and evaluation [J].
Bey, I ;
Jacob, DJ ;
Yantosca, RM ;
Logan, JA ;
Field, BD ;
Fiore, AM ;
Li, QB ;
Liu, HGY ;
Mickley, LJ ;
Schultz, MG .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D19) :23073-23095
[4]   Chemical characteristics of air from differing source regions during the Pacific Exploratory Mission-Tropics A (PEM-Tropics A) [J].
Board, AS ;
Fuelberg, HE ;
Gregory, GL ;
Heikes, BG ;
Schultz, MG ;
Blake, DR ;
Dibb, JE ;
Sandholm, ST ;
Talbot, RW .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D13) :16181-16196
[5]   European scientific assessment of the atmospheric effects of aircraft emissions [J].
Brasseur, GP ;
Cox, RA ;
Hauglustaine, D ;
Isaksen, I ;
Lelieveld, J ;
Lister, DH ;
Sausen, R ;
Schumann, U ;
Wahner, A ;
Wiesen, P .
ATMOSPHERIC ENVIRONMENT, 1998, 32 (13) :2329-2418
[6]   Chemistry-transport model comparison with ozone observations in the midlatitude lowermost stratosphere [J].
Bregman, A ;
Krol, MC ;
Teyssèdre, H ;
Norton, WA ;
Iwi, A ;
Chipperfield, M ;
Pitari, G ;
Sundet, JK ;
Lelieveld, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D15) :17479-17496
[7]  
Brenninkmeijer CAM, 1999, J ATMOS OCEAN TECH, V16, P1373, DOI 10.1175/1520-0426(1999)016<1373:CCAFGM>2.0.CO
[8]  
2
[9]   An evaluation of the performance of chemistry transport models by comparison with research aircraft observations.: Part 1:: Concepts and overall model performance [J].
Brunner, D ;
Staehelin, J ;
Rogers, HL ;
Köhler, MO ;
Pyle, JA ;
Hauglustaine, D ;
Jourdain, L ;
Berntsen, TK ;
Gauss, M ;
Isaksen, ISA ;
Meijer, E ;
van Velthoven, P ;
Pitari, G ;
Mancini, E ;
Grewe, V ;
Sausen, R .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2003, 3 :1609-1631
[10]   Large-scale nitrogen oxide plumes in the tropopause region and implications for ozone [J].
Brunner, D ;
Staehelin, J ;
Jeker, D .
SCIENCE, 1998, 282 (5392) :1305-1309