Response of atmospheric particulate matter to changes in precursor emissions: A comparison of three air quality models

被引:27
作者
Pun, Betty K. [1 ]
Seigneur, Christian [1 ]
Bailey, Elizabeth M. [2 ]
Gautney, Larry L. [2 ]
Douglas, Sharon G. [4 ]
Haney, Jay L. [4 ]
Kumar, Naresh [3 ]
机构
[1] Atmospher & Environm Res Inc, San Ramon, CA USA
[2] Tennessee Valley Author, Muscle Shoals, AL 35660 USA
[3] EPRI, Palo Alto, CA USA
[4] ICF Int, San Rafael, CA USA
关键词
OZONE PRODUCTION; SENSITIVITY; AEROSOLS;
D O I
10.1021/es702333d
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Three mathematical models of air quality (CMAQ, CMAQ-MADRID, and REMSAD) are applied to simulate the response of atmospheric fine particulate matter (PM2.5) concentrations to reductions in the emissions of gaseous precursors for a 10 day period of the July 1999 Southern Oxidants Study (SOS) in Nashville. The models are shown to predict similar directions of the changes in PM2.5 mass and component (sulfate, nitrate, ammonium, and organic compounds) concentrations in response to changes in emissions of sulfur dioxide (SO2), nitrogen oxides (NOx), and volatile organic compounds (VOC), except for the effect Of SO2 reduction on nitrate and the effect of VOC reduction on PM2.5 mass. Furthermore, in many cases where the directional changes are consistent the magnitude of the changes are significantly different among models. Examples are the effects Of SO2 and NO, reductions on nitrate and PM2.5 mass and the effects of VOC reduction on organic compounds, sulfate and nitrate. The spatial resolution significantly influences the results in some cases. Operational model performance for a PM2.5 component appears to provide some useful indication on the reliability of the relative response factors (RRFs) for a change in emissions of a direct precursor, as well as for a change in emissions of a compound that affects this component in an indirect manner, such as via oxidant formation. However, these results need to be confirmed for other conditions and caution is still needed when applying air quality models for the design of emission control strategies. It is advisable to use more than one air quality model (or more than one configuration of a single air quality model) to span the full range of plausible scientific representations of atmospheric processes when investigating future air quality scenarios.
引用
收藏
页码:831 / 837
页数:7
相关论文
共 23 条
[1]   Response of inorganic PM to precursor concentrations [J].
Ansari, AS ;
Pandis, SN .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1998, 32 (18) :2706-2714
[2]   A comparison of the performance of four air quality models for the Southern Oxidants Study episode in July 1999 [J].
Bailey, E. M. ;
Gautney, L. L. ;
Kelsoe, J. J. ;
Jacobs, M. E. ;
Mao, Q. ;
Condrey, J. W. ;
Pun, B. ;
Wu, S. -Y. ;
Seigneur, C. ;
Douglas, S. ;
Haney, J. ;
Kumar, N. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2007, 112 (D5)
[3]   Spatial mapping of VOC and NOx-limitation of ozone formation in central California [J].
Blanchard, CL ;
Fairley, D .
ATMOSPHERIC ENVIRONMENT, 2001, 35 (22) :3861-3873
[4]   Review of the governing equations, computational algorithms, and other components of the models-3 Community Multiscale Air Quality (CMAQ) modeling system [J].
Byun, Daewon ;
Schere, Kenneth L. .
APPLIED MECHANICS REVIEWS, 2006, 59 (1-6) :51-77
[5]  
*EPA, 2006, GUID US MOD OTH ANAL
[6]  
*ICF, 2003, US GUID REG MOD SYST
[7]   Ozone production in the New York City urban plume [J].
Kleinman, LI ;
Daum, PH ;
Imre, DG ;
Lee, JH ;
Lee, YN ;
Nunnermacker, LJ ;
Springston, SR ;
Weinstein-Lloyd, J ;
Newman, L .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D11) :14495-14511
[8]   Sensitivity of ozone production rate to ozone precursors [J].
Kleinman, LI ;
Daum, PH ;
Lee, YN ;
Nunnermacker, LJ ;
Springston, SR ;
Weinstein-Lloyd, J ;
Rudolph, J .
GEOPHYSICAL RESEARCH LETTERS, 2001, 28 (15) :2903-2906
[9]  
McMurry PeterH., 2004, PARTICULATE MATTER S
[10]   Chemical coupling between atmospheric ozone and particulate matter [J].
Meng, Z ;
Dabdub, D ;
Seinfeld, JH .
SCIENCE, 1997, 277 (5322) :116-119