Analysis of ozone and VOCs measured in Shanghai: A case study

被引:112
作者
Geng, Fuhai
Zhao, Chunsheng [1 ]
Tang, Xu
Lu, Guoliang
Tie, Xuexi
机构
[1] Peking Univ, Dept Atmospher Sci, Sch Phys, Beijing 100871, Peoples R China
[2] Shanghai Meteorol Bur, Shanghai, Peoples R China
[3] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
基金
中国国家自然科学基金; 美国国家科学基金会;
关键词
VOCs; ozone; Shanghai; WRF-Chem;
D O I
10.1016/j.atmosenv.2006.09.023
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Shanghai Meteorological Administration has established a volatile organic compounds (VOCs) laboratory and an observational network for VOCs and ozone (O-3) measurements in the city of Shanghai. In this study, the measured VOCs and O-3 concentrations from 15 November (15-Nov) to 26 November (26-Nov) of 2005 in Shanghai show that there are strong day-to-day and diurnal variations. The measured O-3 and VOCs concentrations have very different characterizations between the two periods. During 15-Nov to 21-Nov (defined as the first period), VOCs and 03 concentrations are lower than the values during 22-Nov to 28-Nov (defined as the second period). There is a strong diurnal variation Of O-3 during the second period with maximum concentrations of 40-80 ppbv at noontime, and minimum concentrations at nighttime. By contrast, during the first period, the diurnal variation Of O-3 is in an irregular pattern with maximum concentrations of only 20-30 ppbv. The VOC concentrations change rapidly from 30-50 ppbv during the first period to 80-100 ppbv during the second period. Two chemical models are applied to interpret the measurements. One model is a regional chemical/ dynamical model (WRIF-Chem) and another is a detailed chemical mechanism model (NCAR MM). Model analysis shows that the meteorological conditions are very different between the two periods, and are mainly responsible for the different chemical characterizations Of O-3 and VOCs between the two periods. During the first period, meteorological conditions are characterized by cloudy sky and high-surface winds in Shanghai, resulting in a higher nighttime planetary boundary layer (PBL) and faster transport of air pollutants. By contrast, during the second period, the meteorological conditions are characterized by clear sky and weak surface winds, resulting in a lower nighttime PBL and slower transport of air pollutants. The chemical mechanism model calculation shows that different VOC species has very different contributions to the high-ozone concentrations during the second period. Alkane (40 ppbv) and aromatic (30 ppbv) are among the highest VOC concentrations observed in Shanghai. The analysis suggests that the aromatic is a main contributor for the O-3 chemical production in Shanghai, with approximately 79% of the O-3 being produced by aromatic. This analysis implies that future increase in VOC (especially aromatic) emissions could lead to significant increase in 03 concentrations in Shanghai. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:989 / 1001
页数:13
相关论文
共 28 条
[1]  
[Anonymous], ATMOS CHEM PHYS DISC
[2]   Evaluated kinetic and photochemical data for atmospheric chemistry: Supplement VIII, halogen species - IUPAC Subcommittee on Gas Kinetic Data Evaluation for Atmospheric Chemistry [J].
Atkinson, R ;
Baulch, DL ;
Cox, RA ;
Hampson, RF ;
Kerr, JA ;
Rossi, MJ ;
Troe, J .
JOURNAL OF PHYSICAL AND CHEMICAL REFERENCE DATA, 2000, 29 (02) :167-266
[3]   TIME-DEPENDENT PHOTOCHEMICAL MODEL FOR OZONE NEAR GROUND [J].
CHAMEIDES, WL ;
WALKER, JCG .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS AND ATMOSPHERES, 1976, 81 (03) :413-420
[4]  
Chang J. S., 1989, 4 NAT AC PREC ASS PR
[5]   Kinetics of HO2+HO2→H2O2+O2:: Implications for stratospheric H2O2 -: art. no. 1299 [J].
Christensen, LE ;
Okumura, M ;
Sander, SP ;
Salawitch, RJ ;
Toon, GC ;
Sen, B ;
Blavier, JF ;
Jucks, KW .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (09) :13-1
[6]  
CRUTZEN PJ, 1975, GARP PUBLICATIONS SE, V16, P236
[7]  
DEMORE WB, 2000, JPL PUBLICATIONS
[8]   Fully coupled "online" chemistry within the WRF model [J].
Grell, GA ;
Peckham, SE ;
Schmitz, R ;
McKeen, SA ;
Frost, G ;
Skamarock, WC ;
Eder, B .
ATMOSPHERIC ENVIRONMENT, 2005, 39 (37) :6957-6975
[9]   A global simulation of tropospheric ozone and related tracers: Description and evaluation of MOZART, version 2 [J].
Horowitz, LW ;
Walters, S ;
Mauzerall, DL ;
Emmons, LK ;
Rasch, PJ ;
Granier, C ;
Tie, XX ;
Lamarque, JF ;
Schultz, MG ;
Tyndall, GS ;
Orlando, JJ ;
Brasseur, GP .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D24)
[10]   Progress in developing an ANN model for air pollution index forecast [J].
Jiang, DH ;
Zhang, Y ;
Hu, X ;
Zeng, Y ;
Tan, HG ;
Shao, DM .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (40) :7055-7064