Modeling study on the air quality impacts from emission reductions and atypical meteorological conditions during the 2008 Beijing Olympics

被引:93
作者
Xing, Jia [1 ,2 ,3 ]
Zhang, Yang [3 ]
Wang, Shuxiao [1 ,2 ]
Liu, Xiaohuan [4 ]
Cheng, Shuhui [4 ]
Zhang, Qiang [5 ]
Chen, Yaosheng [3 ]
Streets, David G. [5 ]
Jang, Carey [6 ]
Hao, Jiming [1 ,2 ]
Wang, Wenxing [4 ]
机构
[1] Tsinghua Univ, Dept Environm Sci & Engn, Beijing 100084, Peoples R China
[2] Tsinghua Univ, State Key Joint Lab Environm Simulat & Pollut Con, Beijing 100084, Peoples R China
[3] N Carolina State Univ, Raleigh, NC 27695 USA
[4] Shandong Univ, Jinan 250100, Shandong, Peoples R China
[5] Argonne Natl Lab, Argonne, IL 60439 USA
[6] US EPA, Res Triangle Pk, NC 27711 USA
关键词
Beijing Olympics; Emission control; CMAQ; Process analysis; Sensitivity simulation; PARTICULATE MATTER; OZONE; SENSITIVITY; POLLUTION; PM2.5; CHINA;
D O I
10.1016/j.atmosenv.2011.01.025
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding of the relative impacts of emission reductions and meteorological variations on air quality during the 2008 Beijing Olympics has an important policy implication. In this work, detailed process analyses and sensitivity simulations under different emission and meteorology scenarios were conducted using CMAQ and the Process Analysis tool to quantify the air quality benefits from emission reductions and meteorological variations in August 2008. The results indicate that emission-driven changes dominate surface concentration reductions of SO2, NO2. VOCs, daily maxima O-3 and PM2.5 by -11% to -83%. The effect of meteorology-driven changes on species concentrations can be either ways (by -46% to 105%) at different locations. The dominant processes contributing to O-3, PM2.5, SO42-, NO3-, and secondary organic aerosol (SOA) are identified. Gas-phase chemistry is a major process for O-3 production, and PM processes are dominant sources for PM2.5 in the planetary boundary layer (PBL). The reduced emissions weaken the source contributions of gas-phase chemistry to O-3 and those of PM processes to PM2.5, with weaker vertical mixing processes and horizontal transport in the PBL Compared with 2007, 2008 has a higher humidity, lower temperature and more precipitation that benefit O-3 reduction within the PBL, and a weaker vertical mixing that disbenefits reductions of all pollutants concentrations. Stronger process contributions of cloud processes (e.g., below- and in-cloud scavenging, and wet deposition) in 2008 help reduce concentrations of PM2.5, NO3-, and SOA, but they (e.g., aqueous-phase chemistry) enhance surface SO42- concentrations. Smaller process contributions of aerosol processes help reduce the concentrations of SOA and SO42- but enhance NO3- and PM2.5 in lower layers (1-6) due to the evaporation of NO3-. The ratios of P-H2O2/P-HNO3 increase under the controlled simulation, indicating that the emission control actions enforced during the 2008 Olympics weakened the sensitivity of O-3 chemistry to VOC emissions in urban areas. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1786 / 1798
页数:13
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