globalchange  > 气候变化与战略
DOI: 10.1016/j.atmosenv.2019.117162
论文题名:
Vertical structure and interaction of ozone and fine particulate matter in spring at Nanjing, China: The role of aerosol's radiation feedback
作者: Qu Y.; Wang T.; Wu H.; Shu L.; Li M.; Chen P.; Zhao M.; Li S.; Xie M.; Zhuang B.; Liu J.; Han Y.
刊名: Atmospheric Environment
ISSN: 1352-2310
出版年: 2020
卷: 222
语种: 英语
英文关键词: Aerosols ; Atmospheric chemistry ; Atmospheric structure ; Boundary layers ; Chemical analysis ; Feedback ; Light extinction ; Optical radar ; Ozone ; Ozone layer ; Photolysis ; Surface measurement ; Weather forecasting ; Wind ; Aerosol extinction coefficient ; Atmospheric stability ; Fine particulate matter ; Ground-based lidars ; Nanjing ; Short-wave radiation ; Vertical distributions ; Weather research and forecasting ; Particles (particulate matter) ; ozone ; aerosol ; atmospheric chemistry ; boundary layer ; concentration (composition) ; lidar ; measurement method ; ozone ; particulate matter ; shortwave radiation ; spring (season) ; top of atmosphere ; troposphere ; vertical distribution ; aerosol ; aerosol radiation feedback ; air quality ; boundary layer ; China ; environmental temperature ; forecasting ; particulate matter ; priority journal ; radiation related phenomena ; solar radiation ; spring ; surface property ; troposphere ; wind speed ; Nanjing [Jiangsu]
学科: Aerosol ; Lidar ; Nanjing ; Ozone ; Surface measurement
中文摘要: The vertical structure of ozone (O3) and fine particulate matter (FPM) as well as their interactions are important for understanding the atmospheric chemistry process and their impact on climate. Through a ground-based lidar observation during April 18th-May 22nd 2017 and surface measurement during March 1st-May 31st 2017, this study obtained the vertical distribution of O3 and aerosol extinction coefficient with their correlations during the springtime in the lower troposphere (LT) in Nanjing, eastern China. Surface average O3 and PM2.5 concentrations in spring were 39.89 ppb and 41.93 μg m−3. O3 generally increased with height in the LT, while aerosol extinction coefficient decreased. The correlation between O3 and aerosol extinction coefficient was −0.32 at 300 m, and 0.34 at 1747.5 m. An on-line coupled model Weather Research and Forecasting with Chemistry (WRF-Chem) was used to analyze the effect of aerosol's radiation feedback on ozone. Aerosol reduced the surface downward shortwave radiation by −25.66 W m−2, and increased the upwelling shortwave radiation at the top of atmosphere by 3.19 W m−2 in urban Nanjing. The photolysis rate of NO2 and O1D were reduced by −1% and −0.7% near surface and increased by 0.3% and 0.2% at upper LT. Aerosol-included effect also led to a more stable planet boundary layer (PBL), with −0.24 °C and −0.05 m s−1 changes in temperature and wind speed at surface. However, the temperature and wind speed increased by 0.18 °C and 0.13 m s−1 at 1760 m, respectively. O3 decreased by −3.70% at surface and increased by 0.89% at 2870 m. This study showed that aerosol can affect ozone through altering photolysis rate and atmospheric stability. Aerosol's radiation feedback has a complex effect on the vertical structure of ozone, which leads to ozone decrease near the surface and increase above the aerosol layer. © 2019 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/161049
Appears in Collections:气候变化与战略

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作者单位: School of Atmospheric Sciences, Nanjing University, Nanjing, 210023, China; School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, 510275, China

Recommended Citation:
Qu Y.,Wang T.,Wu H.,et al. Vertical structure and interaction of ozone and fine particulate matter in spring at Nanjing, China: The role of aerosol's radiation feedback[J]. Atmospheric Environment,2020-01-01,222
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