Articles | Volume 17, issue 23
https://doi.org/10.5194/acp-17-14275-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/acp-17-14275-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
01 Dec 2017
Research article |
| 01 Dec 2017
| 01 Dec 2017
Observations of the vertical distributions of summertime atmospheric pollutants and the corresponding ozone production in Shanghai, China
Chengzhi Xing
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China
Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Anhui Province Key Laboratory of Polar Environment and Global Change, USTC, Hefei, 230026, China
Shanshan Wang
CORRESPONDING AUTHOR
Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP), Department of Environmental Science and Engineering, Fudan University, Shanghai, 200433, China
Ka Lok Chan
CORRESPONDING AUTHOR
Meteorological Institute, Ludwig-Maximilians-Universität München, Munich, Germany
College of Environmental Science and Engineering, Ocean University of China, Qingdao, 266100, China
Xin Huang
School of Atmospheric Sciences, Nanjing University, Nanjing, 210093, China
Wenjing Su
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China
Chengxin Zhang
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China
Yunsheng Dong
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Guangqiang Fan
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Tianshu Zhang
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Zhenyi Chen
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Qihou Hu
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Hang Su
Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China
Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, 55020, Germany
Zhouqing Xie
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China
Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
Anhui Province Key Laboratory of Polar Environment and Global Change, USTC, Hefei, 230026, China
Jianguo Liu
Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, 230031, China
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Latest update: 05 Dec 2025
Short summary
Vertical profiles of the aerosol extinction coefficient and NO2 and HCHO concentrations were retrieved from MAX-DOAS measurement, while vertical distribution of O3 was obtained using ozone lidar. The measured O3 vertical distribution indicates that the ozone production not only occurs at surface level but also at higher altitudes (about 1.1 km), which are not directly related to horizontal and vertical transportation but are mainly influenced by the abundance of VOCs in the lower troposphere.
Vertical profiles of the aerosol extinction coefficient and NO2 and HCHO concentrations were...
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