Key Laboratory of Transportation Meteorology of China Meteorological Administration, Nanjing Joint Institute for Atmospheric Sciences, Nanjing 210041, China
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Key Laboratory for Aerosol-Cloud-Precipitation of
China Meteorological Administration, Key Laboratory of Meteorological
Disaster, Ministry of Education (KLME), Special Test Field of National
Integrated Meteorological Observation, Nanjing University of Information
Science and Technology, Nanjing 210044, China
Shuangshuang Shi
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Key Laboratory for Aerosol-Cloud-Precipitation of
China Meteorological Administration, Key Laboratory of Meteorological
Disaster, Ministry of Education (KLME), Special Test Field of National
Integrated Meteorological Observation, Nanjing University of Information
Science and Technology, Nanjing 210044, China
Wen Lu
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Key Laboratory for Aerosol-Cloud-Precipitation of
China Meteorological Administration, Key Laboratory of Meteorological
Disaster, Ministry of Education (KLME), Special Test Field of National
Integrated Meteorological Observation, Nanjing University of Information
Science and Technology, Nanjing 210044, China
Plateau Atmosphere and Environment Key Laboratory of Sichuan Province, School of Atmospheric Sciences, Chengdu University of Information
Technology, Chengdu 610225, China
Hanqing Kang
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Key Laboratory for Aerosol-Cloud-Precipitation of
China Meteorological Administration, Key Laboratory of Meteorological
Disaster, Ministry of Education (KLME), Special Test Field of National
Integrated Meteorological Observation, Nanjing University of Information
Science and Technology, Nanjing 210044, China
Key Laboratory of Transportation Meteorology of China Meteorological Administration, Nanjing Joint Institute for Atmospheric Sciences, Nanjing 210041, China
Viewed
Total article views: 3,023 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,126
819
78
3,023
98
109
HTML: 2,126
PDF: 819
XML: 78
Total: 3,023
BibTeX: 98
EndNote: 109
Views and downloads (calculated since 14 Nov 2022)
Cumulative views and downloads
(calculated since 14 Nov 2022)
Total article views: 2,084 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,590
431
63
2,084
88
94
HTML: 1,590
PDF: 431
XML: 63
Total: 2,084
BibTeX: 88
EndNote: 94
Views and downloads (calculated since 05 May 2023)
Cumulative views and downloads
(calculated since 05 May 2023)
Total article views: 939 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
536
388
15
939
10
15
HTML: 536
PDF: 388
XML: 15
Total: 939
BibTeX: 10
EndNote: 15
Views and downloads (calculated since 14 Nov 2022)
Cumulative views and downloads
(calculated since 14 Nov 2022)
Viewed (geographical distribution)
Total article views: 3,023 (including HTML, PDF, and XML)
Thereof 3,023 with geography defined
and 0 with unknown origin.
Total article views: 2,084 (including HTML, PDF, and XML)
Thereof 2,084 with geography defined
and 0 with unknown origin.
Total article views: 939 (including HTML, PDF, and XML)
Thereof 939 with geography defined
and 0 with unknown origin.
We analyze ozone response to aerosol mixing states in the vertical direction by WRF-Chem simulations. Aerosols generally lead to turbulent suppression, precursor accumulation, low-level photolysis reduction, and upper-level photolysis enhancement under different underlying surface and pollution conditions. Thus, ozone decreases within the entire boundary layer during the daytime, and the decrease is the least in aerosol external mixing states compared to internal and core shell mixing states.
We analyze ozone response to aerosol mixing states in the vertical direction by WRF-Chem...
