Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing, 210044, China
Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing, 210044, China
Kai Meng
Key Laboratory of Meteorology and Ecological Environment of Hebei Province, Hebei Provincial Institute of Meteorological Sciences, Shijiazhuang, 050021, China
Fujian Provincial Key Laboratory of Environmental Engineering, Fujian Academy of Environmental Sciences, Fuzhou, 350011, China
Qingjian Yang
Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing, 210044, China
Yongqing Bai
Hubei Key Laboratory for Heavy Rain Monitoring and Warning Research, Institute of Heavy Rain, China Meteorological Administration, Wuhan, 430205, China
Kai Yang
Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing, 210044, China
Weikang Fu
Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing, 210044, China
Chenghao Tan
State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China
University of Chinese Academy of Sciences, Beijing 100049, China
Yifan Zhang
Xuchang Meteorological Service, Xuchang, 450003, China
Yanzhe Zhang
Ningxia Air Traffic Management Sub-bureau of CAAC, Yinchuan, 750009, China
Zhikuan Li
Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing, 210044, China
Viewed
Total article views: 1,988 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,640
292
56
1,988
142
70
96
HTML: 1,640
PDF: 292
XML: 56
Total: 1,988
Supplement: 142
BibTeX: 70
EndNote: 96
Views and downloads (calculated since 28 Feb 2024)
Cumulative views and downloads
(calculated since 28 Feb 2024)
Total article views: 1,502 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,245
219
38
1,502
107
61
85
HTML: 1,245
PDF: 219
XML: 38
Total: 1,502
Supplement: 107
BibTeX: 61
EndNote: 85
Views and downloads (calculated since 18 Jun 2024)
Cumulative views and downloads
(calculated since 18 Jun 2024)
Total article views: 486 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
395
73
18
486
35
9
11
HTML: 395
PDF: 73
XML: 18
Total: 486
Supplement: 35
BibTeX: 9
EndNote: 11
Views and downloads (calculated since 28 Feb 2024)
Cumulative views and downloads
(calculated since 28 Feb 2024)
Viewed (geographical distribution)
Total article views: 1,988 (including HTML, PDF, and XML)
Thereof 1,988 with geography defined
and 0 with unknown origin.
Total article views: 1,502 (including HTML, PDF, and XML)
Thereof 1,502 with geography defined
and 0 with unknown origin.
Total article views: 486 (including HTML, PDF, and XML)
Thereof 486 with geography defined
and 0 with unknown origin.
We reveal a significant mechanism of stratospheric O3 intrusion (SI) into the atmospheric environment induced by an extratropical cyclone system. This system facilitates the downward transport of stratospheric O3 to the near-surface layer by vertical coupling, involving the upper westerly trough, the middle northeast cold vortex, and the lower extratropical cyclone in the troposphere. On average, stratospheric O3 contributed 26.77 % to near-surface O3 levels over the North China Plain.
We reveal a significant mechanism of stratospheric O3 intrusion (SI) into the atmospheric...
