Jiangsu Key Laboratory of Atmospheric Environment Monitoring and
Pollution Control, Collaborative Innovation Center of Atmospheric
Environment and Equipment Technology, School of Environmental Science and
Engineering, Nanjing University of Information Science and Technology,
Nanjing 210044, China
Guoshuai Zhang
Chinese Academy of Environmental Planning, Beijing 100012, China
Jiali Luo
Key Laboratory for Semi-Arid Climate Change of the Ministry of
Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou
730000, China
Shichang Kang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000,
China
University of Chinese Academy of Sciences, Beijing 100049, China
Department of Earth and Atmospheric Sciences, Saint Louis
University, St. Louis, MO 63108, USA
Junhua Yang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000,
China
Zhenming Ji
School of Atmospheric Sciences, Key Laboratory for Climate Change
and Natural Disaster Studies of and Guangdong Province, Sun Yat-sen
University, Guangzhou 510275, China
State Key Laboratory of Tibetan Plateau Earth System, Environment
and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese
Academy of Sciences, Beijing 100101, China
Research Institute for Sustainability – Helmholtz Centre Potsdam (RIFS), 14467 Potsdam, Germany
Ping Li
University of Chinese Academy of Sciences, Beijing 100049, China
Key Laboratory of Land Surface Process and Climate Change in Cold
and Arid Regions, Northwest Institute of Eco-Environment and Resources,
Chinese Academy of Sciences, Lanzhou 730000, China
Key Laboratory of Land Surface Process and Climate Change in Cold
and Arid Regions, Northwest Institute of Eco-Environment and Resources,
Chinese Academy of Sciences, Lanzhou 730000, China
State Key Laboratory of Tibetan Plateau Earth System, Environment
and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese
Academy of Sciences, Beijing 100101, China
Viewed
Total article views: 4,679 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,569
987
123
4,679
331
97
164
HTML: 3,569
PDF: 987
XML: 123
Total: 4,679
Supplement: 331
BibTeX: 97
EndNote: 164
Views and downloads (calculated since 01 Nov 2022)
Cumulative views and downloads
(calculated since 01 Nov 2022)
Total article views: 2,994 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,288
609
97
2,994
172
84
138
HTML: 2,288
PDF: 609
XML: 97
Total: 2,994
Supplement: 172
BibTeX: 84
EndNote: 138
Views and downloads (calculated since 11 Sep 2023)
Cumulative views and downloads
(calculated since 11 Sep 2023)
Total article views: 1,685 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,281
378
26
1,685
159
13
26
HTML: 1,281
PDF: 378
XML: 26
Total: 1,685
Supplement: 159
BibTeX: 13
EndNote: 26
Views and downloads (calculated since 01 Nov 2022)
Cumulative views and downloads
(calculated since 01 Nov 2022)
Viewed (geographical distribution)
Total article views: 4,679 (including HTML, PDF, and XML)
Thereof 4,658 with geography defined
and 21 with unknown origin.
Total article views: 2,994 (including HTML, PDF, and XML)
Thereof 2,964 with geography defined
and 30 with unknown origin.
Total article views: 1,685 (including HTML, PDF, and XML)
Thereof 1,685 with geography defined
and 0 with unknown origin.
The monthly mean surface ozone concentrations peaked earlier in the south in April and May and later in the north in June and July over the Tibetan Plateau. The migration of monthly surface ozone peaks was coupled with the synchronous movement of tropopause folds and the westerly jet that created conditions conducive to stratospheric ozone intrusion. Stratospheric ozone intrusion significantly contributed to surface ozone across the Tibetan Plateau.
The monthly mean surface ozone concentrations peaked earlier in the south in April and May and...
