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
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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...
