Articles | Volume 23, issue 7
https://doi.org/10.5194/acp-23-4343-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-23-4343-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High frequency of new particle formation events driven by summer monsoon in the central Tibetan Plateau, China
Lizi Tang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Collaborative Innovation Center of Atmospheric Environment and
Equipment Technology, Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control, Nanjing University of Information Science
& Technology, Nanjing, 210044, China
Dongjie Shang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Xin Fang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Jianjiong Mao
Collaborative Innovation Center of Atmospheric Environment and
Equipment Technology, Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control, Nanjing University of Information Science
& Technology, Nanjing, 210044, China
Wanyun Xu
State Key Laboratory of Severe Weather & Key Laboratory for
Atmospheric Chemistry of CMA, Institute of Atmospheric Composition, Chinese
Academy of Meteorological Sciences, Beijing, 100081, China
Jiacheng Zhou
Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics
and Fine Mechanisms, HFIPS, Chinese Academy of Science, Hefei, 230031, Anhui,
China
Weixiong Zhao
Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics
and Fine Mechanisms, HFIPS, Chinese Academy of Science, Hefei, 230031, Anhui,
China
Yaru Wang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Chong Zhang
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Yingjie Zhang
School of Ecology and Nature Conservation, Beijing Forestry
University, Beijing, 100083, China
Jianlin Hu
Collaborative Innovation Center of Atmospheric Environment and
Equipment Technology, Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control, Nanjing University of Information Science
& Technology, Nanjing, 210044, China
Limin Zeng
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Collaborative Innovation Center of Atmospheric Environment and
Equipment Technology, Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control, Nanjing University of Information Science
& Technology, Nanjing, 210044, China
Chunxiang Ye
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Collaborative Innovation Center of Atmospheric Environment and
Equipment Technology, Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control, Nanjing University of Information Science
& Technology, Nanjing, 210044, China
Zhijun Wu
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, International Joint Laboratory for Regional Pollution Control,
Ministry of Education (IJRC), College of Environmental Sciences and
Engineering, Peking University, Beijing, 100871, China
Collaborative Innovation Center of Atmospheric Environment and
Equipment Technology, Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control, Nanjing University of Information Science
& Technology, Nanjing, 210044, China
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Cited
2 citations as recorded by crossref.
- Organic aerosols in the inland Tibetan Plateau: New insights from molecular tracers X. Wan et al. 10.1016/j.scitotenv.2023.163797
- Key characteristics of new particle formation events occurring simultaneously in the Yangtze River Delta and northeast rural sites in China S. Liu et al. 10.1016/j.atmosenv.2024.120406
2 citations as recorded by crossref.
- Organic aerosols in the inland Tibetan Plateau: New insights from molecular tracers X. Wan et al. 10.1016/j.scitotenv.2023.163797
- Key characteristics of new particle formation events occurring simultaneously in the Yangtze River Delta and northeast rural sites in China S. Liu et al. 10.1016/j.atmosenv.2024.120406
Latest update: 22 Nov 2024
Short summary
There was an evident distinction in the frequency of new particle formation (NPF) events at Nam Co station on the Tibetan Plateau: 15 % in pre-monsoon season and 80 % in monsoon season. The frequent NPF events in monsoon season resulted from the higher frequency of southerly air masses, which brought the organic precursors to participate in the NPF process. It increased the amount of aerosol and CCN compared with those in pre-monsoon season, which may markedly affect earth's radiation balance.
There was an evident distinction in the frequency of new particle formation (NPF) events at Nam...
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