Articles | Volume 21, issue 13
https://doi.org/10.5194/acp-21-9995-2021
© Author(s) 2021. 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-21-9995-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Impact of aerosol–radiation interaction on new particle formation
Gang Zhao
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
Yishu Zhu
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
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
Taomou Zong
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
Jingchuan Chen
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
Tianyi Tan
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
Haichao 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
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
Keding Lu
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
Chunsheng Zhao
Department of Atmospheric and Oceanic Sciences, School of Physics, 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
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Cited
8 citations as recorded by crossref.
- Parameterization of the ambient aerosol refractive index with source appointed chemical compositions G. Zhao et al. 10.1016/j.scitotenv.2022.156573
- Vigorous New Particle Formation Above Polluted Boundary Layer in the North China Plain S. Lai et al. 10.1029/2022GL100301
- Particle Number Size Distribution of Wintertime Alpine Aerosols and Their Activation as Cloud Condensation Nuclei in the Guanzhong Plain, Northwest China Y. Chen et al. 10.1029/2022JD037877
- Aerosol Optical Depth Retrieval for Sentinel-2 Based on Convolutional Neural Network Method J. Jiang et al. 10.3390/atmos14091400
- Ambient ultrafine particle (PM0.1): Sources, characteristics, measurements and exposure implications on human health S. Abdillah & Y. Wang 10.1016/j.envres.2022.115061
- Vertical Profiles of Particle Number Size Distribution and Variation Characteristics at the Eastern Slope of the Tibetan Plateau C. Shu et al. 10.3390/rs15225363
- Formation mechanism of typical aromatic sulfuric anhydrides and their potential role in atmospheric nucleation process H. Zhang et al. 10.1016/j.jes.2022.01.015
- A theoretical study on the formation mechanism of carboxylic sulfuric anhydride and its potential role in new particle formation H. Zhang et al. 10.1039/D2RA00226D
8 citations as recorded by crossref.
- Parameterization of the ambient aerosol refractive index with source appointed chemical compositions G. Zhao et al. 10.1016/j.scitotenv.2022.156573
- Vigorous New Particle Formation Above Polluted Boundary Layer in the North China Plain S. Lai et al. 10.1029/2022GL100301
- Particle Number Size Distribution of Wintertime Alpine Aerosols and Their Activation as Cloud Condensation Nuclei in the Guanzhong Plain, Northwest China Y. Chen et al. 10.1029/2022JD037877
- Aerosol Optical Depth Retrieval for Sentinel-2 Based on Convolutional Neural Network Method J. Jiang et al. 10.3390/atmos14091400
- Ambient ultrafine particle (PM0.1): Sources, characteristics, measurements and exposure implications on human health S. Abdillah & Y. Wang 10.1016/j.envres.2022.115061
- Vertical Profiles of Particle Number Size Distribution and Variation Characteristics at the Eastern Slope of the Tibetan Plateau C. Shu et al. 10.3390/rs15225363
- Formation mechanism of typical aromatic sulfuric anhydrides and their potential role in atmospheric nucleation process H. Zhang et al. 10.1016/j.jes.2022.01.015
- A theoretical study on the formation mechanism of carboxylic sulfuric anhydride and its potential role in new particle formation H. Zhang et al. 10.1039/D2RA00226D
Latest update: 20 Nov 2024
Short summary
New particle formation is thought to contribute half of the global cloud condensation nuclei. We find that the new particle formation is more likely to happen in the upper boundary layer than that at the ground, which can be partially explained by the aerosol–radiation interaction. Our study emphasizes the influence of aerosol–radiation interaction on the NPF.
New particle formation is thought to contribute half of the global cloud condensation nuclei. We...
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