Articles | Volume 21, issue 11
https://doi.org/10.5194/acp-21-8575-2021
© 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-21-8575-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The important roles of surface tension and growth rate in the contribution of new particle formation (NPF) to cloud condensation nuclei (CCN) number concentration: evidence from field measurements in southern China
Mingfu Cai
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation
for Environmental Quality, Guangzhou, Guangdong 511443, China
School of Atmospheric Sciences, Guangdong Province Key Laboratory for
Climate Change and Natural Disaster Studies, and Institute of Earth Climate
and Environment System, Sun Yat-sen University, Zhuhai, Guangdong 519082,
China
Institute of Tropical and Marine Meteorology and Guangdong Provincial Key
Laboratory of Regional Numerical Weather Prediction, China Meteorological Administration, Guangzhou 510640,
China
Baoling Liang
School of Atmospheric Sciences, Guangdong Province Key Laboratory for
Climate Change and Natural Disaster Studies, and Institute of Earth Climate
and Environment System, Sun Yat-sen University, Zhuhai, Guangdong 519082,
China
Qibin Sun
School of Atmospheric Sciences, Guangdong Province Key Laboratory for
Climate Change and Natural Disaster Studies, and Institute of Earth Climate
and Environment System, Sun Yat-sen University, Zhuhai, Guangdong 519082,
China
Li Liu
Institute of Tropical and Marine Meteorology and Guangdong Provincial Key
Laboratory of Regional Numerical Weather Prediction, China Meteorological Administration, Guangzhou 510640,
China
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation
for Environmental Quality, Guangzhou, Guangdong 511443, China
Min Shao
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation
for Environmental Quality, Guangzhou, Guangdong 511443, China
Shan Huang
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation
for Environmental Quality, Guangzhou, Guangdong 511443, China
Yuwen Peng
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation
for Environmental Quality, Guangzhou, Guangdong 511443, China
Zelong Wang
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation
for Environmental Quality, Guangzhou, Guangdong 511443, China
Haobo Tan
Institute of Tropical and Marine Meteorology and Guangdong Provincial Key
Laboratory of Regional Numerical Weather Prediction, China Meteorological Administration, Guangzhou 510640,
China
Institute of Tropical and Marine Meteorology and Guangdong Provincial Key
Laboratory of Regional Numerical Weather Prediction, China Meteorological Administration, Guangzhou 510640,
China
Laboratory of Straits Meteorology, Xiamen, Guangdong 361012, China
Hanbin Xu
School of Atmospheric Sciences, Guangdong Province Key Laboratory for
Climate Change and Natural Disaster Studies, and Institute of Earth Climate
and Environment System, Sun Yat-sen University, Zhuhai, Guangdong 519082,
China
Duohong Chen
Guangdong Environmental Monitoring Center, Guangzhou 510308,
China
School of Atmospheric Sciences, Guangdong Province Key Laboratory for
Climate Change and Natural Disaster Studies, and Institute of Earth Climate
and Environment System, Sun Yat-sen University, Zhuhai, Guangdong 519082,
China
Southern Marine Science and Engineering Guangdong Laboratory
(Zhuhai), Zhuhai, Guangdong 519082, China
Guangdong Provincial Observation and Research Station for Climate
Environment and Air Quality Change in the Pearl River Estuary, Guangzhou,
Guangdong 510275, China
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Cited
11 citations as recorded by crossref.
- Measurement report: Distinct size dependence and diurnal variation in organic aerosol hygroscopicity, volatility, and cloud condensation nuclei activity at a rural site in the Pearl River Delta (PRD) region, China M. Cai et al. 10.5194/acp-22-8117-2022
- Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
- Aerosol mixing state, new particle formation, and cloud droplet number concentration in an urban environment S. Kasparoglu et al. 10.1016/j.scitotenv.2024.175307
- Cruise observation of the marine atmosphere and ship emissions in South China Sea: Aerosol composition, sources, and the aging process Q. Sun et al. 10.1016/j.envpol.2022.120539
- Atmospheric Particle Number Concentrations and New Particle Formation over the Southern Ocean and Antarctica: A Critical Review J. Wang et al. 10.3390/atmos14020402
- Particle number size distributions and formation and growth rates of different new particle formation types of a megacity in China L. Dai et al. 10.1016/j.jes.2022.07.029
- 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
- Iodine oxoacids and their roles in sub-3 nm particle growth in polluted urban environments Y. Zhang et al. 10.5194/acp-24-1873-2024
- Measuring the Surface Tension of Atmospheric Particles and Relevant Mixtures to Better Understand Key Atmospheric Processes M. El Haber et al. 10.1021/acs.chemrev.4c00173
- 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
- Enhanced daytime secondary aerosol formation driven by gas–particle partitioning in downwind urban plumes M. Cai et al. 10.5194/acp-24-13065-2024
11 citations as recorded by crossref.
- Measurement report: Distinct size dependence and diurnal variation in organic aerosol hygroscopicity, volatility, and cloud condensation nuclei activity at a rural site in the Pearl River Delta (PRD) region, China M. Cai et al. 10.5194/acp-22-8117-2022
- Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
- Aerosol mixing state, new particle formation, and cloud droplet number concentration in an urban environment S. Kasparoglu et al. 10.1016/j.scitotenv.2024.175307
- Cruise observation of the marine atmosphere and ship emissions in South China Sea: Aerosol composition, sources, and the aging process Q. Sun et al. 10.1016/j.envpol.2022.120539
- Atmospheric Particle Number Concentrations and New Particle Formation over the Southern Ocean and Antarctica: A Critical Review J. Wang et al. 10.3390/atmos14020402
- Particle number size distributions and formation and growth rates of different new particle formation types of a megacity in China L. Dai et al. 10.1016/j.jes.2022.07.029
- 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
- Iodine oxoacids and their roles in sub-3 nm particle growth in polluted urban environments Y. Zhang et al. 10.5194/acp-24-1873-2024
- Measuring the Surface Tension of Atmospheric Particles and Relevant Mixtures to Better Understand Key Atmospheric Processes M. El Haber et al. 10.1021/acs.chemrev.4c00173
- 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
- Enhanced daytime secondary aerosol formation driven by gas–particle partitioning in downwind urban plumes M. Cai et al. 10.5194/acp-24-13065-2024
Latest update: 05 Dec 2024
Short summary
This study investigated the contribution of new particle formation (NPF) events to the number concentration of cloud condensation nuclei (NCCN) and its controlling factors in the Pearl River Delta region. The results show that the surfactant effect can decrease the critical diameter and significantly increase the NCCN during the NPF event. In addition, the growth rate is founded to be the most important controlling factor that affects NCCN for growth of newly-formed particles to the CCN sizes.
This study investigated the contribution of new particle formation (NPF) events to the number...
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