Articles | Volume 21, issue 9
https://doi.org/10.5194/acp-21-7409-2021
© 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-21-7409-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Secondary aerosol formation alters CCN activity in the North China Plain
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, 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, China
Nan Ma
CORRESPONDING AUTHOR
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, China
Juan Hong
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, China
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
Wanyun Xu
State Key Laboratory of Severe Weather, Key Laboratory for Atmospheric Chemistry, Institute of Atmospheric Composition, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Yanyan Zhang
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Yao He
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
Qingwei Luo
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Linhong Xie
Institute for Environmental and Climate Research, Jinan University,
Guangzhou, Guangdong 511443, China
Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou, China
Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
Yafang Cheng
Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
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Cited
10 citations as recorded by crossref.
- Evaluation of the contribution of new particle formation to cloud droplet number concentration in the urban atmosphere S. Jiang et al. 10.5194/acp-21-14293-2021
- Prediction of CCN spectra parameters in the North China Plain using a random forest model M. Liang et al. 10.1016/j.atmosenv.2022.119323
- Kinetic Limitations Affect Cloud Condensation Nuclei Activity Measurements Under Low Supersaturation J. Tao et al. 10.1029/2022GL101603
- Source Apportionment of Cloud Nuclei at 260 m and Ground Level in Urban Beijing S. Jiang et al. 10.1029/2022JD038339
- Particle number size distribution of PM1 and PM10 in fogs and implications on fog droplet evolutions S. Wu et al. 10.1016/j.atmosenv.2022.119086
- Current Challenges in Visibility Improvement in Sichuan Basin G. Zhao et al. 10.1029/2022GL098836
- Studies on the improvement of modelled solar radiation and the attenuation effect of aerosol using the WRF-Solar model with satellite-based AOD data over north China X. Cheng et al. 10.1016/j.renene.2022.06.141
- Hygroscopicity of Water‐Soluble PM2.5 in Rural Northwest China: Contrasting Contributors Between Summer and Winter Y. Chen et al. 10.1029/2021JD034977
- Investigation of physico-chemical characteristics and associated CCN activation for different combustion sources through Chamber experiment approach S. Mukherjee et al. 10.1016/j.atmosenv.2021.118726
- The effects of number and mass concentration of aerosol components on scattering coefficients in Xianghe, southeast of Beijing, China – A case study J. Zou et al. 10.1016/j.atmosenv.2022.118938
10 citations as recorded by crossref.
- Evaluation of the contribution of new particle formation to cloud droplet number concentration in the urban atmosphere S. Jiang et al. 10.5194/acp-21-14293-2021
- Prediction of CCN spectra parameters in the North China Plain using a random forest model M. Liang et al. 10.1016/j.atmosenv.2022.119323
- Kinetic Limitations Affect Cloud Condensation Nuclei Activity Measurements Under Low Supersaturation J. Tao et al. 10.1029/2022GL101603
- Source Apportionment of Cloud Nuclei at 260 m and Ground Level in Urban Beijing S. Jiang et al. 10.1029/2022JD038339
- Particle number size distribution of PM1 and PM10 in fogs and implications on fog droplet evolutions S. Wu et al. 10.1016/j.atmosenv.2022.119086
- Current Challenges in Visibility Improvement in Sichuan Basin G. Zhao et al. 10.1029/2022GL098836
- Studies on the improvement of modelled solar radiation and the attenuation effect of aerosol using the WRF-Solar model with satellite-based AOD data over north China X. Cheng et al. 10.1016/j.renene.2022.06.141
- Hygroscopicity of Water‐Soluble PM2.5 in Rural Northwest China: Contrasting Contributors Between Summer and Winter Y. Chen et al. 10.1029/2021JD034977
- Investigation of physico-chemical characteristics and associated CCN activation for different combustion sources through Chamber experiment approach S. Mukherjee et al. 10.1016/j.atmosenv.2021.118726
- The effects of number and mass concentration of aerosol components on scattering coefficients in Xianghe, southeast of Beijing, China – A case study J. Zou et al. 10.1016/j.atmosenv.2022.118938
Latest update: 16 Aug 2024
Short summary
The mechanism of secondary aerosol (SA) formation can be affected by relative humidity (RH) and has different influences on the particle CCN activity under different RH conditions. In the North China Plain, we find different responses of CCN activity and enhancements of CCN number concentration to SA formation under different RH conditions. In addition, variations of aerosol mixing state due to SA formation contribute some of the largest uncertainties in predicting CCN number concentration.
The mechanism of secondary aerosol (SA) formation can be affected by relative humidity (RH) and...
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