Articles | Volume 19, issue 9 
            
                
                    
            
            
            https://doi.org/10.5194/acp-19-5889-2019
                    © Author(s) 2019. 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-19-5889-2019
                    © Author(s) 2019. This work is distributed under 
the Creative Commons Attribution 4.0 License.
                the Creative Commons Attribution 4.0 License.
Diurnal variation and size dependence of the hygroscopicity of organic aerosol at a forest site in Wakayama, Japan: their relationship to CCN concentrations
Yange Deng
                                            Graduate School of Environmental Studies, Nagoya University, Nagoya,
Japan
                                        
                                    
                                            Institute for Space-Earth Environmental Research, Nagoya University, Nagoya,
Japan
                                        
                                    Hikari Yai
                                            Graduate School of Environmental Studies, Nagoya University, Nagoya,
Japan
                                        
                                    Hiroaki Fujinari
                                            Graduate School of Environmental Studies, Nagoya University, Nagoya,
Japan
                                        
                                    Kaori Kawana
                                            Institute of Low Temperature Science, Hokkaido University, Hokkaido, Japan
                                        
                                    
                                            now at: Research and Development Center for Global Change, Japan Agency
for Marine-Earth Science and Technology, Yokohama, Japan
                                        
                                    Tomoki Nakayama
                                            Institute for Space-Earth Environmental Research, Nagoya University, Nagoya,
Japan
                                        
                                    
                                            now at: Graduate School of Fisheries and Environmental Sciences,
Nagasaki University, Nagasaki, Japan
                                        
                                    Michihiro Mochida
CORRESPONDING AUTHOR
                                            
                                    
                                            Graduate School of Environmental Studies, Nagoya University, Nagoya,
Japan
                                        
                                    
                                            Institute for Space-Earth Environmental Research, Nagoya University, Nagoya,
Japan
                                        
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                            Cited
13 citations as recorded by crossref.
- CCN estimations at a high-altitude remote site: role of organic aerosol variability and hygroscopicity F. Rejano et al. 10.5194/acp-24-13865-2024
 - Hygroscopicity of urban aerosols and its link to size-resolved chemical composition during spring and summer in Seoul, Korea N. Kim et al. 10.5194/acp-20-11245-2020
 - Distinct diurnal variation in organic aerosol hygroscopicity and its relationship with oxygenated organic aerosol Y. Kuang et al. 10.5194/acp-20-865-2020
 - Hygroscopic growth and CCN activation of aerosols during Indian Summer Monsoon over a rain-shadow region V. Jayachandran et al. 10.1016/j.atmosres.2021.105976
 - 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
 - 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
 - Highly significant impact of mineral dust on aerosol hygroscopicity at New Delhi Z. Arub et al. 10.1016/j.atmosenv.2021.118375
 - Characterization of size-resolved aerosol hygroscopicity and liquid water content in Nanjing of the Yangtze River Delta Y. Jiang et al. 10.1016/j.jes.2024.03.035
 - 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 M. Cai et al. 10.5194/acp-21-8575-2021
 - Technical note: Quantified organic aerosol subsaturated hygroscopicity by a simple optical scatter monitor system through field measurements J. Zhang et al. 10.5194/acp-24-13445-2024
 - Contrasting effects of secondary organic aerosol formations on organic aerosol hygroscopicity Y. Kuang et al. 10.5194/acp-21-10375-2021
 - 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
 - Offline analysis of the chemical composition and hygroscopicity of submicrometer aerosol at an Asian outflow receptor site and comparison with online measurements Y. Deng et al. 10.5194/acp-22-5515-2022
 
13 citations as recorded by crossref.
- CCN estimations at a high-altitude remote site: role of organic aerosol variability and hygroscopicity F. Rejano et al. 10.5194/acp-24-13865-2024
 - Hygroscopicity of urban aerosols and its link to size-resolved chemical composition during spring and summer in Seoul, Korea N. Kim et al. 10.5194/acp-20-11245-2020
 - Distinct diurnal variation in organic aerosol hygroscopicity and its relationship with oxygenated organic aerosol Y. Kuang et al. 10.5194/acp-20-865-2020
 - Hygroscopic growth and CCN activation of aerosols during Indian Summer Monsoon over a rain-shadow region V. Jayachandran et al. 10.1016/j.atmosres.2021.105976
 - 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
 - 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
 - Highly significant impact of mineral dust on aerosol hygroscopicity at New Delhi Z. Arub et al. 10.1016/j.atmosenv.2021.118375
 - Characterization of size-resolved aerosol hygroscopicity and liquid water content in Nanjing of the Yangtze River Delta Y. Jiang et al. 10.1016/j.jes.2024.03.035
 - 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 M. Cai et al. 10.5194/acp-21-8575-2021
 - Technical note: Quantified organic aerosol subsaturated hygroscopicity by a simple optical scatter monitor system through field measurements J. Zhang et al. 10.5194/acp-24-13445-2024
 - Contrasting effects of secondary organic aerosol formations on organic aerosol hygroscopicity Y. Kuang et al. 10.5194/acp-21-10375-2021
 - 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
 - Offline analysis of the chemical composition and hygroscopicity of submicrometer aerosol at an Asian outflow receptor site and comparison with online measurements Y. Deng et al. 10.5194/acp-22-5515-2022
 
Latest update: 03 Nov 2025
Short summary
                    Organic aerosol (OA) components account for 20–90 % of sub-micrometer aerosol mass and have a broad distribution of hygroscopicity. For the first time, the diurnal variation and size dependence of the hygroscopicity of OA were characterized for a forest in East Asia. The observed variation and dependence were assessed from the viewpoint of biogenic secondary organic aerosol formation, and they strongly affected the contribution of OA to the CCN number concentration.
                    Organic aerosol (OA) components account for 20–90 % of sub-micrometer aerosol mass and have a...
                    
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