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.
Research article
| 
06 May 2019
Research article |
| 06 May 2019
| 06 May 2019
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
12 citations as recorded by crossref.
- 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
- 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
- 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
- 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
- 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
- Highly significant impact of mineral dust on aerosol hygroscopicity at New Delhi Z. Arub et al. 10.1016/j.atmosenv.2021.118375
- 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
- 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
12 citations as recorded by crossref.
- 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
- 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
- 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
- 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
- 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
- Highly significant impact of mineral dust on aerosol hygroscopicity at New Delhi Z. Arub et al. 10.1016/j.atmosenv.2021.118375
- 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
- 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
Latest update: 14 Dec 2024
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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