Articles | Volume 20, issue 21
https://doi.org/10.5194/acp-20-12515-2020
© Author(s) 2020. 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-20-12515-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
01 Nov 2020
Research article | Highlight paper |
| 01 Nov 2020
| 01 Nov 2020
Large contribution of organics to condensational growth and formation of cloud condensation nuclei (CCN) in the remote marine boundary layer
Guangjie Zheng
Center for Aerosol Science and Engineering, Department of Energy,
Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri, USA
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
Chongai Kuang
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
Janek Uin
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
Thomas Watson
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
Center for Aerosol Science and Engineering, Department of Energy,
Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, Missouri, USA
Environmental and Climate Science Department, Brookhaven National
Laboratory, Upton, New York, USA
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26 citations as recorded by crossref.
- Sea ice concentration impacts dissolved organic gases in the Canadian Arctic C. Wohl et al. 10.5194/bg-19-1021-2022
- Maximum Supersaturation in the Marine Boundary Layer Clouds Over the North Atlantic X. Gong et al. 10.1029/2022AV000855
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- Management of hailstorms under a changing climate in agriculture: a review V. Rana et al. 10.1007/s10311-022-01502-0
- Global organic and inorganic aerosol hygroscopicity and its effect on radiative forcing M. Pöhlker et al. 10.1038/s41467-023-41695-8
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- Environmental effects on aerosol–cloud interaction in non-precipitating marine boundary layer (MBL) clouds over the eastern North Atlantic X. Zheng et al. 10.5194/acp-22-335-2022
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- Addressing the difficulties in quantifying droplet number response to aerosol from satellite observations H. Jia et al. 10.5194/acp-22-7353-2022
- Chemical precursors of new particle formation in coastal New Zealand M. Peltola et al. 10.5194/acp-23-3955-2023
- Drivers of Cloud Condensation Nuclei in the Eastern North Atlantic as Observed at the ARM Site V. Ghate et al. 10.1029/2023JD038636
- Atmospheric Benzothiazoles in a Coastal Marine Environment E. Franklin et al. 10.1021/acs.est.1c04422
- Observation on the Droplet Ranging from 2 to 16 μm in Cloud Droplet Size Distribution Based on Digital Holography P. Gao et al. 10.3390/rs14102414
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- Aerosol and Cloud Experiments in the Eastern North Atlantic (ACE-ENA) J. Wang et al. 10.1175/BAMS-D-19-0220.1
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- Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
- An evaluation of new particle formation events in Helsinki during a Baltic Sea cyanobacterial summer bloom R. Thakur et al. 10.5194/acp-22-6365-2022
- Vertical profiles of trace gas and aerosol properties over the eastern North Atlantic: variations with season and synoptic condition Y. Wang et al. 10.5194/acp-21-11079-2021
- Further analysis of CCN data at a mid-Antarctica Peninsula field site T. DeFelice 10.1016/j.atmosres.2021.105556
Latest update: 18 Apr 2024
Short summary
Condensational growth of Aitken-mode particles is a major source of cloud condensation nuclei in the remote marine boundary layer. It has been long thought that over remote oceans, condensation growth is dominated by sulfate that derives from ocean-emitted dimethyl sulfide. In this study, we present the first long-term observational evidence that, contrary to conventional thinking, organics play an even more important role than sulfate in particle growth over remote oceans throughout the year.
Condensational growth of Aitken-mode particles is a major source of cloud condensation nuclei in...
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