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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29 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
- Influence of open ocean biogeochemistry on aerosol and clouds: Recent findings and perspectives K. Sellegri et al. 10.1525/elementa.2023.00058
- Condensation of organic-inorganic vapours governs the production of ultrafine secondary marine cloud nuclei W. Xu et al. 10.1038/s43247-024-01519-z
- Factors controlling marine aerosol size distributions and their climate effects over the northwest Atlantic Ocean region B. Croft et al. 10.5194/acp-21-1889-2021
- Marine volatile organic compounds and their impacts on marine aerosol—A review Z. Yu & Y. Li 10.1016/j.scitotenv.2021.145054
- Observed Relationships Between Cloud Droplet Effective Radius and Biogenic Gas Concentrations in Summertime Marine Stratocumulus Over the Eastern North Atlantic M. Miller et al. 10.1029/2021EA001929
- On the correlation between hygroscopic properties and chemical composition of cloud condensation nuclei obtained from the chemical aging of soot particles with O3 and SO2 J. Wu et al. 10.1016/j.scitotenv.2023.167745
- Optical Modeling of Sea Salt Aerosols Using in situ Measured Size Distributions and the Impact of Larger Size Particles W. Lin & L. Bi 10.1007/s00376-024-3351-3
- Evaluation of the Sources, Precursors, and Processing of Aerosols at a High-Altitude Tropical Site P. Dominutti et al. 10.1021/acsearthspacechem.2c00149
- Influences of Recent Particle Formation on Southern Ocean Aerosol Variability and Low Cloud Properties I. McCoy et al. 10.1029/2020JD033529
- 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
- Secondary Organic Aerosol Formation Regulates Cloud Condensation Nuclei in the Global Remote Troposphere M. Liu & H. Matsui 10.1029/2022GL100543
- 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
- Regularized inversion of aerosol hygroscopic growth factor probability density function: application to humidity-controlled fast integrated mobility spectrometer measurements J. Zhang et al. 10.5194/amt-15-2579-2022
- New particle formation in coastal New Zealand with a focus on open-ocean air masses M. Peltola et al. 10.5194/acp-22-6231-2022
- 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
- Impact of dry intrusion events on the composition and mixing state of particles during the winter Aerosol and Cloud Experiment in the Eastern North Atlantic (ACE-ENA) J. Tomlin et al. 10.5194/acp-21-18123-2021
- Contribution of Speciated Monoterpenes to Secondary Aerosol in the Eastern North Atlantic D. Kilgour et al. 10.1021/acsestair.3c00112
- Rapid measurement of RH-dependent aerosol hygroscopic growth using a humidity-controlled fast integrated mobility spectrometer (HFIMS) J. Zhang et al. 10.5194/amt-14-5625-2021
- 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: 22 Nov 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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