Articles | Volume 15, issue 16
https://doi.org/10.5194/acp-15-9203-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-9203-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmospheric new particle formation as a source of CCN in the eastern Mediterranean marine boundary layer
Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, Greece
Department of Physics, University of Helsinki, P.O. Box 64, 00014, University of Helsinki, Helsinki, Finland
V.-M. Kerminen
Department of Physics, University of Helsinki, P.O. Box 64, 00014, University of Helsinki, Helsinki, Finland
G. Kouvarakis
Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, Greece
I. Stavroulas
Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, Greece
A. Bougiatioti
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA
National Technical University of Athens, Zografou Campus, 15780, Athens, Greece
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA
School of Chemical & Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA, 30332, USA
ICE-HT, Foundation for Research and Technology, Hellas, 26504, Patras, Greece
H. E. Manninen
Department of Physics, University of Helsinki, P.O. Box 64, 00014, University of Helsinki, Helsinki, Finland
Institute of Physics, University of Tartu, Ülikooli 18, 50090, Tartu, Estonia
T. Petäjä
Department of Physics, University of Helsinki, P.O. Box 64, 00014, University of Helsinki, Helsinki, Finland
M. Kulmala
Department of Physics, University of Helsinki, P.O. Box 64, 00014, University of Helsinki, Helsinki, Finland
N. Mihalopoulos
Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, Greece
Institute for Environmental Research & Sustainable Development, National Observatory of Athens (NOA), I. Metaxa & Vas. Pavlou, 15236 Palea Penteli, Greece
Energy, Environment and Water Research Center, The Cyprus Institute, Nicosia 2121, Cyprus
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- Unexpectedly significant stabilizing mechanism of iodous acid on iodic acid nucleation under different atmospheric conditions L. Liu et al. 10.1016/j.scitotenv.2022.159832
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43 citations as recorded by crossref.
- Towards understanding the characteristics of new particle formation in the Eastern Mediterranean R. Baalbaki et al. 10.5194/acp-21-9223-2021
- Cloud condensation nuclei properties of South Asian outflow over the northern Indian Ocean during winter V. Nair et al. 10.5194/acp-20-3135-2020
- Investigating the contribution of grown new particles to cloud condensation nuclei with largely varying preexisting particles – Part 1: Observational data analysis X. Wei et al. 10.5194/acp-23-15325-2023
- Impacts of the aerosol mixing state and new particle formation on CCN in summer at the summit of Mount Tai (1534m) in Central East China Z. Wu et al. 10.1016/j.scitotenv.2024.170622
- Measurement report: Cloud processes and the transport of biological emissions affect southern ocean particle and cloud condensation nuclei concentrations K. Sanchez et al. 10.5194/acp-21-3427-2021
- The synergistic nucleation of iodous acid and sulfuric acid: A vital mechanism in polluted marine regions H. Zu et al. 10.1016/j.atmosenv.2023.120266
- New particle formation leads to cloud dimming R. Sullivan et al. 10.1038/s41612-018-0019-7
- Rapid iodine oxoacid nucleation enhanced by dimethylamine in broad marine regions H. Zu et al. 10.5194/acp-24-5823-2024
- Regional New Particle Formation over the Eastern Mediterranean and Middle East P. Kalkavouras et al. 10.3390/atmos12010013
- Greenhouse gases (CO2 and CH4) at an urban background site in Athens, Greece: Levels, sources and impact of atmospheric circulation K. Dimitriou et al. 10.1016/j.atmosenv.2021.118372
- A phenomenology of new particle formation (NPF) at 13 European sites D. Bousiotis et al. 10.5194/acp-21-11905-2021
- On the regional aspects of new particle formation in the Eastern Mediterranean: A comparative study between a background and an urban site based on long term observations P. Kalkavouras et al. 10.1016/j.atmosres.2020.104911
- Mass and number concentration distribution of marine aerosol in the Western Pacific and the influence of continental transport Y. Ma et al. 10.1016/j.envpol.2022.118827
- Characterization of aerosol particles at Cabo Verde close to sea level and at the cloud level – Part 1: Particle number size distribution, cloud condensation nuclei and their origins X. Gong et al. 10.5194/acp-20-1431-2020
- Exploring the use of ground-based remote sensing to identify new particle formation events: A case study in the Beijing area Y. Zhang et al. 10.1016/j.scitotenv.2024.176693
- Spatial extent of new particle formation events over the Mediterranean Basin from multiple ground-based and airborne measurements K. Berland et al. 10.5194/acp-17-9567-2017
- Biomass-burning impact on CCN number, hygroscopicity and cloud formation during summertime in the eastern Mediterranean A. Bougiatioti et al. 10.5194/acp-16-7389-2016
- Geometrical and Microphysical Properties of Clouds Formed in the Presence of Dust above the Eastern Mediterranean E. Marinou et al. 10.3390/rs13245001
- Formation and growth of atmospheric nanoparticles in the eastern Mediterranean: results from long-term measurements and process simulations N. Kalivitis et al. 10.5194/acp-19-2671-2019
- Evaluation of global simulations of aerosol particle and cloud condensation nuclei number, with implications for cloud droplet formation G. Fanourgakis et al. 10.5194/acp-19-8591-2019
- Effect of aerosol types from various sources at an urban location on spectral curvature of scattering and absorption coefficients D. Kaskaoutis et al. 10.1016/j.atmosres.2021.105865
- New particle formation in the southern Aegean Sea during the Etesians: importance for CCN production and cloud droplet number P. Kalkavouras et al. 10.5194/acp-17-175-2017
- Effects of boundary layer dynamics and meteorology on ultrafine particle formation and growth Z. Watson et al. 10.1016/j.atmosenv.2023.119952
- Particle number size distribution statistics at City-Centre Urban Background, urban background, and remote stations in Greece during summer S. Vratolis et al. 10.1016/j.atmosenv.2019.05.064
- Nucleation-mode particle pool and large increases in <i>N</i><sub>cn</sub> and <i>N</i><sub>ccn</sub> observed over the northwestern Pacific Ocean in the spring of 2014 J. Wang et al. 10.5194/acp-19-8845-2019
- Observations of particle number size distributions and new particle formation in six Indian locations M. Sebastian et al. 10.5194/acp-22-4491-2022
- Characterization of aerosol properties at Cyprus, focusing on cloud condensation nuclei and ice-nucleating particles X. Gong et al. 10.5194/acp-19-10883-2019
- Concentration levels and source apportionment of ultrafine particles in road microenvironments G. Argyropoulos et al. 10.1016/j.atmosenv.2016.01.009
- Cloud condensation nuclei characteristics during the Indian summer monsoon over a rain-shadow region V. Jayachandran et al. 10.5194/acp-20-7307-2020
- Comparison of aerosol number size distribution and new particle formation in summer at alpine and urban regions in the Guanzhong Plain, Northwest China H. Liu et al. 10.1016/j.scitotenv.2024.176601
- Seasonal significance of new particle formation impacts on cloud condensation nuclei at a mountaintop location N. Hirshorn et al. 10.5194/acp-22-15909-2022
- Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
- Direct measurement of the growth of small particles in ambient air using captive aerosol chambers Z. Zhu et al. 10.1016/j.atmosenv.2024.120915
- Long-term quantitative field study of New Particle Formation (NPF) events as a source of Cloud Condensation Nuclei (CCN) in the urban background of Vienna C. Dameto de España et al. 10.1016/j.atmosenv.2017.06.001
- Shipborne observations reveal contrasting Arctic marine, Arctic terrestrial and Pacific marine aerosol properties J. Park et al. 10.5194/acp-20-5573-2020
- Isoprene suppression of new particle formation: Potential mechanisms and implications S. Lee et al. 10.1002/2016JD024844
- Regional new particle formation as modulators of cloud condensation nuclei and cloud droplet number in the eastern Mediterranean P. Kalkavouras et al. 10.5194/acp-19-6185-2019
- Annual cycle of hygroscopic properties and mixing state of the suburban aerosol in Athens, Greece C. Spitieri et al. 10.5194/acp-23-235-2023
- The Atmospheric Aerosol over Western Greece-Six Years of Aerosol Observations at the Navarino Environmental Observatory H. Hansson et al. 10.3390/atmos12040445
- The versatile size analyzing nuclei counter (vSANC) T. Pinterich et al. 10.1080/02786826.2016.1210783
- New particle formation and sub-10 nm size distribution measurements during the A-LIFE field experiment in Paphos, Cyprus S. Brilke et al. 10.5194/acp-20-5645-2020
- Influence of pollutants on activity of aerosol cloud condensation nuclei (CCN) during pollution and post-rain periods in Guangzhou, southern China J. Duan et al. 10.1016/j.scitotenv.2018.06.053
- Unexpectedly significant stabilizing mechanism of iodous acid on iodic acid nucleation under different atmospheric conditions L. Liu et al. 10.1016/j.scitotenv.2022.159832
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Latest update: 21 Nov 2024
Short summary
Cloud condensation nuclei (CCN) production associated with atmospheric new particle formation (NPF) is presented, and this is the first direct evidence of CCN production resulting from NPF in the eastern Mediterranean atmosphere. We show that condensation of both gaseous sulfuric acid and organic compounds from multiple sources leads to the rapid growth of nucleated particles. Sub-100nm particles were found to be substantially less hygroscopic than larger particles during the active NPF period.
Cloud condensation nuclei (CCN) production associated with atmospheric new particle formation...
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