Articles | Volume 18, issue 16
https://doi.org/10.5194/acp-18-12085-2018
© Author(s) 2018. 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-18-12085-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
22 Aug 2018
Research article |
| 22 Aug 2018
| 22 Aug 2018
Comprehensive analysis of particle growth rates from nucleation mode to cloud condensation nuclei in boreal forest
Pauli Paasonen
CORRESPONDING AUTHOR
Institute for Atmospheric and Earth System Research (INAR) / Physics,
Faculty of Science, University of Helsinki, Finland
Maija Peltola
Institute for Atmospheric and Earth System Research (INAR) / Physics,
Faculty of Science, University of Helsinki, Finland
Jenni Kontkanen
Institute for Atmospheric and Earth System Research (INAR) / Physics,
Faculty of Science, University of Helsinki, Finland
Heikki Junninen
Institute for Atmospheric and Earth System Research (INAR) / Physics,
Faculty of Science, University of Helsinki, Finland
Institute of Physics, University of Tartu, Ülikooli 18, 50090
Tartu, Estonia
Veli-Matti Kerminen
Institute for Atmospheric and Earth System Research (INAR) / Physics,
Faculty of Science, University of Helsinki, Finland
Markku Kulmala
Institute for Atmospheric and Earth System Research (INAR) / Physics,
Faculty of Science, University of Helsinki, Finland
Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for
Soft Matter Science and Engineering, Beijing University of Chemical
Technology, 100029 Beijing, China
Joint International Research Laboratory of Atmospheric and Earth
System Sciences, School of Atmospheric Sciences, Nanjing University, 210046
Nanjing, China
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Cited
25 citations as recorded by crossref.
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- Dynamic and timing properties of new aerosol particle formation and consecutive growth events I. Salma & Z. Németh 10.5194/acp-19-5835-2019
- Iodine oxoacids and their roles in sub-3 nm particle growth in polluted urban environments Y. Zhang et al. 10.5194/acp-24-1873-2024
- Dynamics of aerosol, humidity, and clouds in air masses travelling over Fennoscandian boreal forests M. Räty et al. 10.5194/acp-23-3779-2023
- Aerosol microphysics and chemistry reveal the COVID19 lockdown impact on urban air quality K. Eleftheriadis et al. 10.1038/s41598-021-93650-6
- Activation properties of aerosol particles as cloud condensation nuclei at urban and high-altitude remote sites in southern Europe F. Rejano et al. 10.1016/j.scitotenv.2020.143100
- Aerosol formation and growth rates from chamber experiments using Kalman smoothing M. Ozon et al. 10.5194/acp-21-12595-2021
- Statistical analysis and environmental impact of pre-existing particle growth events in a Northern Chinese coastal megacity: A 725-day study in 2010–2018 X. Wei et al. 10.1016/j.scitotenv.2024.173227
- SO<sub>2</sub> and NH<sub>3</sub> emissions enhance organosulfur compounds and fine particle formation from the photooxidation of a typical aromatic hydrocarbon Z. Yang et al. 10.5194/acp-21-7963-2021
- Measurement report: New particle formation characteristics at an urban and a mountain station in northern China Y. Zhou et al. 10.5194/acp-21-17885-2021
- Evaluation of the Submicron Particles Distribution Between Mountain and Urban Site: Contribution of the Transportation for Defining Environmental and Human Health Issues M. Manigrasso et al. 10.3390/ijerph16081339
- 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
- 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
- Explaining apparent particle shrinkage related to new particle formation events in western Saudi Arabia does not require evaporation S. Hakala et al. 10.5194/acp-23-9287-2023
- Assessing volatile organic compound sources in a boreal forest using positive matrix factorization (PMF) M. Vestenius et al. 10.1016/j.atmosenv.2021.118503
- Reduction in Anthropogenic Emissions Suppressed New Particle Formation and Growth: Insights From the COVID‐19 Lockdown V. Kanawade et al. 10.1029/2021JD035392
- Mitigation Impact of Different Harvest Scenarios of Finnish Forests That Account for Albedo, Aerosols, and Trade-Offs of Carbon Sequestration and Avoided Emissions T. Kalliokoski et al. 10.3389/ffgc.2020.562044
- Variation of size-segregated particle number concentrations in wintertime Beijing Y. Zhou et al. 10.5194/acp-20-1201-2020
- Diel cycle of sea spray aerosol concentration J. Flores et al. 10.1038/s41467-021-25579-3
- Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
- Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
- Refined classification and characterization of atmospheric new-particle formation events using air ions L. Dada et al. 10.5194/acp-18-17883-2018
- Chemical precursors of new particle formation in coastal New Zealand M. Peltola et al. 10.5194/acp-23-3955-2023
- Overview: Recent advances in the understanding of the northern Eurasian environments and of the urban air quality in China – a Pan-Eurasian Experiment (PEEX) programme perspective H. Lappalainen et al. 10.5194/acp-22-4413-2022
- Cloud condensation nuclei characteristics at the Southern Great Plains site: role of particle size distribution and aerosol hygroscopicity P. Patel & J. Jiang 10.1088/2515-7620/ac0e0b
25 citations as recorded by crossref.
- Measurement report: Atmospheric new particle formation at a peri-urban site in Lille, northern France S. Crumeyrolle et al. 10.5194/acp-23-183-2023
- Dynamic and timing properties of new aerosol particle formation and consecutive growth events I. Salma & Z. Németh 10.5194/acp-19-5835-2019
- Iodine oxoacids and their roles in sub-3 nm particle growth in polluted urban environments Y. Zhang et al. 10.5194/acp-24-1873-2024
- Dynamics of aerosol, humidity, and clouds in air masses travelling over Fennoscandian boreal forests M. Räty et al. 10.5194/acp-23-3779-2023
- Aerosol microphysics and chemistry reveal the COVID19 lockdown impact on urban air quality K. Eleftheriadis et al. 10.1038/s41598-021-93650-6
- Activation properties of aerosol particles as cloud condensation nuclei at urban and high-altitude remote sites in southern Europe F. Rejano et al. 10.1016/j.scitotenv.2020.143100
- Aerosol formation and growth rates from chamber experiments using Kalman smoothing M. Ozon et al. 10.5194/acp-21-12595-2021
- Statistical analysis and environmental impact of pre-existing particle growth events in a Northern Chinese coastal megacity: A 725-day study in 2010–2018 X. Wei et al. 10.1016/j.scitotenv.2024.173227
- SO<sub>2</sub> and NH<sub>3</sub> emissions enhance organosulfur compounds and fine particle formation from the photooxidation of a typical aromatic hydrocarbon Z. Yang et al. 10.5194/acp-21-7963-2021
- Measurement report: New particle formation characteristics at an urban and a mountain station in northern China Y. Zhou et al. 10.5194/acp-21-17885-2021
- Evaluation of the Submicron Particles Distribution Between Mountain and Urban Site: Contribution of the Transportation for Defining Environmental and Human Health Issues M. Manigrasso et al. 10.3390/ijerph16081339
- 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
- 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
- Explaining apparent particle shrinkage related to new particle formation events in western Saudi Arabia does not require evaporation S. Hakala et al. 10.5194/acp-23-9287-2023
- Assessing volatile organic compound sources in a boreal forest using positive matrix factorization (PMF) M. Vestenius et al. 10.1016/j.atmosenv.2021.118503
- Reduction in Anthropogenic Emissions Suppressed New Particle Formation and Growth: Insights From the COVID‐19 Lockdown V. Kanawade et al. 10.1029/2021JD035392
- Mitigation Impact of Different Harvest Scenarios of Finnish Forests That Account for Albedo, Aerosols, and Trade-Offs of Carbon Sequestration and Avoided Emissions T. Kalliokoski et al. 10.3389/ffgc.2020.562044
- Variation of size-segregated particle number concentrations in wintertime Beijing Y. Zhou et al. 10.5194/acp-20-1201-2020
- Diel cycle of sea spray aerosol concentration J. Flores et al. 10.1038/s41467-021-25579-3
- Atmospheric nanoparticle growth D. Stolzenburg et al. 10.1103/RevModPhys.95.045002
- Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
- Refined classification and characterization of atmospheric new-particle formation events using air ions L. Dada et al. 10.5194/acp-18-17883-2018
- Chemical precursors of new particle formation in coastal New Zealand M. Peltola et al. 10.5194/acp-23-3955-2023
- Overview: Recent advances in the understanding of the northern Eurasian environments and of the urban air quality in China – a Pan-Eurasian Experiment (PEEX) programme perspective H. Lappalainen et al. 10.5194/acp-22-4413-2022
- Cloud condensation nuclei characteristics at the Southern Great Plains site: role of particle size distribution and aerosol hygroscopicity P. Patel & J. Jiang 10.1088/2515-7620/ac0e0b
Discussed (preprint)
Latest update: 12 Nov 2024
Short summary
We determine aerosol growth rates in diameter ranges from below 10 to over 300 nm from long-term data with a novel automatic method. We show that aerosol growth rate in boreal forest increases with increasing particle diameter from 10 nm to cloud condensation nuclei (CCN) sizes and that the growth rate of sub-CCN particles is not suppressed by increasing condensation sink. Our findings suggest that aerosol growth to CCN sizes is a faster and less self-regulated process than previously estimated.
We determine aerosol growth rates in diameter ranges from below 10 to over 300 nm from long-term...
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