Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010

Secondary new particle formation affects atmospheric aerosol and cloud droplet numbers and thereby, the aerosol effects on climate. In this paper, the frequency of nucleation events and the associated particle formation and growth rates, along with their seasonal variation, was analysed based on ove...

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Published in:Atmospheric Chemistry and Physics
Main Authors: E. Asmi, N. Kivekäs, V.-M. Kerminen, M. Komppula, A.-P. Hyvärinen, J. Hatakka, Y. Viisanen, H. Lihavainen
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/acp-11-12959-2011
https://doaj.org/article/951504c2b3d7414597f6740d60c05fb3
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spelling ftdoajarticles:oai:doaj.org/article:951504c2b3d7414597f6740d60c05fb3 2023-05-15T17:42:22+02:00 Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010 E. Asmi N. Kivekäs V.-M. Kerminen M. Komppula A.-P. Hyvärinen J. Hatakka Y. Viisanen H. Lihavainen 2011-12-01T00:00:00Z https://doi.org/10.5194/acp-11-12959-2011 https://doaj.org/article/951504c2b3d7414597f6740d60c05fb3 EN eng Copernicus Publications http://www.atmos-chem-phys.net/11/12959/2011/acp-11-12959-2011.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-11-12959-2011 1680-7316 1680-7324 https://doaj.org/article/951504c2b3d7414597f6740d60c05fb3 Atmospheric Chemistry and Physics, Vol 11, Iss 24, Pp 12959-12972 (2011) Physics QC1-999 Chemistry QD1-999 article 2011 ftdoajarticles https://doi.org/10.5194/acp-11-12959-2011 2022-12-31T12:14:15Z Secondary new particle formation affects atmospheric aerosol and cloud droplet numbers and thereby, the aerosol effects on climate. In this paper, the frequency of nucleation events and the associated particle formation and growth rates, along with their seasonal variation, was analysed based on over ten years of aerosol measurements conducted at the Pallas GAW station in northern Finland. The long-term measurements also allowed a detailed examination of factors possibly favouring or suppressing particle formation. Effects of meteorological parameters and air mass properties as well as vapour sources and sinks for particle formation frequency and event parameters were inspected. In addition, the potential of secondary particle formation to increase the concentration of cloud condensation nuclei (CCN) sized particles was examined. Findings from these long-term measurements confirmed previous observations: event frequency peaked in spring and the highest growth rates were observed in summer, affiliated with increased biogenic activity. Events were almost exclusively observed in marine air masses on sunny cloud-free days. A low vapour sink by the background particle population as well as an elevated sulphuric acid concentration were found to favour particle formation. These were also conditions taking place most likely in marine air masses. Inter-annual trend showed a minimum in event frequency in 2003, when also the smallest annual median of growth rate was observed. This gives further evidence of the importance and sensitivity of particle formation for the condensing vapour concentrations at Pallas site. The particle formation was observed to increase CCN 80 (>80 nm particle number) concentrations especially in summer and autumn seasons when the growth rates were the highest. When the growing mode exceeded the selected 80 nm limit, on average in those cases, 211 ± 114% increase of CCN 80 concentrations was observed. Article in Journal/Newspaper Northern Finland Directory of Open Access Journals: DOAJ Articles Atmospheric Chemistry and Physics 11 24 12959 12972
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
E. Asmi
N. Kivekäs
V.-M. Kerminen
M. Komppula
A.-P. Hyvärinen
J. Hatakka
Y. Viisanen
H. Lihavainen
Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010
topic_facet Physics
QC1-999
Chemistry
QD1-999
description Secondary new particle formation affects atmospheric aerosol and cloud droplet numbers and thereby, the aerosol effects on climate. In this paper, the frequency of nucleation events and the associated particle formation and growth rates, along with their seasonal variation, was analysed based on over ten years of aerosol measurements conducted at the Pallas GAW station in northern Finland. The long-term measurements also allowed a detailed examination of factors possibly favouring or suppressing particle formation. Effects of meteorological parameters and air mass properties as well as vapour sources and sinks for particle formation frequency and event parameters were inspected. In addition, the potential of secondary particle formation to increase the concentration of cloud condensation nuclei (CCN) sized particles was examined. Findings from these long-term measurements confirmed previous observations: event frequency peaked in spring and the highest growth rates were observed in summer, affiliated with increased biogenic activity. Events were almost exclusively observed in marine air masses on sunny cloud-free days. A low vapour sink by the background particle population as well as an elevated sulphuric acid concentration were found to favour particle formation. These were also conditions taking place most likely in marine air masses. Inter-annual trend showed a minimum in event frequency in 2003, when also the smallest annual median of growth rate was observed. This gives further evidence of the importance and sensitivity of particle formation for the condensing vapour concentrations at Pallas site. The particle formation was observed to increase CCN 80 (>80 nm particle number) concentrations especially in summer and autumn seasons when the growth rates were the highest. When the growing mode exceeded the selected 80 nm limit, on average in those cases, 211 ± 114% increase of CCN 80 concentrations was observed.
format Article in Journal/Newspaper
author E. Asmi
N. Kivekäs
V.-M. Kerminen
M. Komppula
A.-P. Hyvärinen
J. Hatakka
Y. Viisanen
H. Lihavainen
author_facet E. Asmi
N. Kivekäs
V.-M. Kerminen
M. Komppula
A.-P. Hyvärinen
J. Hatakka
Y. Viisanen
H. Lihavainen
author_sort E. Asmi
title Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010
title_short Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010
title_full Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010
title_fullStr Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010
title_full_unstemmed Secondary new particle formation in Northern Finland Pallas site between the years 2000 and 2010
title_sort secondary new particle formation in northern finland pallas site between the years 2000 and 2010
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/acp-11-12959-2011
https://doaj.org/article/951504c2b3d7414597f6740d60c05fb3
genre Northern Finland
genre_facet Northern Finland
op_source Atmospheric Chemistry and Physics, Vol 11, Iss 24, Pp 12959-12972 (2011)
op_relation http://www.atmos-chem-phys.net/11/12959/2011/acp-11-12959-2011.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
doi:10.5194/acp-11-12959-2011
1680-7316
1680-7324
https://doaj.org/article/951504c2b3d7414597f6740d60c05fb3
op_doi https://doi.org/10.5194/acp-11-12959-2011
container_title Atmospheric Chemistry and Physics
container_volume 11
container_issue 24
container_start_page 12959
op_container_end_page 12972
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