Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest

Secondary aerosol formation from gas-phase precursors is a frequent phenomenon occurring in a boreal environment. Traditionally, this process is identified visually from observational data on total and ion number size distributions. Here, we introduce a new, objective classification method for the n...

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Main Authors: Leino, Katri, Nieminen, Tuomo, Manninen, Hanna E., Petäjä, Tuukka, Kerminen, Veli-Matti, Kulmala, Markku
Other Authors: Department of Physics, Aerosol-Cloud-Climate -Interactions (ACCI)
Format: Article in Journal/Newspaper
Language:English
Published: Finnish Environment Institute 2016
Subjects:
Online Access:http://hdl.handle.net/10138/165318
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author Leino, Katri
Nieminen, Tuomo
Manninen, Hanna E.
Petäjä, Tuukka
Kerminen, Veli-Matti
Kulmala, Markku
author2 Department of Physics
Aerosol-Cloud-Climate -Interactions (ACCI)
author_facet Leino, Katri
Nieminen, Tuomo
Manninen, Hanna E.
Petäjä, Tuukka
Kerminen, Veli-Matti
Kulmala, Markku
author_sort Leino, Katri
collection HELDA – University of Helsinki Open Repository
description Secondary aerosol formation from gas-phase precursors is a frequent phenomenon occurring in a boreal environment. Traditionally, this process is identified visually from observational data on total and ion number size distributions. Here, we introduce a new, objective classification method for the new particle formation events based on measured intermediate-ion concentrations. The intermediate-ion concentration is a suitable indicator of new particle formation, because it is linked to the atmospheric new particle formation. The concentration of intermediate ions is typically very low (below 5 cm(-3)) when there is no new particle formation or precipitation events occurring. In this study, we analysed concentrations of negative intermediate ions at the Station for Measuring Ecosystem Atmosphere Relations (SMEAR II) in Hyytiala, Finland, during the years 2003-2013. We found that the half-hour median concentration of negative intermediate ions in sizes 2-4 nm was > 20 cm(-3) during 77.5% of event days classified by traditional method. The corresponding value was 92.3% in the case of 2-7 nm negative ions. In addition, the intermediate-ion concentration varied seasonally in a similar manner as the number of event days, peaking in the spring. A typical diurnal variation of the intermediate-ion concentration resembled that of the particle concentration during the event days. We developed here a new method for classifying new particle formation events based on intermediate-ion concentrations. The new method is complementary to the traditional event analysis and it can also be used as an automatic way of determining new particle formation events from large data sets. Peer reviewed
format Article in Journal/Newspaper
genre Arctic
genre_facet Arctic
id ftunivhelsihelda:oai:helda.helsinki.fi:10138/165318
institution Open Polar
language English
op_collection_id ftunivhelsihelda
op_relation This research was supported by the European Research Council (ERC) Advanced Grant (ATM-NUCLE, 227463), the European Union's Horizon 2020 research and innovation programme under grant agreement no. 654109 (ACTRIS-2), CRAICC project (Cryosphere-Atmosphere Interaction in a Changing Arctic Climate) and the Academy of Finland Centre of Excellence program (projects no. 1118615 and 272041). The research leading to these results has received funding also from the European Union Seventh Framework Programme (FP7/2007-2013 ACTRIS) under grant agreement no. 262254 and European Union's Horizon 2020 research and innovation programme under grant agreement no. 654109 (ACTRIS2).
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spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/165318 2025-02-16T15:00:56+00:00 Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest Leino, Katri Nieminen, Tuomo Manninen, Hanna E. Petäjä, Tuukka Kerminen, Veli-Matti Kulmala, Markku Department of Physics Aerosol-Cloud-Climate -Interactions (ACCI) 2016-08-08T09:05:01Z 13 application/pdf http://hdl.handle.net/10138/165318 eng eng Finnish Environment Institute This research was supported by the European Research Council (ERC) Advanced Grant (ATM-NUCLE, 227463), the European Union's Horizon 2020 research and innovation programme under grant agreement no. 654109 (ACTRIS-2), CRAICC project (Cryosphere-Atmosphere Interaction in a Changing Arctic Climate) and the Academy of Finland Centre of Excellence program (projects no. 1118615 and 272041). The research leading to these results has received funding also from the European Union Seventh Framework Programme (FP7/2007-2013 ACTRIS) under grant agreement no. 262254 and European Union's Horizon 2020 research and innovation programme under grant agreement no. 654109 (ACTRIS2). http://hdl.handle.net/10138/165318 84970968608 000378019700007 other info:eu-repo/semantics/openAccess openAccess AEROSOL-SIZE DISTRIBUTIONS ATMOSPHERIC IONS FORMATION EVENTS GROWTH-RATES SMEAR-II NUCLEATION AIR SPECTROMETER MOBILITY CLUSTERS Physical sciences Environmental sciences Article publishedVersion 2016 ftunivhelsihelda 2025-01-21T16:11:30Z Secondary aerosol formation from gas-phase precursors is a frequent phenomenon occurring in a boreal environment. Traditionally, this process is identified visually from observational data on total and ion number size distributions. Here, we introduce a new, objective classification method for the new particle formation events based on measured intermediate-ion concentrations. The intermediate-ion concentration is a suitable indicator of new particle formation, because it is linked to the atmospheric new particle formation. The concentration of intermediate ions is typically very low (below 5 cm(-3)) when there is no new particle formation or precipitation events occurring. In this study, we analysed concentrations of negative intermediate ions at the Station for Measuring Ecosystem Atmosphere Relations (SMEAR II) in Hyytiala, Finland, during the years 2003-2013. We found that the half-hour median concentration of negative intermediate ions in sizes 2-4 nm was > 20 cm(-3) during 77.5% of event days classified by traditional method. The corresponding value was 92.3% in the case of 2-7 nm negative ions. In addition, the intermediate-ion concentration varied seasonally in a similar manner as the number of event days, peaking in the spring. A typical diurnal variation of the intermediate-ion concentration resembled that of the particle concentration during the event days. We developed here a new method for classifying new particle formation events based on intermediate-ion concentrations. The new method is complementary to the traditional event analysis and it can also be used as an automatic way of determining new particle formation events from large data sets. Peer reviewed Article in Journal/Newspaper Arctic HELDA – University of Helsinki Open Repository
spellingShingle AEROSOL-SIZE DISTRIBUTIONS
ATMOSPHERIC IONS
FORMATION EVENTS
GROWTH-RATES
SMEAR-II
NUCLEATION
AIR
SPECTROMETER
MOBILITY
CLUSTERS
Physical sciences
Environmental sciences
Leino, Katri
Nieminen, Tuomo
Manninen, Hanna E.
Petäjä, Tuukka
Kerminen, Veli-Matti
Kulmala, Markku
Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
title Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
title_full Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
title_fullStr Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
title_full_unstemmed Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
title_short Intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
title_sort intermediate ions as a strong indicator of new particle formation bursts in a boreal forest
topic AEROSOL-SIZE DISTRIBUTIONS
ATMOSPHERIC IONS
FORMATION EVENTS
GROWTH-RATES
SMEAR-II
NUCLEATION
AIR
SPECTROMETER
MOBILITY
CLUSTERS
Physical sciences
Environmental sciences
topic_facet AEROSOL-SIZE DISTRIBUTIONS
ATMOSPHERIC IONS
FORMATION EVENTS
GROWTH-RATES
SMEAR-II
NUCLEATION
AIR
SPECTROMETER
MOBILITY
CLUSTERS
Physical sciences
Environmental sciences
url http://hdl.handle.net/10138/165318