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dc.contributor.authorLaakso, L.
dc.contributor.authorHirsikko, T.
dc.contributor.authorNieminen, S.
dc.contributor.authorGagné, S.
dc.contributor.authorLehtipalo, K.
dc.date.accessioned2012-09-10T10:30:59Z
dc.date.available2012-09-10T10:30:59Z
dc.date.issued2011
dc.identifier.citationHirsikko, T. et al. 2011. Atmospheric ions and nucleation: a review of observations. Atmospheric chemistry and physics, 11(2):767-798. [http://www.atmospheric-chemistry-and-physics.net]en_US
dc.identifier.issn1680-7316
dc.identifier.issn1680-7324 (eISSN)
dc.identifier.urihttp://hdl.handle.net/10394/7260
dc.description.abstractThis review is based on ca. 260 publications, 93 of which included data on the temporal and spatial variation of the concentration of small ions (<1.6 nm in diameter) especially in the lower troposphere, chemical composition, or formation and growth rates of sub-3 nm ions. This information was collected on tables and figures. The small ions exist all the time in the atmosphere, and the average concentrations of positive and negative small ions are typically 200–2500 cm−3. However, concentrations up to 5000 cm−3 have been observed. The results are in agreement with observations of ion production rates in the atmosphere. We also summarised observations on the conversion of small ions to intermediate ions, which can act as embryos for new atmospheric aerosol particles. Those observations include the formation rates (J2[ion]) of 2-nm intermediate ions, growth rates (GR[ion]) of sub-3 nm ions, and information on the chemical composition of the ions. Unfortunately, there were only a few studies which presented J2[ion] and GR[ion]. Based on the publications, the formation rates of 2-nm ions were 0–1.1 cm−3 s−1, while the total 2-nm particle formation rates varied between 0.001 and 60 cm−3 s−1. Due to small changes in J2[ion], the relative importance of ions in 2-nm particle formation was determined by the large changes in J2[tot], and, accordingly the contribution of ions increased with decreasing J2[tot]. Furthermore, small ions were observed to activate for growth earlier than neutral nanometer-sized particles and at lower saturation ratio of condensing vapours.(anonymous or attributed), additional short comments by other members of the scientific community (attributed) and the authors' replies are also published in ACPD. In the second stage, the peer-review process is completed and, if accepted, the final revised papers are published in ACP. To ensure publication precedence for authors, and to provide a lasting record of scientific discussion, ACPD and ACP are both ISSN-registered, permanently archived and fully citable.en_US
dc.description.urihttp://dx.doi.org/10.5194/acp-11-767-2011
dc.description.urihttp://www.atmos-chem-phys.net/11/767/2011/acp-11-767-2011.pdf
dc.language.isoenen_US
dc.publisherCopernicus Publicationsen_US
dc.titleAtmospheric ions and nucleation: a review of observationsen_US
dc.typeArticleen_US


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