Atmospheric new particle formation at Utö, Baltic Sea 2003-2005

dc.bibliographicCitation.firstPage345
dc.bibliographicCitation.issue3eng
dc.bibliographicCitation.lastPage352
dc.bibliographicCitation.volume60
dc.contributor.authorHyvärinen, A.-P.
dc.contributor.authorKomppula, M.
dc.contributor.authorEngler, C.
dc.contributor.authorKivekäs, N.
dc.contributor.authorKerminen, V.-M.
dc.contributor.authorDal Maso, M.
dc.contributor.authorViisanen, Y.
dc.contributor.authorLihavainen, H.
dc.date.accessioned2018-02-07T16:38:50Z
dc.date.available2019-06-26T17:17:23Z
dc.date.issued2017
dc.description.abstractNearly 3 yr (March 2003–December 2005) of continuous particle number size distribution measurements have been conducted at the island of Ut¨o in the Baltic Sea. The measured particle size range was from 7 to 530 nm. During the measurement period, a total of 103 regional new-particle formation events were observed. The characteristics of the nucleation events at Ut¨o were similar to those reported in the literature in other Nordic sites, though measured condensation sinks were rather high (geometric mean of 3.8 × 10−3 s−1) during event days. Clear evidence was found that new particles nucleate regionally near Ut¨o, rather than are transported from greater distances. However, the Baltic Sea seems to have an inhibiting effect on new-particle formation. The boreal forest areas in the continental Finland were found to have an enhancing effect on the nucleation probability in Ut¨o, suggesting that at least some of the precursor gases for nucleation and/or condensational growth of particles originate from these forests. In addition to regional new-particle formation events, a total of 94 local events were observed in Ut¨o. These are short-lived events with a small footprint area, and can at least partly be tracked down to the emissions of ship traffic operating at Ut¨o.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/788
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/377
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2008.00343.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 60, Issue 3, Page 345-352eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosol formationeng
dc.subjectatmospheric sinkeng
dc.subjectnucleationeng
dc.subjectparticle sizeeng
dc.subjectprobabilityeng
dc.subjectsize distributioneng
dc.subject.ddc550eng
dc.titleAtmospheric new particle formation at Utö, Baltic Sea 2003-2005eng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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