Novel insights on new particle formation derived from a pan-european observing system

dc.bibliographicCitation.firstPage1482
dc.bibliographicCitation.issue1
dc.bibliographicCitation.volume8
dc.contributor.authorDall’Osto, M.
dc.contributor.authorBeddows, D.C.S.
dc.contributor.authorAsmi, A.
dc.contributor.authorPoulain, L.
dc.contributor.authorHao, L.
dc.contributor.authorFreney, E.
dc.contributor.authorAllan, J.D.
dc.contributor.authorCanagaratna, M.
dc.contributor.authorCrippa, M.
dc.contributor.authorBianchi, F.
dc.contributor.authorde Leeuw, G.
dc.contributor.authorEriksson, A.
dc.contributor.authorSwietlicki, E.
dc.contributor.authorHansson, H.C.
dc.contributor.authorHenzing, J.S.
dc.contributor.authorGranier, C.
dc.contributor.authorZemankova, K.
dc.contributor.authorLaj, P.
dc.contributor.authorOnasch, T.
dc.contributor.authorPrevot, A.
dc.contributor.authorPutaud, J. P.
dc.contributor.authorSellegri, K.
dc.contributor.authorVidal, M.
dc.contributor.authorVirtanen, A.
dc.contributor.authorSimo, R.
dc.contributor.authorWorsnop, D.
dc.contributor.authorO’Dowd, C.
dc.contributor.authorKulmala, M.
dc.contributor.authorHarrison, Roy M.
dc.date.accessioned2023-04-27T11:59:30Z
dc.date.available2023-04-27T11:59:30Z
dc.date.issued2018
dc.description.abstractThe formation of new atmospheric particles involves an initial step forming stable clusters less than a nanometre in size (<~1 nm), followed by growth into quasi-stable aerosol particles a few nanometres (~1-10 nm) and larger (>~10 nm). Although at times, the same species can be responsible for both processes, it is thought that more generally each step comprises differing chemical contributors. Here, we present a novel analysis of measurements from a unique multi-station ground-based observing system which reveals new insights into continental-scale patterns associated with new particle formation. Statistical cluster analysis of this unique 2-year multi-station dataset comprising size distribution and chemical composition reveals that across Europe, there are different major seasonal trends depending on geographical location, concomitant with diversity in nucleating species while it seems that the growth phase is dominated by organic aerosol formation. The diversity and seasonality of these events requires an advanced observing system to elucidate the key processes and species driving particle formation, along with detecting continental scale changes in aerosol formation into the future.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/12135
dc.identifier.urihttp://dx.doi.org/10.34657/11169
dc.language.isoeng
dc.publisherLondon : Nature Publishing Group
dc.relation.doihttps://doi.org/10.1038/s41598-017-17343-9
dc.relation.essn2045-2322
dc.relation.ispartofseriesScientific Reports 8 (2018), Nr. 1eng
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectaerosoleng
dc.subjectcluster analysiseng
dc.subjectEuropeeng
dc.subjectgrowth curveeng
dc.subjectseasonal variationeng
dc.subject.ddc500
dc.subject.ddc600
dc.titleNovel insights on new particle formation derived from a pan-european observing systemeng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleScientific Reports
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.subjectPhysikger
wgl.typeZeitschriftenartikelger
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