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

dc.contributor.authorDall'Osto, Manuel
dc.contributor.authorBeddows, David 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 Barcelona, Montserrat
dc.contributor.authorVirtanen, A.
dc.contributor.authorSimó, Rafel
dc.contributor.authorWorsnop, D.
dc.contributor.authorO'Dowd, Colin
dc.contributor.authorKulmala, M.
dc.contributor.authorHarrison, Roy M.
dc.date.accessioned2018-11-08T16:34:02Z
dc.date.available2018-11-08T16:34:02Z
dc.date.issued2018-01-24
dc.date.updated2018-11-08T16:34:02Z
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.
dc.format.extent11 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec679138
dc.identifier.issn2045-2322
dc.identifier.pmid29367716
dc.identifier.urihttps://hdl.handle.net/2445/125931
dc.language.isoeng
dc.publisherNature Publishing Group
dc.relation.isformatofReproducció del document publicat a: https://doi.org/10.1038/s41598-017-17343-9
dc.relation.ispartofScientific Reports, 2018, vol. 8, p. 1482
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/H2020/654109/EU//ACTRIS-2
dc.relation.projectIDinfo:eu-repo/grantAgreement/EC/FP7/624680/EU//MANU
dc.relation.urihttps://doi.org/10.1038/s41598-017-17343-9
dc.rightscc-by (c) Dall'Osto, M. et al., 2018
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es
dc.sourceArticles publicats en revistes (Biologia Evolutiva, Ecologia i Ciències Ambientals)
dc.subject.classificationOzó atmosfèric
dc.subject.classificationContaminació atmosfèrica
dc.subject.otherAtmospheric ozone
dc.subject.otherAtmospheric pollution
dc.titleNovel insights on new particle formation derived from a pan- european observing system
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion

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