Infrequent new particle formation over the remote boreal forest of Siberia

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dc.bibliographicCitation.firstPage167eng
dc.bibliographicCitation.journalTitleAtmospheric environmenteng
dc.bibliographicCitation.lastPage169eng
dc.bibliographicCitation.volume200eng
dc.contributor.authorWiedensohler, A.
dc.contributor.authorMa, N.
dc.contributor.authorBirmili, W.
dc.contributor.authorHeintzenberg, J.
dc.contributor.authorDitas, F.
dc.contributor.authorAndreae, M.O.
dc.contributor.authorPanov, A.
dc.date.accessioned2021-10-15T05:04:44Z
dc.date.available2021-10-15T05:04:44Z
dc.date.issued2018
dc.description.abstractAerosol particle number size distributions (PNSD) were investigated to verify, if extremely low-volatility organic vapors (ELVOC) from natural sources alone could induce new particle formation and growth events over the remote boreal forest region of Siberia, hundreds of kilometers away from significant anthropogenic sources. We re-evaluated observations determined at a height of 300 m of the remote observatory ZOTTO (Zotino Tall Tower Observatory, http://www.zottoproject.org). We found that new particle formation events occurred only on 11 days in a 3-year period, suggesting that homogeneous nucleation with a subsequent condensational growth could not be the major process, maintaining the particle number concentration in the planetary boundary layer of the remote boreal forest area of Siberia. © 2018 Elsevier Ltdeng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6985
dc.identifier.urihttps://doi.org/10.34657/6032
dc.language.isoengeng
dc.publisherAmsterdam [u.a.] : Elsevier Scienceeng
dc.relation.doihttps://doi.org/10.1016/j.atmosenv.2018.12.013
dc.relation.essn1873-2844
dc.relation.issn0004-6981
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.ddc690eng
dc.subject.otherBoundary layerseng
dc.subject.otherNucleationeng
dc.subject.otherObservatorieseng
dc.subject.otherAerosol particleseng
dc.subject.otherAnthropogenic sourceseng
dc.subject.otherCondensational growtheng
dc.subject.otherHomogeneous nucleationeng
dc.subject.otherNatural sourceseng
dc.subject.otherNew particle formationeng
dc.subject.otherParticle number concentrationeng
dc.subject.otherPlanetary boundary layerseng
dc.subject.otherForestryeng
dc.subject.otheraerosoleng
dc.subject.otheranthropogenic sourceeng
dc.subject.otherboreal foresteng
dc.subject.otherboundary layereng
dc.subject.otherforest covereng
dc.subject.othernucleationeng
dc.subject.otherobservatoryeng
dc.subject.othersize distributioneng
dc.subject.otherarticleeng
dc.subject.otherboundary layereng
dc.subject.otherconcentration (parameters)eng
dc.subject.otherheighteng
dc.subject.otherRussian Federationeng
dc.subject.othertaigaeng
dc.subject.otherSiberiaeng
dc.titleInfrequent new particle formation over the remote boreal forest of Siberiaeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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