Global analysis of continental boundary layer new particle formation based on long-term measurements

dc.bibliographicCitation.firstPage14737
dc.bibliographicCitation.issue19
dc.bibliographicCitation.lastPage14756
dc.bibliographicCitation.volume18
dc.contributor.authorNieminen, Tuomo
dc.contributor.authorKerminen, Veli-Matti
dc.contributor.authorPetäjä, Tuukka
dc.contributor.authorAalto, Pasi P.
dc.contributor.authorArshinov, Mikhail
dc.contributor.authorAsmi, Eija
dc.contributor.authorBaltensperger, Urs
dc.contributor.authorBeddows, David C. S.
dc.contributor.authorBeukes, Johan Paul
dc.contributor.authorCollins, Don
dc.contributor.authorDing, Aijun
dc.contributor.authorHarrison, Roy M.
dc.contributor.authorHenzing, Bas
dc.contributor.authorHooda, Rakesh
dc.contributor.authorHu, Min
dc.contributor.authorHõrrak, Urmas
dc.contributor.authorKivekäs, Niku
dc.contributor.authorKomsaare, Kaupo
dc.contributor.authorKrejci, Radovan
dc.contributor.authorKristensson, Adam
dc.contributor.authorLaakso, Lauri
dc.contributor.authorLaaksonen, Ari
dc.contributor.authorLeaitch, W. Richard
dc.contributor.authorLihavainen, Heikki
dc.contributor.authorMihalopoulos, Nikolaos
dc.contributor.authorNémeth, Zoltán
dc.contributor.authorNie, Wei
dc.contributor.authorO'Dowd, Colin
dc.contributor.authorSalma, Imre
dc.contributor.authorSellegri, Karine
dc.contributor.authorSvenningsson, Birgitta
dc.contributor.authorSwietlicki, Erik
dc.contributor.authorTunved, Peter
dc.contributor.authorUlevicius, Vidmantas
dc.contributor.authorVakkari, Ville
dc.contributor.authorVana, Marko
dc.contributor.authorWiedensohler, Alfred
dc.contributor.authorWu, Zhijun
dc.contributor.authorVirtanen, Annele
dc.contributor.authorKulmala, Markku
dc.date.accessioned2023-03-07T10:42:54Z
dc.date.available2023-03-07T10:42:54Z
dc.date.issued2018
dc.description.abstractAtmospheric new particle formation (NPF) is an important phenomenon in terms of global particle number concentrations. Here we investigated the frequency of NPF, formation rates of 10 nm particles, and growth rates in the size range of 10–25 nm using at least 1 year of aerosol number size-distribution observations at 36 different locations around the world. The majority of these measurement sites are in the Northern Hemisphere. We found that the NPF frequency has a strong seasonal variability. At the measurement sites analyzed in this study, NPF occurs most frequently in March–May (on about 30 % of the days) and least frequently in December-February (about 10 % of the days). The median formation rate of 10 nm particles varies by about 3 orders of magnitude (0.01–10 cm−3 s−1) and the growth rate by about an order of magnitude (1–10 nm h−1). The smallest values of both formation and growth rates were observed at polar sites and the largest ones in urban environments or anthropogenically influenced rural sites. The correlation between the NPF event frequency and the particle formation and growth rate was at best moderate among the different measurement sites, as well as among the sites belonging to a certain environmental regime. For a better understanding of atmospheric NPF and its regional importance, we would need more observational data from different urban areas in practically all parts of the world, from additional remote and rural locations in North America, Asia, and most of the Southern Hemisphere (especially Australia), from polar areas, and from at least a few locations over the oceans.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/11720
dc.identifier.urihttp://dx.doi.org/10.34657/10753
dc.language.isoeng
dc.publisherKatlenburg-Lindau : EGU
dc.relation.doihttps://doi.org/10.5194/acp-18-14737-2018
dc.relation.essn1680-7324
dc.relation.ispartofseriesAtmospheric chemistry and physics 18 (2018), Nr. 19
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0
dc.subjectaerosol-size distributioneng
dc.subjecthigh-altitude siteeng
dc.subjectcondensation nuclei productioneng
dc.subjectformation eventseng
dc.subjectatmospheric nucleationeng
dc.subjectfree troposphereeng
dc.subjectsulfuric-acideng
dc.subjectblack carboneng
dc.subjectairborne measurementseng
dc.subjectparticulate mattereng
dc.subject.ddc550
dc.titleGlobal analysis of continental boundary layer new particle formation based on long-term measurementseng
dc.typearticle
dc.typeText
dcterms.bibliographicCitation.journalTitleAtmospheric chemistry and physics
tib.accessRightsopenAccess
wgl.contributorTROPOS
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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