The contribution of sulphuric acid to atmospheric particle formation and growth: A comparison between boundary layers in Northern and Central Europe

dc.bibliographicCitation.firstPage1773eng
dc.bibliographicCitation.issue7eng
dc.bibliographicCitation.lastPage1785eng
dc.bibliographicCitation.volume5
dc.contributor.authorFiedler, V.
dc.contributor.authorDal Maso, M.
dc.contributor.authorBoy, M.
dc.contributor.authorAufmhoff, H.
dc.contributor.authorHoffmann, J.
dc.contributor.authorSchuck, T.
dc.contributor.authorBirmili, W.
dc.contributor.authorHanke, M.
dc.contributor.authorUecker, J.
dc.contributor.authorArnold, F.
dc.contributor.authorKulmala, M.
dc.date.accessioned2017-10-05T12:59:54Z
dc.date.available2019-06-26T17:17:42Z
dc.date.issued2005
dc.description.abstractAtmospheric gaseous sulphuric acid was measured and its influence on particle formation and growth was investigated building on aerosol data. The measurements were part of the EU-project QUEST and took place at two different measurement sites in Northern and Central Europe (Hyytiälä, Finland, March-April 2003 and Heidelberg, Germany, March-April 2004). From a comprehensive data set including sulphuric acid, particle number size distributions and meteorological data, particle growth rates, particle formation rates and source rates of condensable vapors were inferred. Growth rates were determined in two different ways, from particle size distributions as well as from a so-called timeshift analysis. Moreover, correlations between sulphuric acid and particle number concentration between 3 and 6 nm were examined and the influence of air masses of different origin was investigated. Measured maximum concentrations of sulphuric acid were in the range from 1x106 to 16x106cm-3. The gaseous sulphuric acid lifetime with respect to condensation on aerosol particles ranged from 2 to 33min in Hyytiälä and from 0.5 to 8 min in Heidelberg. Most calculated values (growth rates, formation rates, vapor source rates) were considerably higher in Central Europe (Heidelberg), due to the more polluted air and higher preexistent aerosol concentrations. Close correlations between H2SO4 and nucleation mode particles (size range: 3-6 nm) were found on most days at both sites. The percentage contribution of sulphuric acid to particle growth was below 10% at both places and to initial growth below 20%. An air mass analysis indicated that at Heidelberg new particles were formed predominantly in air advected from southwesterly directions.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1309
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/452
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-5-1773-2005
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 5, Issue 7, Page 1773-1785eng
dc.rights.licenseCC BY-NC-SA 2.5 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by-nc-sa/2.5/eng
dc.subjectatmospheric chemistryeng
dc.subjectatmospheric particleeng
dc.subjectboundary layereng
dc.subjectgrowth rateeng
dc.subjectsulfuric acideng
dc.subject.ddc550eng
dc.titleThe contribution of sulphuric acid to atmospheric particle formation and growth: A comparison between boundary layers in Northern and Central Europeeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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