A statistical proxy for sulphuric acid concentration

dc.bibliographicCitation.firstPage11319eng
dc.bibliographicCitation.issue21eng
dc.bibliographicCitation.lastPage11334eng
dc.bibliographicCitation.volume11
dc.contributor.authorMikkonen, S.
dc.contributor.authorRomakkaniemi, S.
dc.contributor.authorSmith, J.N.
dc.contributor.authorKorhonen, H.
dc.contributor.authorPetäjä, T.
dc.contributor.authorPlass-Duelmer, C.
dc.contributor.authorBoy, M.
dc.contributor.authorMcMurry, P.H.
dc.contributor.authorLehtinen, K.E.J.
dc.contributor.authorJoutsensaari, J.
dc.contributor.authorHamed, A.
dc.contributor.authorMauldin III, R.L.
dc.contributor.authorBirmili, W.
dc.contributor.authorSpindler, G.
dc.contributor.authorArnold, F.
dc.contributor.authorKulmala, M.
dc.contributor.authorLaaksonen, A.
dc.date.accessioned2017-11-09T18:30:56Z
dc.date.available2019-06-26T17:17:50Z
dc.date.issued2011
dc.description.abstractGaseous sulphuric acid is a key precursor for new particle formation in the atmosphere. Previous experimental studies have confirmed a strong correlation between the number concentrations of freshly formed particles and the ambient concentrations of sulphuric acid. This study evaluates a body of experimental gas phase sulphuric acid concentrations, as measured by Chemical Ionization Mass Spectrometry (CIMS) during six intensive measurement campaigns and one long-term observational period. The campaign datasets were measured in Hyytiälä, Finland, in 2003 and 2007, in San Pietro Capofiume, Italy, in 2009, in Melpitz, Germany, in 2008, in Atlanta, Georgia, USA, in 2002, and in Niwot Ridge, Colorado, USA, in 2007. The long term data were obtained in Hohenpeissenberg, Germany, during 1998 to 2000. The measured time series were used to construct proximity measures ("proxies") for sulphuric acid concentration by using statistical analysis methods. The objective of this study is to find a proxy for sulfuric acid that is valid in as many different atmospheric environments as possible. Our most accurate and universal formulation of the sulphuric acid concentration proxy uses global solar radiation, SO2 concentration, condensation sink and relative humidity as predictor variables, yielding a correlation measure (R) of 0.87 between observed concentration and the proxy predictions. Interestingly, the role of the condensation sink in the proxy was only minor, since similarly accurate proxies could be constructed with global solar radiation and SO2 concentration alone. This could be attributed to SO2 being an indicator for anthropogenic pollution, including particulate and gaseous emissions which represent sinks for the OH radical that, in turn, is needed for the formation of sulphuric acid.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/734
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/476
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/acp-11-11319-2011
dc.relation.ispartofseriesAtmospheric Chemistry and Physics, Volume 11, Issue 21, Page 11319-11334eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectatmospheric chemistryeng
dc.subjectdata seteng
dc.subjectmass spectrometryeng
dc.subjectrelative humidityeng
dc.subjectsolar radiationeng
dc.subjectstatistical analysiseng
dc.subjectsulfur dioxideeng
dc.subjectsulfuric acideng
dc.subject.ddc550eng
dc.titleA statistical proxy for sulphuric acid concentrationeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Chemistry and Physicseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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