Meteorological and trace gas factors affecting the number concentration of atmospheric Aitken (DP Combining double low line 50 nm) particles in the continental boundary layer: Parameterization using a multivariate mixed effects model

dc.bibliographicCitation.firstPage1eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.lastPage13eng
dc.bibliographicCitation.volume4
dc.contributor.authorMikkonen, S.
dc.contributor.authorKorhonen, H.
dc.contributor.authorRomakkaniemi, S.
dc.contributor.authorSmith, J.N.
dc.contributor.authorJoutsensaari, J.
dc.contributor.authorLehtinen, K.E.J.
dc.contributor.authorHamed, A.
dc.contributor.authorBreider, T.J.
dc.contributor.authorBirmili, W.
dc.contributor.authorSpindler, G.
dc.contributor.authorPlass-Duelmer, C.
dc.contributor.authorFacchini, M.C.
dc.contributor.authorLaaksonen, A.
dc.date.accessioned2018-01-11T23:16:24Z
dc.date.available2019-06-26T17:21:18Z
dc.date.issued2011
dc.description.abstractMeasurements of aerosol size distribution and different gas and meteorological parameters, made in three polluted sites in Central and Southern Europe: Po Valley, Italy, Melpitz and Hohenpeissenberg in Germany, were analysed for this study to examine which of the meteorological and trace gas variables affect the number concentration of Aitken (Dp= 50 nm) particles. The aim of our study was to predict the number concentration of 50 nm particles by a combination of in-situ meteorological and gas phase parameters. The statistical model needs to describe, amongst others, the factors affecting the growth of newly formed aerosol particles (below 10 nm) to 50 nm size, but also sources of direct particle emissions in that size range. As the analysis method we used multivariate nonlinear mixed effects model. Hourly averages of gas and meteorological parameters measured at the stations were used as predictor variables; the best predictive model was attained with a combination of relative humidity, new particle formation event probability, temperature, condensation sink and concentrations of SO2, NO2 and ozone. The seasonal variation was also taken into account in the mixed model structure. Model simulations with the Global Model of Aerosol Processes (GLOMAP) indicate that the parameterization can be used as a part of a larger atmospheric model to predict the concentration of climatically active particles. As an additional benefit, the introduced model framework is, in theory, applicable for any kind of measured aerosol parameter.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1100
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/850
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/gmd-4-1-2011
dc.relation.ispartofseriesGeoscientific Model Development, Volume 4, Issue 1, Page 1-13eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectAitken nucleuseng
dc.subjectatmospheric modelingeng
dc.subjectatmospheric pollutioneng
dc.subjectboundary layereng
dc.subjectconcentration (composition)eng
dc.subjectcondensationeng
dc.subjectmultivariate analysiseng
dc.subjectnumerical modeleng
dc.subjectozoneeng
dc.subjectparameterizationeng
dc.subjectparticle sizeeng
dc.subjectrelative humidityeng
dc.subjectseasonal variationeng
dc.subjectsize distributioneng
dc.subjecttrace gaseng
dc.subject.ddc550eng
dc.titleMeteorological and trace gas factors affecting the number concentration of atmospheric Aitken (DP Combining double low line 50 nm) particles in the continental boundary layer: Parameterization using a multivariate mixed effects modeleng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleGeoscientific Model Developmenteng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
gmd-4-1-2011.pdf
Size:
681.65 KB
Format:
Adobe Portable Document Format
Description: