Do new sea spray aerosol source functions improve the results of a regional aerosol model?

dc.bibliographicCitation.firstPage265eng
dc.bibliographicCitation.journalTitleAtmospheric environmenteng
dc.bibliographicCitation.lastPage278eng
dc.bibliographicCitation.volume198eng
dc.contributor.authorBarthel, Stefan
dc.contributor.authorTegen, Ina
dc.contributor.authorWolke, Ralf
dc.date.accessioned2021-10-14T09:00:30Z
dc.date.available2021-10-14T09:00:30Z
dc.date.issued2018
dc.description.abstractSea spray aerosol particle is a dominating part of the global aerosol mass load of natural origin. Thus, it strongly influences the atmospheric radiation balance and cloud properties especially over the oceans. Uncertainties of the estimated climate impacts by this aerosol type are partly caused by the uncertainties in the particle size dependent emission fluxes of sea spray aerosol particle. We present simulations with a regional aerosol transport model system in two domains, for three months and compared the model results to measurements at four stations using various sea spray aerosol particle source source functions. Despite these limitations we found the results using different source functions are within the range of most model uncertainties. Especially the model's ability to produce realistic wind speeds is crucial. Furthermore, the model results are more affected by a function correcting the emission flux for the effect of the sea surface temperature than by the use of different source functions. © 2018 The Authorseng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6983
dc.identifier.urihttps://doi.org/10.34657/6030
dc.language.isoengeng
dc.publisherAmsterdam [u.a.] : Elsevier Scienceeng
dc.relation.doihttps://doi.org/10.1016/j.atmosenv.2018.10.016
dc.relation.essn1873-2844
dc.relation.issn0004-6981
dc.rights.licenseCC BY-NC-ND 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/eng
dc.subject.ddc550eng
dc.subject.otherAerosolseng
dc.subject.otherAtmospheric radiationeng
dc.subject.otherAtmospheric temperatureeng
dc.subject.otherOceanographyeng
dc.subject.otherParticle sizeeng
dc.subject.otherSubmarine geophysicseng
dc.subject.otherSurface propertieseng
dc.subject.otherSurface waterseng
dc.subject.otherUncertaintyeng
dc.subject.otheranalysiseng
dc.subject.otherAerosol modelingeng
dc.subject.otherAerosol transport modeleng
dc.subject.otherCloud propertieseng
dc.subject.otherMarine aerosolseng
dc.subject.otherModel uncertaintieseng
dc.subject.otherSea spray aerosolseng
dc.subject.otherSea surface temperature (SST)eng
dc.subject.otherSource functionseng
dc.subject.otherAtmospheric movementseng
dc.subject.otheraerosoleng
dc.subject.othermarine environmenteng
dc.subject.othermeasurement methodeng
dc.subject.othermodelingeng
dc.subject.otherparticle sizeeng
dc.subject.otherradiation balanceeng
dc.subject.othersea surfaceeng
dc.subject.othertemperatureeng
dc.subject.othersimulationeng
dc.subject.otheruncertainty analysiseng
dc.subject.otheraerosoleng
dc.subject.otherarticleeng
dc.subject.othersea surface temperatureeng
dc.subject.othersimulationeng
dc.subject.otheruncertaintyeng
dc.subject.otherwind speedeng
dc.titleDo new sea spray aerosol source functions improve the results of a regional aerosol model?eng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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