EARLINET observations of the 14-22-May long-range dust transport event during SAMUM 2006: Validation of results from dust transport modelling

dc.bibliographicCitation.firstPage325
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.lastPage339
dc.bibliographicCitation.volume61
dc.contributor.authorMüller, D.
dc.contributor.authorHeinold, B.
dc.contributor.authorTesche, M.
dc.contributor.authorTegen, I.
dc.contributor.authorAlthausen, D.
dc.contributor.authorAlados Arboledas, L.
dc.contributor.authorAmiridis, V.
dc.contributor.authorAmodeo, A.
dc.contributor.authorAnsmann, A.
dc.contributor.authorBalis, D.
dc.contributor.authorComeron, A.
dc.contributor.authorD’mico, G.
dc.contributor.authorGerasopoulos, E.
dc.contributor.authorGuerrero-Rascado, J.L.
dc.contributor.authorFreudenthaler, V.
dc.contributor.authorGiannakaki, E.
dc.contributor.authorHeese, B.
dc.contributor.authorIarlori, M.
dc.contributor.authorKnippertz, P.
dc.contributor.authorMamouri, R.E.
dc.contributor.authorMona, L.
dc.contributor.authorPapayannis, A.
dc.contributor.authorPappalardo, G.
dc.contributor.authorPerrone, R-M.
dc.contributor.authorPisani, G.
dc.contributor.authorRizi, V.
dc.contributor.authorSicard, M.
dc.contributor.authorSpinelli, N.
dc.contributor.authorTafuro, A.
dc.contributor.authorWiegner, M.
dc.date.accessioned2018-02-06T04:38:09Z
dc.date.available2019-06-26T17:17:13Z
dc.date.issued2017
dc.description.abstractWe observed a long-range transport event of mineral dust from North Africa to South Europe during the Saharan Mineral Dust Experiment (SAMUM) 2006. Geometrical and optical properties of that dust plume were determined with Sun photometer of the Aerosol Robotic Network (AERONET) and Raman lidar near the North African source region, and with Sun photometers of AERONET and lidars of the European Aerosol Research Lidar Network (EARLINET) in the far field in Europe. Extinction-to-backscatter ratios of the dust plume over Morocco and Southern Europe do not differ. Ångstr¨om exponents increase with distance from Morocco. We simulated the transport, and geometrical and optical properties of the dust plume with a dust transport model. The model results and the experimental data show similar times regarding the appearance of the dust plume over each EARLINET site. Dust optical depth from the model agrees in most cases to particle optical depth measured with the Sun photometers. The vertical distribution of the mineral dust could be satisfactorily reproduced, if we use as benchmark the extinction profiles measured with lidar. In some cases we find differences. We assume that insufficient vertical resolution of the dust plume in the model calculations is one reason for these deviations.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/915
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/328
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2008.00400.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 61, Issue 1, Page 325-339eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosoleng
dc.subjectatmospheric transporteng
dc.subjectbackscattereng
dc.subjectdusteng
dc.subjectexperimental studyeng
dc.subjectlidareng
dc.subjectlong range transporteng
dc.subjectobservational methodeng
dc.subjectoptical deptheng
dc.subjectphotometereng
dc.subjectvertical distributioneng
dc.subject.ddc550eng
dc.titleEARLINET observations of the 14-22-May long-range dust transport event during SAMUM 2006: Validation of results from dust transport modellingeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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