Depolarization ratio profiling at several wavelengths in pure Saharan dust during SAMUM 2006

dc.bibliographicCitation.firstPage165
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.lastPage179
dc.bibliographicCitation.volume61
dc.contributor.authorFreudenthaler, Volker
dc.contributor.authorEsselborn, Michael
dc.contributor.authorWiegner, Matthias
dc.contributor.authorHeese, Birgit
dc.contributor.authorTesche, Matthias
dc.contributor.authorAnsmann, Albert
dc.contributor.authorMüller, Detlef
dc.contributor.authorAlthausen, Dietrich
dc.contributor.authorWirth, Martin
dc.contributor.authorFix, Andreas
dc.contributor.authorEhret, Gerhard
dc.contributor.authorKnippertz, Peter
dc.contributor.authorToledano, Carlos
dc.contributor.authorGasteiger, Josef
dc.contributor.authorGarhammer, Markus
dc.contributor.authorSeefeldner, Meinhard
dc.date.accessioned2018-02-06T16:38:27Z
dc.date.available2019-06-26T17:17:16Z
dc.date.issued2017
dc.description.abstractVertical profiles of the linear particle depolarization ratio of pure dust clouds were measured during the Saharan Mineral Dust Experiment (SAMUM) at Ouarzazate, Morocco (30.9◦N, –6.9◦E), close to source regions in May–June 2006, with four lidar systems at four wavelengths (355, 532, 710 and 1064 nm). The intercomparison of the lidar systems is accompanied by a discussion of the different calibration methods, including a new, advanced method, and a detailed error analysis. Over the whole SAMUM periode pure dust layers show a mean linear particle depolarization ratio at 532 nm of 0.31, in the range between 0.27 and 0.35, with a mean Ångström exponent (AE, 440–870 nm) of 0.18 (range 0.04–0.34) and still high mean linear particle depolarization ratio between 0.21 and 0.25 during periods with aerosol optical thickness less than 0.1, with a mean AE of 0.76 (range 0.65–1.00), which represents a negative correlation of the linear particle depolarization ratio with the AE. A slight decrease of the linear particle depolarization ratio with wavelength was found between 532 and 1064 nm from 0.31 ± 0.03 to 0.27 ± 0.04.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/863
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/345
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2008.00396.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 61, Issue 1, Page 165-179eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosoleng
dc.subjectdusteng
dc.subjectoptical deptheng
dc.subjectparticle sizeeng
dc.subjectsize distributioneng
dc.subjectvertical profileeng
dc.subjectwavelengtheng
dc.subject.ddc550eng
dc.titleDepolarization ratio profiling at several wavelengths in pure Saharan dust during SAMUM 2006eng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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