Optical and microphysical properties of smoke over Cape Verde inferred from multiwavelength lidar measurements

dc.bibliographicCitation.firstPage677
dc.bibliographicCitation.issue4eng
dc.bibliographicCitation.lastPage694
dc.bibliographicCitation.volume63
dc.contributor.authorTesche, Matthias
dc.contributor.authorMüller, Detlef
dc.contributor.authorGross, Silke
dc.contributor.authorAnsmann, Albert
dc.contributor.authorAlthausen, Dietrich
dc.contributor.authorFreudenthaler, Volker
dc.contributor.authorWeinzierl, Bernadett
dc.contributor.authorVeira, Andreas
dc.contributor.authorPetzold, Andreas
dc.date.accessioned2018-02-03T04:36:12Z
dc.date.available2019-06-26T17:17:07Z
dc.date.issued2017
dc.description.abstractLidar measurements of mixed dust/smoke plumes over the tropical Atlantic ocean were carried out during the winter campaign of SAMUM-2 at Cape Verde. Profiles of backscatter and extinction coefficients, lidar ratios, and Ångstr¨om exponents related to pure biomass-burning aerosol from southern West Africa were extracted from these observations. Furthermore, these findings were used as input for an inversion algorithm to retrieve microphysical properties of pure smoke. Seven measurement days were found suitable for the procedure of aerosol-type separation and successive inversion of optical data that describe biomass-burning smoke. We inferred high smoke lidar ratios of 87 ± 17 sr at 355 nm and 79 ± 17 sr at 532 nm. Smoke lidar ratios and Ångstr¨om exponents are higher compared to the ones for the dust/smoke mixture. These numbers indicate higher absorption and smaller sizes for pure smoke particles compared to the dust/smoke mixture. Inversion of the smoke data set results in mean effective radii of 0.22 ± 0.08 μm with individual results varying between 0.10 and 0.36 μm. The single-scattering albedo for pure biomass-burning smoke was found to vary between 0.63 and 0.89 with a very low mean value of 0.75 ± 0.07. This is in good agreement with findings of airborne in situ measurements which showed values of 0.77 ± 0.03. Effective radii from the inversion were similar to the ones found for the fine mode of the in situ size distributions.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1157
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/291
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Franciseng
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2011.00549.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 63, Issue 4, Page 677 -694eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosoleng
dc.subjectbackscattereng
dc.subjectbiomass burningeng
dc.subjectdusteng
dc.subjectextinction coefficienteng
dc.subjectin situ measurementeng
dc.subjectlidareng
dc.subjectlight scatteringeng
dc.subjectoptical propertyeng
dc.subjectsize distributioneng
dc.subjectsmokeeng
dc.subject.ddc550eng
dc.titleOptical and microphysical properties of smoke over Cape Verde inferred from multiwavelength lidar measurementseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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