Profiling of Saharan dust and biomass-burning smoke with multiwavelength polarization Raman lidar at Cape Verde

dc.bibliographicCitation.firstPage649
dc.bibliographicCitation.issue4eng
dc.bibliographicCitation.lastPage676
dc.bibliographicCitation.volume63
dc.contributor.authorTesche, Matthias
dc.contributor.authorGross, Silke
dc.contributor.authorAnsmann, Albert
dc.contributor.authorMüller, Detlef
dc.contributor.authorAlthausen, Dietrich
dc.contributor.authorFreudenthaler, Volker
dc.contributor.authorEsselborn, Michael
dc.date.accessioned2018-02-05T16:37:42Z
dc.date.available2019-06-26T17:17:08Z
dc.date.issued2017
dc.description.abstractExtensive lidar measurements of Saharan dust and biomass-burning smoke were performed with one airborne and three ground-based instruments in the framework of the second part of the SAharan Mineral dUst experiMent (SAMUM-2a) during January and February of 2008 at Cape Verde. Further lidar observations with one system only were conducted duringMay and June of 2008 (SAMUM-2b). The active measurements were supported by Sun photometer observations. During winter, layers of mineral dust from the Sahara and biomass-burning smoke from southern West Africa pass Cape Verde on their way to South America while pure dust layers cross the Atlantic on their way to the Caribbean during summer. The mean 500-nm aerosol optical thickness (AOT) observed during SAMUM-2a was 0.35 ± 0.18. SAMUM-2a observations showed transport of pure dust within the lowermost 1.5 km of the atmospheric column. In the height range from 1.5 to 5.0 km, mixed dust/smoke layers with mean lidar ratios of 67 ± 14 sr at 355 and 532 nm, respectively, prevailed. Within these layers, wavelength-independent linear particle depolarization ratios of 0.12–0.18 at 355, 532, and 710 nm indicate a large contribution (30–70%) of mineral dust to the measured optical properties. Ångstr¨om exponents for backscatter and extinction of around 0.7 support this finding. Mean extinction coefficients in the height range between 2 and 4 km were 66 ± 6 Mm−1 at 355 nm and 48 ± 5 Mm−1 at 532 nm. Comparisons with airborne high-spectral-resolution lidar observations show good agreement within the elevated layers. 3–5 km deep dust layers where observed during SAMUM-2b. These layers showed optical properties similar to the ones of SAMUM-1 in Morocco with a mean 500-nm AOT of 0.4 ± 0.2. Dust extinction coefficients were about 80 ± 6 Mm−1 at 355 and 532 nm. Dust lidar ratios were 53 ± 10 sr at 355 and 532 nm, respectively. Dust depolarization ratios showed an increase with wavelength from 0.31 ± 0.10 at 532 nm to 0.37 ± 0.07 at 710 nm.
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1198
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/294
dc.language.isoengeng
dc.publisherMilton Park : Taylor & Francis
dc.relation.doihttps://doi.org/10.1111/j.1600-0889.2011.00548.x
dc.relation.ispartofseriesTellus B: Chemical and Physical Meteorology, Volume 63, Issue 4, Page 649-676eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectaerosol property
dc.subjectairborne survey
dc.subjectatmospheric transport
dc.subjectbiomass burning
dc.subjectdust
dc.subjectextinction coefficient
dc.subjectground-based measurement
dc.subjectlidar
dc.subjectsmoke
dc.subject.ddc550
dc.titleProfiling of Saharan dust and biomass-burning smoke with multiwavelength polarization Raman lidar at Cape Verde
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleTellus B: Chemical and Physical Meteorologyeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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