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dc.contributor.authorTesche, Matthias
dc.contributor.authorGross, Silke
dc.contributor.authorAnsmann, Albert
dc.contributor.authorMueller, D.
dc.contributor.authorAlthausen, Dietrich
dc.contributor.authorFreudenthaler, Volker
dc.contributor.authorEsselborn, Michael
dc.date.accessioned2013-08-01T08:48:08Z
dc.date.available2013-08-01T08:48:08Z
dc.date.issued2011-09
dc.identifier.citationTesche , M , Gross , S , Ansmann , A , Mueller , D , Althausen , D , Freudenthaler , V & Esselborn , M 2011 , ' Profiling of Saharan dust and biomass-burning smoke with multiwavelength polarization Raman lidar at Cape Verde ' , Tellus Series B-Chemical and Physical Meteorology , vol. 63 , no. 4 , pp. 649-676 . https://doi.org/10.1111/j.1600-0889.2011.00548.x
dc.identifier.issn0280-6509
dc.identifier.otherORCID: /0000-0002-0203-7654/work/68611609
dc.identifier.urihttp://hdl.handle.net/2299/11251
dc.descriptionPublished under the terms of the Creative Commons Attribution-Noncommercial 3.0 Unported License
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 during May 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. Angstrom 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.en
dc.format.extent28
dc.format.extent3440345
dc.language.isoeng
dc.relation.ispartofTellus Series B-Chemical and Physical Meteorology
dc.subjectAEROSOL CHARACTERIZATION
dc.subjectDEPOSITION
dc.subjectTRANSPORT
dc.subjectOPTICAL-PROPERTIES
dc.subjectNORTH-AFRICAN DUST
dc.subjectDESERT DUST
dc.subjectTROPOSPHERIC AEROSOLS
dc.subjectGREECE
dc.subjectATLANTIC-OCEAN
dc.subjectTHESSALONIKI
dc.titleProfiling of Saharan dust and biomass-burning smoke with multiwavelength polarization Raman lidar at Cape Verdeen
dc.contributor.institutionSchool of Physics, Astronomy and Mathematics
dc.contributor.institutionCentre for Atmospheric and Climate Physics Research
dc.contributor.institutionSchool of Physics, Engineering & Computer Science
dc.contributor.institutionDepartment of Physics, Astronomy and Mathematics
dc.description.statusPeer reviewed
rioxxterms.versionofrecord10.1111/j.1600-0889.2011.00548.x
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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