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dc.contributor.authorTesche, Matthias
dc.contributor.authorMueller, D.
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.accessioned2013-08-01T08:33:12Z
dc.date.available2013-08-01T08:33:12Z
dc.date.issued2011-09
dc.identifier.citationTesche , M , Mueller , D , Gross , S , Ansmann , A , Althausen , D , Freudenthaler , V , Weinzierl , B , Veira , A & Petzold , A 2011 , ' Optical and microphysical properties of smoke over Cape Verde inferred from multiwavelength lidar measurements ' , Tellus Series B-Chemical and Physical Meteorology , vol. 63 , no. 4 , pp. 677-694 . https://doi.org/10.1111/j.1600-0889.2011.00549.x
dc.identifier.issn0280-6509
dc.identifier.otherORCID: /0000-0002-0203-7654/work/68611721
dc.identifier.urihttp://hdl.handle.net/2299/11249
dc.descriptionPublished under the terms of the Creative Commons Attribution-Noncommercial 3.0 Unported License.
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 Angstrom 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 Angstrom 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 mu m with individual results varying between 0.10 and 0.36 mu m. 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.en
dc.format.extent18
dc.format.extent1653254
dc.language.isoeng
dc.relation.ispartofTellus Series B-Chemical and Physical Meteorology
dc.subjectAEROSOLS
dc.subjectAIRCRAFT
dc.subjectINVERSION
dc.subjectEXTINCTION
dc.subjectCALIBRATION
dc.subjectPARTICLE PARAMETERS
dc.subjectRETRIEVAL
dc.subjectSAFARI 2000
dc.subjectABSORPTION
dc.subjectREGULARIZATION
dc.titleOptical and microphysical properties of smoke over Cape Verde inferred from multiwavelength lidar measurementsen
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.1600-0889.2011.00549.x
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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