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dc.contributor.authorMueller, D.
dc.contributor.authorWeinzierl, B.
dc.contributor.authorPetzold, A.
dc.contributor.authorKandler, K.
dc.contributor.authorAnsmann, A.
dc.contributor.authorMueller, T.
dc.contributor.authorTesche, Matthias
dc.contributor.authorFreudenthaler, V.
dc.contributor.authorEsselborn, M.
dc.contributor.authorHeese, B.
dc.contributor.authorAlthausen, D.
dc.contributor.authorSchladitz, A.
dc.contributor.authorOtto, S.
dc.contributor.authorKnippertz, P.
dc.identifier.citationMueller , D , Weinzierl , B , Petzold , A , Kandler , K , Ansmann , A , Mueller , T , Tesche , M , Freudenthaler , V , Esselborn , M , Heese , B , Althausen , D , Schladitz , A , Otto , S & Knippertz , P 2010 , ' Mineral dust observed with AERONET Sun photometer, Raman lidar, and in situ instruments during SAMUM 2006 : Shape-independent particle properties ' , Journal of Geophysical Research: Atmospheres , vol. 115 , no. D7 , D07202 .
dc.identifier.otherPURE: 1979138
dc.identifier.otherPURE UUID: a409ed46-8da3-45d1-8359-86a3f57f5c65
dc.identifier.otherWOS: 000276545500001
dc.identifier.otherScopus: 77951076735
dc.identifier.otherORCID: /0000-0002-0203-7654/work/68611592
dc.description.abstractAerosol Robotic Network (AERONET) Sun photometer observations were carried out at Ouarzazate, Morocco, during the Saharan Mineral Dust Experiment (SAMUM) 2006. Data from one measurement day, 19 May 2006, are used to derive particle optical and microphysical parameters with AERONET's latest version of light-scattering model for non-spherical particle geometry. In our analysis we also make use of a novel measurement channel at 1638 nm wavelength. We compare the results to data products obtained by airborne high-spectral-resolution lidar, several ground-based Raman lidar, and airborne and ground-based in situ measurement platforms. We chose that specific measurement day because the dust plume was vertically well mixed. Extinction coefficients from AERONET Sun photometer and lidar observations and in situ measurements agree well. Angstrom exponents from Sun photometer and lidar are in close agreement, too. Airborne in situ measurements of dust particle size distributions show larger effective radii than inferred from the AERONET data. Complex refractive indices that are derived with the AERONET algorithm differ from the values obtained with different independent techniques employed in our study. The single-scattering albedo was derived from the airborne observations of particle size distributions and complex refractive indices. Single-scattering albedo differs to the value inferred from the AERONET data. The differences may be attributed to the different effective radii that we obtained from the various techniques. The differences between the data products from the various measurement platforms, however, cannot be generalized, as we could only test data for one measurement day. An analysis of additional measurements is under way.en
dc.relation.ispartofJournal of Geophysical Research: Atmospheres
dc.subjectSAHARAN DUST
dc.titleMineral dust observed with AERONET Sun photometer, Raman lidar, and in situ instruments during SAMUM 2006 : Shape-independent particle propertiesen
dc.contributor.institutionSchool of Physics, Astronomy and Mathematics
dc.contributor.institutionScience & Technology Research Institute
dc.contributor.institutionCentre for Atmospheric and Climate Physics Research
dc.description.statusPeer reviewed
rioxxterms.typeJournal Article/Review

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