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Dual-wavelength Raman and depolarization lidar observations were performedduring the Saharan Aerosol Long-range Transport and Aerosol-Cloud interactionExperiment in Barbados in June and July 2013 to characterize the opticalproperties and vertical distribution of long-range transported Saharan dustafter transport across the Atlantic Ocean. Four major dust events werestudied during the measurements from 15 June to 13 July 2013 with aerosoloptical depths at 532 nm of up to 0.6. The vertical aerosol distribution wascharacterized by a three-layer structure consisting of the boundary layer,the entrainment or mixing layer and the pure Saharan dust layer. The upperboundary of the pure dust layer reached up to 4.5 km in height. Thecontribution of the pure dust layer was about half of the total aerosoloptical depth at 532 nm. The total dust contribution was about 50–70 %of the total aerosol optical depth at 532 nm. The lidar ratio within thepure dust layer was found to be wavelength independent with mean values of53 ± 5 sr at 355 nm and 56 ± 7 sr at 532 nm. For the particlelinear depolarization ratio, wavelength-independent mean values of0.26 ± 0.03 at 355 nm and 0.27 ± 0.01 at 532 nm havebeen found

Optical properties of long-range transported Saharan dust over Barbados as measured by dual-wavelength depolarization Raman lidar measurements