Tellus B · 2008 · 697 citations · 41 references
Natural SciencesEarth SciencesAtmospheric ChemistryAtmospheric ScienceCloud PhysicsAerosol PhysicsAerosol Remote SensingAtmospheric OpticsCloud PropertiesLidar Remote SensingParticulate MatterAerosol Optical PropertiesAerosol Optical ThicknessDepolarizationDepolarization RatioDust Aerosol Remote SensingLidar CalibrationLidar SystemsMineral Dust Aerosols
Vertical profiles of the linear particle depolarization ratio of pure dust clouds were measured during the Saharan Mineral Dust Experiment (SAMUM) at Ouarzazate, Morocco (30.9◦N, –6.9◦E), close to source regions in May–June 2006, with four lidar systems at four wavelengths (355, 532, 710 and 1064 nm). The intercomparison of the lidar systems is accompanied by a discussion of the different calibration methods, including a new, advanced method, and a detailed error analysis. Over the whole SAMUM periode pure dust layers show a mean linear particle depolarization ratio at 532 nm of 0.31, in the range between 0.27 and 0.35, with a mean Ångström exponent (AE, 440–870 nm) of 0.18 (range 0.04–0.34) and still high mean linear particle depolarization ratio between 0.21 and 0.25 during periods with aerosol optical thickness less than 0.1, with a mean AE of 0.76 (range 0.65–1.00), which represents a negative correlation of the linear particle depolarization ratio with the AE. A slight decrease of the linear particle depolarization ratio with wavelength was found between 532 and 1064 nm from 0.31 ± 0.03 to 0.27 ± 0.04.
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Analysis of atmospheric lidar observations: some comments
F. G. Fernald · Applied Optics · 1984 · 2K citations
Lidar inversion with variable backscatter/extinction ratios
James D. Klett · Applied Optics · 1985 · 1.1K citations
Albert Ansmann, Jens Bösenberg, Anatoli Chaikovsky et al. · Journal of Geophysical Research Atmospheres · 2003 · 524 citations · Full text