TY - JOUR
T1 - Depolarization ratio profiling at several wavelengths in pure Saharan dust during SAMUM 2006
AU - Freudenthaler, Volker
AU - Esselborn, Michael
AU - Wiegner, Matthias
AU - Heese, Birgit
AU - Tesche, Matthias
AU - Ansmann, Albert
AU - Mueller, D.
AU - Althausen, Dietrich
AU - Wirth, Martin
AU - Fix, Andreas
AU - Ehret, Gerhard
AU - Knippertz, Peter
AU - Toledano, Carlos
AU - Gasteiger, Josef
AU - Garhammer, Markus
AU - Seefeldner, Andmeinhard
N1 - Published under the terms of the Creative Commons Attribution-Noncommercial 3.0 Unported License
PY - 2009/2
Y1 - 2009/2
N2 - 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 degrees N, -6.9 degrees 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 angstrom ngstrom 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.
AB - 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 degrees N, -6.9 degrees 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 angstrom ngstrom 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.
KW - AEROSOLS
KW - CONTRAILS
KW - LINEAR DEPOLARIZATION
KW - BACKSCATTER
KW - RAMAN LIDAR
KW - EXTINCTION
KW - PARAMETERS
KW - CLOUDS
KW - POLARIZATION LIDAR
KW - RETURNS
U2 - 10.1111/j.1600-0889.2008.00396.x
DO - 10.1111/j.1600-0889.2008.00396.x
M3 - Article
SN - 0280-6509
VL - 61
SP - 165
EP - 179
JO - Tellus Series B-Chemical and Physical Meteorology
JF - Tellus Series B-Chemical and Physical Meteorology
IS - 1
ER -