We investigate the discrepancies in measurements of light extinction and extinction-to-backsatter ratio (lidar ratio) of desert dust with CALIPSO and ground-based lidar systems. Multiwavelength polarization Raman lidar measurements in the Saharan dust plume performed at Praia, Cape Verde, 15.0 degrees N, 23.5 degrees W, during SAMUM-2 in June 2008 were analyzed and compared to results of nearby CALIPSO overflights. The particle extinction coefficients and thus the optical depth are underestimated in the CALIPSO products by about 30% compared to Raman lidar measurements. A pre-defined lidar ratio of 40 sr at 532 nm is used for mineral dust in the CALIPSO algorithms in agreement with values of 41 +/- 6 sr found from constrained retrievals. Ho...
Extensive lidar measurements of Saharan dust and biomass-burning smoke were performed with one airbo...
Multiwavelength aerosol Raman lidar in combination with polarization lidar at Praia (14.9 degrees N,...
A numerical model is used to investigate the dependence at 351 nm of desert-aerosol extinction and ...
Ground-based Raman lidar measurements during the second Saharan Mineral Dust Experiment (SAMUM-2) in...
The microphysical properties of mineral dust aerosols are quite complex: aside from the variability ...
Four years (2010–2013) of observations with polarization lidar and sun/sky photometer at the combine...
We demonstrate improvements in CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observ...
The Saharan Mineral Dust Experiment (SAMUM) 2006, Morocco, aimed at the characterization of optical,...
Nearly pure Saharan dust was observed with an Aerosol Robotic Network (AERONET) Sun photometer, seve...
Nearly pure Saharan dust was observed with an Aerosol Robotic Network (AERONET) Sun photometer, seve...
Nearly pure Saharan dust was observed with an Aerosol Robotic Network (AERONET) Sun photometer, seve...
Functional relationships linking at λ0=351 nm aerosol extinction αλ0aer and backscatter coefficient ...
[1] We determine the extinction‐to‐backscatter (Sa) ratios of dust using (1) airborne in situ measur...
We compared CALIPSO column aerosol optical depths at 0.532 μm to measurements at 147 AERONET sites, ...
In couple of years we expect the launch of the CALIPSO lidar spaceborne mission designed to observe ...
Extensive lidar measurements of Saharan dust and biomass-burning smoke were performed with one airbo...
Multiwavelength aerosol Raman lidar in combination with polarization lidar at Praia (14.9 degrees N,...
A numerical model is used to investigate the dependence at 351 nm of desert-aerosol extinction and ...
Ground-based Raman lidar measurements during the second Saharan Mineral Dust Experiment (SAMUM-2) in...
The microphysical properties of mineral dust aerosols are quite complex: aside from the variability ...
Four years (2010–2013) of observations with polarization lidar and sun/sky photometer at the combine...
We demonstrate improvements in CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observ...
The Saharan Mineral Dust Experiment (SAMUM) 2006, Morocco, aimed at the characterization of optical,...
Nearly pure Saharan dust was observed with an Aerosol Robotic Network (AERONET) Sun photometer, seve...
Nearly pure Saharan dust was observed with an Aerosol Robotic Network (AERONET) Sun photometer, seve...
Nearly pure Saharan dust was observed with an Aerosol Robotic Network (AERONET) Sun photometer, seve...
Functional relationships linking at λ0=351 nm aerosol extinction αλ0aer and backscatter coefficient ...
[1] We determine the extinction‐to‐backscatter (Sa) ratios of dust using (1) airborne in situ measur...
We compared CALIPSO column aerosol optical depths at 0.532 μm to measurements at 147 AERONET sites, ...
In couple of years we expect the launch of the CALIPSO lidar spaceborne mission designed to observe ...
Extensive lidar measurements of Saharan dust and biomass-burning smoke were performed with one airbo...
Multiwavelength aerosol Raman lidar in combination with polarization lidar at Praia (14.9 degrees N,...
A numerical model is used to investigate the dependence at 351 nm of desert-aerosol extinction and ...