Validation of CALIPSO space-borne-derived attenuated backscatter coefficient profiles using a ground-based lidar in Athens, Greece

The particle backscatter coefficients were multiplied with the most appropriate lidar ratio, which is given by the Raman lidar observations of extinction and backscatter coefficient

Based on 8 years of (January 2008– December 2015) cloud phase information from the GCM-Oriented Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Cloud

We reviewed the capabilities of space- borne instruments (lidar, mid-infrared, microwave) applied to the detection of PSCs and uptake of HNO3 and used the results to investigate

Apparent scattering ratios calculated from the two lidar measurements of to- tal attenuated backscatter at 532 nm show similar aerosol and cloud layer structures both under

Data for direct evaluation of the obtained mean vertical profiles were taken from the dataset of Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) onboard the NASA

To evaluate the e ff ect of the calibration issue on the stratospheric aerosol backscatter, we performed an experiment by taking the ratio of a mid-latitude northern hemisphere

For data gathered with firmware 1.71, the cosmetic shift can be corrected based on a combination of back- ground signal profile estimates and average attenuated backscatter across

(a) Lidar backscatter and truck temperature at Intercept F at 15:00 PDT, which marks the foremost advance of the smoke- filled density current. (b) Lidar backscatter and

Interestingly, an aqueous solution containing NaCl indeed accelerated both the acylhydrazone and oxime formation reactions in a salt con- centration-dependent manner, which corroborates