the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Aerosol microphysical retrievals from precision filter radiometer direct solar radiation measurements and comparison with AERONET
S. Kazadzis
I. Veselovskii
V. Amiridis
J. Gröbner
A. Suvorina
S. Nyeki
E. Gerasopoulos
N. Kouremeti
M. Taylor
A. Tsekeri
C. Wehrli
Related authors
Measurements of transported smoke layers were performed with a lidar in Lille and a five-channel fluorescence lidar in Moscow. Results show the peak of fluorescence in the boundary layer is at 438 nm, while in the smoke layer it shifts to longer wavelengths. The fluorescence depolarization is 45 % to 55 %. The depolarization ratio of the water vapor channel is low (2 ± 0.5 %) in the absence of fluorescence and can be used to evaluate the contribution of fluorescence to water vapor signal.
nearwavelengths (380, 440, 500 and 870 nm) in the period 2005–2015. The goal of this study is to assess whether their long term AOD data are comparable and consistent.
Related subject area
Measurements of transported smoke layers were performed with a lidar in Lille and a five-channel fluorescence lidar in Moscow. Results show the peak of fluorescence in the boundary layer is at 438 nm, while in the smoke layer it shifts to longer wavelengths. The fluorescence depolarization is 45 % to 55 %. The depolarization ratio of the water vapor channel is low (2 ± 0.5 %) in the absence of fluorescence and can be used to evaluate the contribution of fluorescence to water vapor signal.