Klett's new backward inversion algorithm is used to derive optical extinction coefficient profiles from lidar returns from cloudy and foggy atmospheres. Possible influences of multiple scattering and spatially varying backscatter/extinction ratios are discussed, and a series of examples, especially showing the structure of cloud boundaries, are presented. (IFU
International audienceWe propose a method for calculating the ratio R of the indices of the total an...
AbstractThe background aerosol conditions and the conditions contaminated with aerosol of antropogen...
In the lowermost part of the atmosphere, the boundary layer, the amount of aerosols is high. Aerosol...
Accurate lidar-based measurements of cloud optical extinction, even though perhaps limited to the cl...
Here we depart from the inhomogeneous solution of a lidar equation using the backward inversion algo...
The proponents successfully developed a C-language program that is able to calculate the extinction ...
The lidar equation is a special form of the radiative transport equation in single scattering approx...
165-179The relationship between backscattering and extinction coefficients in a turbid atmosphere is...
The presence of multiple scattering contributions to a space borne lidar returns from molecular atmo...
Potter [Appl. Opt. 26, 1250 (1987)] has presented a method to determine profiles of the atmospheric ...
The traditional approach to inverting aerosol extinction makes use of the assumption of a constant L...
A method is developed based on Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (C...
A first inversion of the backscatter profile and extinction-to-backscatter ratio from pulsed elastic...
Up to now, the extraction of extinction and backscatter coefficients from a lidar signa] or lidar in...
Backscattered power data from the Doppler LIght Detection And Ranging (LIDAR) systems at the Hong Ko...
International audienceWe propose a method for calculating the ratio R of the indices of the total an...
AbstractThe background aerosol conditions and the conditions contaminated with aerosol of antropogen...
In the lowermost part of the atmosphere, the boundary layer, the amount of aerosols is high. Aerosol...
Accurate lidar-based measurements of cloud optical extinction, even though perhaps limited to the cl...
Here we depart from the inhomogeneous solution of a lidar equation using the backward inversion algo...
The proponents successfully developed a C-language program that is able to calculate the extinction ...
The lidar equation is a special form of the radiative transport equation in single scattering approx...
165-179The relationship between backscattering and extinction coefficients in a turbid atmosphere is...
The presence of multiple scattering contributions to a space borne lidar returns from molecular atmo...
Potter [Appl. Opt. 26, 1250 (1987)] has presented a method to determine profiles of the atmospheric ...
The traditional approach to inverting aerosol extinction makes use of the assumption of a constant L...
A method is developed based on Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (C...
A first inversion of the backscatter profile and extinction-to-backscatter ratio from pulsed elastic...
Up to now, the extraction of extinction and backscatter coefficients from a lidar signa] or lidar in...
Backscattered power data from the Doppler LIght Detection And Ranging (LIDAR) systems at the Hong Ko...
International audienceWe propose a method for calculating the ratio R of the indices of the total an...
AbstractThe background aerosol conditions and the conditions contaminated with aerosol of antropogen...
In the lowermost part of the atmosphere, the boundary layer, the amount of aerosols is high. Aerosol...
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