Lidar returns from cloud decks and from the Earth's surface are useful for calibrating single scatter lidar signals from space. To this end analytical methods (forward and backward) are presented for inverting lidar waveforms in terms of the path integrated lidar retum and the transmission losses over that range interval, using an exponential relation between extinction and backscatter. The atmospheric backscatter coefficient has been expressed in the equivalent diffuse reflection coefficient of the surface. Also is shown that the path integrated lidar return from clouds can be used to verify the lidar calibration
Atmospheric lidar observations provide a unique capability to directly observe the vertical profile ...
Klett's new backward inversion algorithm is used to derive optical extinction coefficient profiles f...
165-179The relationship between backscattering and extinction coefficients in a turbid atmosphere is...
The inversion of lidar returns from homogeneous atmospheres has been done customarily through the we...
In this study a systematic approach is used to find the most suitable algorithm for the inversion of...
Up to now, the extraction of extinction and backscatter coefficients from a lidar signa] or lidar in...
Accurate lidar-based measurements of cloud optical extinction, even though perhaps limited to the cl...
International audienceSpaceborne active lidar systems are under development to give new insight into...
In this paper a technique for autocalibration of a cloud lidar is demonstrated. It is shown that the...
A first inversion of the backscatter profile and extinction-to-backscatter ratio from pulsed elastic...
The lidar equation is a special form of the radiative transport equation in single scattering approx...
International audienceIn the framework of the scientific cooperation between the CEILAP laboratory (...
Lidars are ideally placed to investigate the effects of aerosol and cloud on the climate system due ...
It is used here the lidar equation describing signals from a weakly turbid atmosphere to solve the p...
A method for interpreting elastic-lidar return signals in heavily-polluted atmospheres is presented....
Atmospheric lidar observations provide a unique capability to directly observe the vertical profile ...
Klett's new backward inversion algorithm is used to derive optical extinction coefficient profiles f...
165-179The relationship between backscattering and extinction coefficients in a turbid atmosphere is...
The inversion of lidar returns from homogeneous atmospheres has been done customarily through the we...
In this study a systematic approach is used to find the most suitable algorithm for the inversion of...
Up to now, the extraction of extinction and backscatter coefficients from a lidar signa] or lidar in...
Accurate lidar-based measurements of cloud optical extinction, even though perhaps limited to the cl...
International audienceSpaceborne active lidar systems are under development to give new insight into...
In this paper a technique for autocalibration of a cloud lidar is demonstrated. It is shown that the...
A first inversion of the backscatter profile and extinction-to-backscatter ratio from pulsed elastic...
The lidar equation is a special form of the radiative transport equation in single scattering approx...
International audienceIn the framework of the scientific cooperation between the CEILAP laboratory (...
Lidars are ideally placed to investigate the effects of aerosol and cloud on the climate system due ...
It is used here the lidar equation describing signals from a weakly turbid atmosphere to solve the p...
A method for interpreting elastic-lidar return signals in heavily-polluted atmospheres is presented....
Atmospheric lidar observations provide a unique capability to directly observe the vertical profile ...
Klett's new backward inversion algorithm is used to derive optical extinction coefficient profiles f...
165-179The relationship between backscattering and extinction coefficients in a turbid atmosphere is...