Abstract

The problem of the backscattered laser radiation field formation is solved based on the theory of optical radiation transfer in broken cloudiness as a scattering medium with random geometry. The dependence of the energy characteristics of a lidar return averaged over the ensemble of cloud-field realizations on the type of clouds (cumulus and stratus), cloud fraction, optogeometrical parameters of a cloud field, lidar's geometric parameters, and the distance to a cloudy layer. It has been shown that over long periods the multiple light scattering between the cumulus clouds is the dominating contribution to the lidar signal power.

© 1987 Optical Society of America

Lidar depolarization from multiple scattering in marine stratus clouds

Kenneth Sassen and Richard L. Petrilla
Appl. Opt. 25(9) 1450-1459 (1986)

Retrieval of water cloud properties from carbon dioxide lidar soundings

C. M. R. Platt and T. Takashima
Appl. Opt. 26(7) 1257-1263 (1987)

Retrieval of cloud optical parameters from space-based backscatter lidar data

Yuri S. Balin, Svetlana V. Samoilova, Margarita M. Krekova, and David M. Winker
Appl. Opt. 38(30) 6365-6373 (1999)

Simulated polarization diversity lidar returns from water and precipitating mixed phase clouds

Kenneth Sassen, Hongjie Zhao, and Gregory C. Dodd
Appl. Opt. 31(15) 2914-2923 (1992)

Polarization structure of lidar signals reflected from ice crystal clouds

Georgii M. Krekov, Margarita M. Krekova, Dmitrii N. Romashov, and Vitalii S. Shamanaev
Appl. Opt. 44(19) 4148-4156 (2005)