Advantages introduced by Raman lidar systems for cloud base determination d
uring precipitating periods are explored using two case studies of light ra
in and virga conditions. A combination of the Raman lidar derived profiles
of water vapor mixing ratio and aerosol scattering ratio, together with the
Raman scattered signals from liquid drops, can minimize or even eliminate
some of the problems associated with cloud boundary detection using elastic
backscatter lidars.