Improvements made to the NASA Goddard Space Flight Center Stratospheri
c Ozone Lidar system have extended its atmospheric-aerosol-measuring c
apabilities. The methods by which aerosol-scattering ratio, aerosol ba
ckscatter, and aerosol extinction are simultaneously derived from lida
r data are reported, and results obtained during several intercomparis
on campaigns at worldwide locations are shown. The results track the e
volution of the Mt. Pinatubo aerosol cloud from 1991 to 1994 and repor
t wavelength-dependence information for aerosol backscatter between 30
8 and 351 nm. Two analysis techniques, a more common inversion method
and a combined elastic-Raman-backscatter approach, are also compared.
(C) 1995 Optical Society of America