The NASA Goddard Space Flight Center stratospheric ozone lidar system
has the capability of collecting both Rayleigh-Mie and Raman backscatt
er data simultaneously at a number of wavelengths. Here we report on a
n improved method by which temperature can be derived from a combinati
on of the Rayleigh-Mie return at 351-nm lidar channels and the Raman n
itrogen return at 382-nm lidar channels. We also examine some common t
echniques by which temperatures are retrieved from lidar data. Finally
, we show results obtained in 1995 during two Network for the Detectio
n of Stratospheric Change intercomparison campaigns at Lauder, New Zea
land and Mauna Loa, Hawaii.