The inversion of lidar returns from homogeneous atmospheres has been d
one customarily through the well-known slope method. The logarithmic o
peration over the range-corrected and system-normalized received signa
l used in this method introduces a bias in the statistics of the noise
-affected processed signal that can severely distort the estimates of
the atmospheric attenuation and backscatter coefficients under measure
ment. It is shown that a fitting of the theoretically expected exponen
tial signal to the range-corrected received one, using as the initial
guess the results provided by the slope method and a least-squares ite
rative procedure, can yield enhanced accuracy under low signal-to-nois
e ratios and especially in moderate-to-high extinction conditions. (C)
1998 Optical Society of America.