Atmospheric Velocity Spectral Width Measurements Using the Statistical Distribution of Pulsed CO2 Lidar Return Signal Intensities

Abstract

A pulsed CO2 lidar with coherent detection has been used to measure the correlation time of the backscatter of an ensemble of atmospheric aerosol particles which are illuminated by the pulsed radiation. The correlation time of the backscatter of the return signal, which is directly related to the velocity spectral width, can be used to study the velocity structure constant of atmospheric turbulence and wind shear. Various techniques for correlation time measurement are discussed, and several measurement results are presented for the technique using the information contained in the statistical distribution of a set of lidar return signal intensities.