Abstract

It is now customary to consider atmospheric aerosol as a passive conservative admixture in the atmosphere, that is, it does not disappear and fully floats by the wind vortexes. A serious argument in favor of that statement is the fact that the spectrum of fluctuations of backscattering is similar to that of wind speed, that is, in spectrum, as a rule, the extent region is present, corresponding to inertia interval of the Kolmogorov-Obukhov spectrum. The first was E. Eloranta, which by laser sounding of the atmospheric aerosol had derived the fluctuation spectra of lidar signal similar to that of wind speed.

© 1994 IEEE