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Abstract
The difficulties of determining the particle spectrum of the atmosphere aerosol are considered. The transparency and scattering pattern methods which allow one to determine the particle size distribution function of an arbitrary system are described. The requirements which these methods present to initial optical information are indicated. The examples of the inversion of the transparency and scattering pattern are given.DOI: 10.1111/j.2153-3490.1966.tb00271.x