The authors present a method that can being use to retrieve the stratospheric ozone concentration, the aerosol extinction and the microphysical aerosol characteristics. Method was based on the direct solar radiation extinction measurements from the satellite multichanel spectrometer "Spektr-256". The Angstrom's approximation of the aerosol extinction of the wavelength dependence in O.45-O.83mkm is being realized to separate of the aerosol and ozone optical thickness. The Tichonov's method for reconstruction is being used. The aerosol type and the vertical aerosol refractive index the suppositions give possibility for every altitude step -65m to calculate the aerosol size distributions, the average aerosol radius and width size distributions. The above-mentioned remote sensing method is being applied the authors to the serial experimental dates 1993-1994 years.In remote sensing time the aerosol size distributions have been taking ofthe single-modal shape distributions, generally, are being shown the calculating maps of the size distributions. The presence of the considerable fluctuations the average aerosol radius and width size distributions are being permitted an assumption, that the stratospheric aerosol was band-like structure with thickness ofthe bands about 1km.
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