Vol. 2, issue 11, article # 2

pdf Muldashev T. Z., Pavlov V. E., Teifel' Ya. A. On the determination of the atmospheric optical depth due to aerosol scattering from sky brightness measurements in the visible region of the spectrum. // Atmospheric and oceanic optics. 1989. V. 2. No. 11. P. 959-963.
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Results of the numerical solution of the radiative transfer equation for the atmosphere with a trimodal particle size distribution are analyzed. Approximate formulas are derived by which the aerosol optical depth can be determined from observations of the absolute phase functions of the sky brightness.


1. G.Sh. Livshits and V.E. Pavlov, Atmospheric Optics (Nauka, Moscow, 1968).
2. E.B. Pyaskovskaya-Fesenkova, Investigation of Light Scattering in the Earth’s Atmosphere (Izd. Akad. Nauk SSSR, Moscow, 1957).
3. G.Sh. Livshits, Light Scattering in the Atmosphere (Nauka, Alma-Ata, 1957).
4. M.A. Nazaraliev, V.Т. Pavlov, Izv, Akad. Nauk SSSR, Ser. FAO, 15, No. 6, 619 (1979).
5. G.V. Rosenberg, G.I. Gorchakov, Yu.S. Georgievskii, Yu.S. Lyubovtseva, Physics of the Atmosphere and Problems of Climate (Nauka, Moscow, 1980).
6. V.S. Antufeev, A.I. Ivanov, G.Sh. Livshits, G.A. Mikhailov, Izv. Akad. Nauk SSSR, Ser. FAO, 16, No. 2, 146 (1980).
7. E.G. Yanovitskii and Z.O. Dumanskii, Tables of Light Scattering by a Polydisperse System of Spherical Particles (Naukova Dumka, Kiev, 1972).
8. T.Z. Muldashev and I.M. Sultangazin, Zh. Vychisl. Mat.i Mat. Fiz. 26, No. 6, 882 (1986).