Abstract
Based on an experimental study of directed dissipation coefficients and aerosol microstructure in the coastal area the problem of wind regime manifestation is considered. It is shown that the main changes of parameters of dissipation indicatrix form near angles ϕ=15°–165°, which are conditioned by submicron fractions of aerosol particles, take place without regard for wind regime. Usually they are defined by effect of relative air humidity. It is found that specific manifestations of wind regime are observed close to small dissipation angles and are conditioned by the effect of coarse-dispersed aerosol fractions.
Similar content being viewed by others
References
Blyutgen, I.Geography of Climates, Vol. 1. Progress, Moscow, 1972, pp. 311–367.
Meison, B. J.Physics of Clouds. Gidrometeoizdat, Leningrad, 1961.
Rasula, N. (Ed.)Chemistry of the Lower Atmosphere. Mir, Moscow, 1976.
Batcher, S. and Charlson, R.Introduction to the Chemistry of the Atmoshere. Mir, Moscow, 1977.
Rozenberg, G. V. Property of atmospheric aerosole on optical analysis data.Izv. Acad. Sci. USSR Fiz. Atmos. Okeana (1967)3, 936–949.
Georgievsky, Yu. S. and Rozenberg, G. V. Humidity as a factor of changes in aerosols.Izv. Acad. Sci. USSR Fiz. Atmos. Okeana (1973)9, 126–138.
Lyubovtseva, Yu. C. On photochemical and condensational changes in submicron fraction of aerosols.Izv. Acad. Sci. USSR Fiz. Atmos. Okeana (1978)14, 229–234.
Bouma, T. J. A statistical study of the relationship between visibility and relative humidity of Leeuwarden.Bull. Am. Meteorol. Soc. (1960)41, 357–365.
Rozenberg, G. V., Gorchakov, G. I., Georgievsky, Yu. S. et al. Optical parameters of atmospheric aerosols In:Fizika Atmospherie i Problemi Klimata (Physics of Atmosphere and Problems of Climate). Nauka, Moscow, 1980, pp. 216–257.
Weakening of Light in the Earth's Atmosphere. (Visual and Ultraviolet Zones of Spectrum). Hauka, Alma-Ata, Kaz. SSR, 1976.
Gorchakov, G. I., Gorchakov, I.A., Lykocov, E. A. et al. On determination of the coefficient of refraction of polarisation of dispersed light.Izv. Acad. Sci. USSR Fiz. Atmos. Okeana (1976)12, 612–620.
Kerkov, G. M. and Rahimov, R. F. Cumulative contribution of fraction of aerosol particles in the formation of diffused emission field.All Union Symposium on Spreading Laser and Rays in Atmosphere, Tomsk, 1979, pp. 99–104.
Mitropol'sky, A. K.Techniques of Statistical Calculations, 2nd end., Nauka, Moscow, 1971, pp. 363–364.
Chernyakova, A. P.Hydrophysical and Hydrochemical Studies in the Black Sea. Nauka, Moscow, 1967, pp. 10–15.
Zyev, V. E., Kabanov M. V., Panchenko, M. V., et al. Some results of the study of optical properties of seashore smoke.Izv. Acad. Sci. USSR Fiz. Atmos. Okeana (1978)14, 1268–1275.
Patterson, E. M. Measurements of aerosol optical properties and size distributions in remote continental and marine regions.JRC 1980, Int. Radiat. Symp., Fort Collins. CO., 1980, Vol. V, Extended Abstract, pp. 147–149.
Kozlov, V. C., Pol'kin, V. V. and Fadeev V. Ya. Some results of the study of microstructures of aerosol in shore region.II Conference on Atmospheric Optics, Tomsk, 1980, pp. 182–185.
Additional information
UDK 551.593
Rights and permissions
About this article
Cite this article
Panchenko, M.V., Pol'kin, V.V. & Fadeev, V.Y. On the effect of the coastal zone wind regime on the optical characteristics of haze. Soviet Journal of Physical Oceanography 1, 63–71 (1987). https://doi.org/10.1007/BF02198289
Issue Date:
DOI: https://doi.org/10.1007/BF02198289