Влияние уровня температурной инверсии атмосферы на тепловой эффект пыльной мглы

Studied data on air temperature, obtained at meteorological stations in Dushanbe, Termez, Bayramali, Repеtek and Kurgan-Tube. Found that, depending on the particular geographical situation of the observation point dusty haze leads to different consequences for the temperature of the surface layer of the atmosphere. The contribution of the temperature effect of the dusty haze associated with a geographical area and the terrain location points. These results confirm the assumption that the stabilizing role of diffusion layers in a dusty atmosphere.