Features of Diurnal Variability of Ultrafine Aerosol in the Air of the Baikal Coastal Zone and Arid Zone of Mongolia

Author:

Zayakhanov A. S.,Zhamsueva G. S.,Sungrapova I. P.,Tsydypov V. V.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Earth-Surface Processes,Atomic and Molecular Physics, and Optics,Oceanography

Reference20 articles.

1. M. V. Kabanov and M. V. Panchenko, Scattering of Optical Waves in Dispersion Media. Part 3. Atmospheric Aerosol (Publishing House of the Tomsk Division of Siberian Branch of the Academy of Sciences of USSR, Tomsk, 1984) [in Russian].

2. K. Ya. Kondrat’ev, “From nano- to global scales: properties, processes of formation, and aftereffects of atmospheric aerosol impacts. 5. Aerosol and chemical processes in the atmosphere,” Atmos. Ocean. Opt. 18 (3), 177–188 (2005).

3. K. Ya. Kondrat’ev, “Aerosol and climate studies: current state and prospects 1. Aerosol formation, its properties, and their transformations,” Atmos. Ocean. Opt. 19 (1), 1–16 (2006).

4. M. Yu. Arshinov and B. D. Belan, “Diurnal behavior of the concentration of fine and ultrafine aerosol,” Atmos. Ocean. Opt. 13 (11), 909–916 (2000).

5. M. Yu. Arshinov, B. D. Belan, V. K. Kovalevskii, and G. I Tolmachev., “Results of climatic–ecological monitoring at TOR station. III. Atmospheric aerosol,” Atmos. Ocean. Opt. 8 (8), 620–623 (1995).

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