The results of an experimental study of ultrafine aerosol characteristics in the Baikal region and the Gobi Desert are described. The comparative analysis of the dispersion composition of atmospheric aerosol in different climate conditions is carried out. It is ascertained that the total content of ultrafine aerosol in the atmosphere of the Gobi Desert is significantly lower than in the Baikal atmosphere and soil aerosols prevail. In the Lake Baikal region, nanometer-size aerosols are also present, mainly of anthropogenic and organic origin; two peaks are observable in the diurnal variations in the total number concentration of aerosols in the afternoon and evening. In the morning and afternoon, the number of nucleation-mode particles increases due to intensification of breeze circulation, which promotes transport of anthropogenic impurities from the lake and activation of photochemical reactions.
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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].
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).
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).
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).
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).
M. Yu. Arshinov and B. D. Belan, “Study of the aerosol size distribution during spring haze and biomass burning events,” Opt. Atmos. Okeana 24 (6), 468–477 (2011).
A. S. Zayakhanov, G. S. Zhamsueva, V. V. Tsydypov, and T. S. Bal’zhanov, “Study of submicron aerosol fractions in the atmosphere of the Goby Dessert,” Vestn. VSGUTU, No. 1, 10–12 (2015).
P. K. Koutsenogii, “Project "Aerosols of Siberia”, the first results,” Atmos. Ocean. Opt. 7 (8), 542–546 (1994).
P. K. Kutsenogii, N. S. Bufetov, E. I. Kirov, and S. I. Shuiskii, “Dynamics of diurnal and seasonal cycles of aerosol formation in the atmosphere as it follows from measurements in Novosibirsk region,” Atmos. Ocean. Opt. 8 (9), 725–731 (1995).
A. S. Kozlov, A. N. Ankilov, A. M. Baklanov, E.D. Veselovskii, A. L. Vlasenko, S. I. Eremenko, S. B. Malyshkin, S. E. Pashchenko, and A. V. Shitov, “Study of the aerosol properties in air over Teletskoe lake,” Atmos. Ocean. Opt. 11 (6), 553–557 (1998).
G. S. Zhamsueva, A. S. Zayakhanov, A. V. Starikov, V. V. Tsydypov, A. A. Ayurzhanaev, T. V. Khodzher, L. P. Golobokova, and U. G. Filippova, “Chemical composition of aerosols in the atmosphere of Mongolia,” Rus. Meteorol. Hydrol. 37 (8), 546–552 (2012).
A. S. Safatov, G. A. Buryak, S. E. Ol’kin, I. K. Reznikova, Yu. V. Marchenko, B. M. Desyatkov, N. A. Lapteva, I. S. Andreeva, A. S. Kozlov, S. B.,Malyshkin I. A. Sutorikhin, V. I. Bukatyi, S. A. Litvinenko, B. S. Smolyakov, and M. P. Shinkorenko, “Results of the complex ecological study of water and near-shore air of bitter-salty lakes of Altai region in summer of 2011,” Opt. Atmos. Okeana 25 (6), 550–558 (2012).
M. Yu. Arshinov and B. D. Belan, “Vertical distribution of nanoparticles in the continental troposphere,” Atmos. Ocean. Opt. 7 (7), 489–499 (2004).
A. Ankilov, A. Baklanov, M. Colhoun, K.-H. Enderle, J. Gras, Yu. Julanov, D. Kaller, A. Lindner, A. A. Lushnikov, R. Mavliev, F. McGovern, A. Mirme, T. C. O’Connor, J. Podzimek, O. Preining, G. P. Reischl, R. Rudolf, G. J. Sem, W. W. Szymanski, E. Tamm, A. E. Vrtala, P. E. Wagner, W. Winklmayr, and V. Zagaynov, “Intercomparison of number concentration measurements by various aerosol particle counters,” Atmos. Res. 62, 177–207 (2002).
A. A. Azbukin, A. Ya. Bogushevich, V. S. Il’icheskii, V. A. Korol’kov, A. A. Tikhomirov, and V. D. Sheveleva, “Automated Ultrasonic Meteorological Complex AMK-03,” Meteorol. Gidrol., No. 11, 89–97 (2006).
A. S. Zayakhanov, G. S. Zhamsueva, and V. V. Tsydypov, “Hardware-software system for monitoring the content of atmospheric impurities,” Meas. Tech. 58 (3), 355–361 (2015).
M. Yu. Arshinov, B. D. Belan, and T. K. Sklyadneva, “Study of aerosol nano-particles and their interaction with ozone,” in Proc. of EUROTRAC Symposium 98, (WIT Press, Southampton, 1999), vol. 1, p. 495–500.
F. N. Alyea, D. M. Cunnold, and R. G. Prinn, “Meteorological constraints on tropospheric halocarbon and nitrous oxide destructions by siliceous land surfaces,” Atmos. Environ. 12 (5), 1009–1011 (1978).
G. Toupance, “Mesure et comportement du PAN dans l’atmosphere,” Pollut. Atmos. 33, Spec. Iss., 142–150 (1991).
S. Kamm, O. Mohler, and K.-H. Naumann, “Heterogeneous interaction of ozone, NO2 and N2O5 with soot aerosol,” in Proc. of EUROTRAC Symposium 98 (WIT press, Southampton, 1999), vol. 1, 649–655.
Original Russian Text © A.S. Zayakhanov, G.S. Zhamsueva, I.P. Sungrapova, V.V. Tsydypov, 2018, published in Optika Atmosfery i Okeana.
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Zayakhanov, A.S., Zhamsueva, G.S., Sungrapova, I.P. et al. Features of Diurnal Variability of Ultrafine Aerosol in the Air of the Baikal Coastal Zone and Arid Zone of Mongolia. Atmos Ocean Opt 31, 257–262 (2018). https://doi.org/10.1134/S1024856018030168
- ultrafine aerosol
- nucleation mode
- Aitken mode