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Mongolian cyclones are the main baric formations that are associated with the transfer of heat and moisture to the territory of the Baikal region. Traditionally, the formation of Mongolian cyclones is associated with the development of high-altitude troughs and the outflow of Arctic air to the northern and central regions of Mongolia. Large-scale circulation factors of mobile cyclogenesis change in modern climatic conditions. Therefore, the study of synoptic processes and meteorological factors during the formation of Mongolian cyclones in different time periods was carried out. Particular attention was paid to the study of the conditions for the formation of large floods during the emergence of southern cyclones in the Baikal region. Correlation analysis with variations in the climatic indices of the Northern and Southern Hemispheres was carried out to study the possible influence of oceanic processes in the development of mobile cyclogenesis on the territory of Mongolia.
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I. V. Latysheva, S. Zh. Vologzhina, K. A. Loshchenko, "Mongolian cyclones in a changing climate," Proc. SPIE 11916, 27th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, 1191668 (15 December 2021); https://doi.org/10.1117/12.2603380