Peculiarities of Thunderstorms Occurrences on the Border of the Western Siberia Plains and Altai Mountains

Nina Kocheeva (), Muhabat Chankibaeva (), Aleksandr Minaev (), Maria Sukhova () and Anton Modorov ()
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Nina Kocheeva: Department of Geography Gorno Altaisk State University GASU Russian Federation, Postal: RU
Muhabat Chankibaeva: Department of Geography Gorno Altaisk State University GASU Russian Federation, Postal: RU
Aleksandr Minaev: Department of Geography Gorno Altaisk State University GASU 649000 1 Lenkin Str Gorno Altaisk Russian Federation, Postal: RU
Maria Sukhova: Department of Geography Gorno Altaisk State University GASU Laboratory of Landscape Water and Ecological Researches and Environmental Management Institute of Water and Environmental Problems of the Siberian Branch of the Russian Academy of Science 656038 1 Molodezhnaya Str Barnaul Russian Federation, Postal: RU
Anton Modorov: Department of Geography Gorno Altaisk State University GASU 649000 1 Lenkin Str Gorno Altaisk Russian Federation, Postal: RU

Journal of Advanced Research in Management, 2017, vol. 8, issue 5, 1061-1068

Abstract: Mountains of Altai are characterized by the greatest elevation in the Siberian region creating an obstacle for Western air masses transfer This fact determines the diversity of micro climatic conditions Complex climatic and geomorphologic factors create the variety of storms in certain regions of the mountainous country At the same time the climate and the weather in the mountains of Altai is the product of processes of general atmospheric circulation Any economic activity feels the risk during storms The airport on the territory of the Altai Republic which receives a lot of passengers especially in the summer operates again Therefore it is rational to conduct the study of the relationship of thunderstorm activity with cyclonic activity which was the purpose of the study on the Northern slopes of the Altai where the airport and the weather station are situated The results of the study allowed identifying the periods of thunderstorms manifestation on the border of the plains of Western Siberia and the Altai Mountains as well as their confinement to the frontal phenomena

Date: 2017
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