Geology, geography and global energy

Scientific and Technical Journal

Mapping of geological and geographical characteristic and thunderstorm activity in the Republic of Altai

2018. №2, pp. 167-177

Karanina S.J. - C.Sc. in Fisics and Mathematics, Associate Professor, Gorno-Altaisk State University (GASU), 1 Lenkin st., Gorno-Altaisk, Altai Republic, 649000, Russian Federation, krechetovas@yandex.ru

Kocheeva N.A. - C.Sc. in Geology and Mineralogy, Associate Professor, Gorno-Altaisk State University (GASU), 1 Lenkin st., Gorno-Altaisk, Altai Republic, 649000, Russian Federation, nina_kocheewa@mail.ru

Karanin A.V. - C.Sc. in Geography, Associate Professor, Gorno-Altaisk State University (GASU), 1 Lenkin st., Gorno-Altaisk, Altai Republic, 649000, Russian Federation, vedmedk@bk.ru

The Republic of Altai is situated within the homonymous mountainous country, which is the highest part of the Western Siberia. The study of thunderstorms occurring in mountainous countries, is a challenge. Traditional methods of monitoring used by the meteorological service has shown its effectiveness, but does not give a complete picture about this natural phenomenon. The mapping of data arrays containing information about the storm, showed a high level of correlation, which gives grounds for use in mountainous country data of instrumental observations. The results obtained using the WWLLN data have confirmed and substantiated the earlier results, which were not devoid of produce hypotheses. The relationship of thunderstorm activity with geological structure was studied on the example of the anomalies of the magnetic field. For the first time managed to prove the relationship of the manifestations of atmospherical with the peculiarities of the magnetic field in borders of the Altai Republic.

Key words: атмосферики, горная страна, Алтай, гроза, атмосферное электричество, регистрация атмосфериков, распределение атмосфериков, atmosferici, mountainous country, Altai, thunderstorm, atmospheric electricity, check atmosferico, the distribution of atmospherical

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