Siberian High as an important factor for development of cyclonic activity in the Far Eastern region in winter, spring and summer seasons
https://doi.org/10.26428/1606-9919-2021-201-879-894
Abstract
Influence of the Siberian High longitudinal position on cyclonic activity over the Far Eastern Seas and the Pacific Ocean in winter, spring and summer is considered. Eastward shift of this atmospheric center causes general decreasing of number of cyclones over the region, but their intensity increases; on the contrary: cyclones are more frequent but weaker when the Siberian High is located in western position. The Siberian High, being a winter center, cannot influence directly on spring and summer cyclones, but it influences on formation of the Far Eastern Low, which intensity correlates with number and intensity of spring and summer cyclones.
About the Author
S. Yu. Glebova
Pacific branch of VNIRO (TINRO)
Russian Federation
Russian Federation
Glebova Svetlana Yu., Ph.D., leading researcher
4, Shevchenko Alley, Vladivostok, 690091
References
1. Babkin, V.I., Vorobyev, V.N., and Smirnov, N.P., The Siberian High and its influence on the discharge of the Ob, Yenisei, and Lena, Meteorol. Gidrol., 2005, no. 4, pp. 102–108.
2. Glebova, S.Yu., Winter cyclogenesis over the ocean as a factor of subsequent changes in the atmospheric and thermal regime of the Far-Eastern Seas and North-West Pacific (with one year lag), Izv. Tikhookean. Nauchno-Issled. Inst. Rybn. Khoz. Okeanogr., 2012, vol. 170, pp. 136–150.
3. Dashko, N.A., Varlamov, S.M., Khan, E.H., and Kim, E.S., Centers of action of the atmosphere of the Asia-Pacific region and summer weather features on the coast of the Sea of Japan and the Sea of Okhotsk, Meteorol. Gidrol., 1997, no. 9, pp. 14–23.
4. Dmitriev, A.A. and Ivanov, N.A., On the extreme development of some atmospheric action centers and the influence of geophysical and tidal forces on them, Tr. Arkt. Antarkt. Nauchno-Issled. Inst., 1976, vol. 330, pp. 130–149.
5. Il’inskii, O.K., The summer Far Eastern low-pressure area, Tr. Dal’nevost. Nauchno-Issled. Gidrometeorol. Inst., 1960, vol. 11, pp. 3–53.
6. Ilyinsky, O.K., The experience of identifying the main forms of atmospheric circulation over the Far East, Tr. Dal’nevost. Nauchno-Issled. Gidrometeorol. Inst., 1965, vol. 20, pp. 26–45.
7. Ilyinsky, O.K., The main features of the summer circulation of the troposphere over the temperate latitudes of East Asia, in Tr. 1-y nauch. konf. po obshchey tsirkulyatsii atmosfery (Tr. 1st Scientific conference on the general circulation of the atmosphere), Moscow: Gidrometeoizdat, 1962, pp. 175–182.
8. Kalachikova, V.S., Synoptic conditions for the formation and destruction of the Asian anticyclone, Tr. Dal’nevost. Nauchno-Issled. Gidrometeorol. Inst., 1965, vol. 26, pp. 83–102.
9. Kunitsyn, A.V., On the quantitative characteristics of cyclonic activity, Meteorol. Gidrol., 1956, no. 6, pp. 29–30.
10. Morozova, S.V., Characteristics of winter Asian anticyclone under current climate changes, News of the Altai branch of the Russian Geographical Society, 2014, vol. 1(35), pp. 55–57.
11. Pogosyan, Kh.P., Seasonal fluctuations of the general atmospheric circulation, Tr. Tsentr. Inst. Prognozov, Leningrad: Gidrometeoizdat, 1947, vol. 1, no. 28.
12. Podnebesnykh, N.V., Dynamics of cyclonic and anticyclonic activity over Siberia, Extended Abstract of Cand. Sci. (Geogr.) Dissertation, Tomsk: Institute of Monitoring of Climatic and Ecological Systems of the Siberian Branch of the Russian Academy of Sciences, 2010.
13. Polyanskaya, E.A., Sinopticheskiye protsessy Vostochnoy Sibiri i Dal’nego Vostoka (Synoptic processes in Eastern Siberia and the Far East), Saratov: SGU, 2011.
14. Prostyakov, S.M., Tipy sinopticheskikh protsessov Vostochnoy Azii (Types of synoptic processes in East Asia), Moscow: Gidrometeoizdat, 1947.
15. Savina, S.S. and Khmelevskaya, L.V., Changes in the circulation of the atmosphere and climate in the XX century, Priroda, 1969, no. 2, pp. 38–46.
16. Stekhnovskiy, D.I., Baricheskoye pole zemnogo shara (Baric field of the globe), Moscow: Gidrometeoizdat, 1962.
17. Tunegolovets, V.P., Cyclonic activity over the northwestern part of the Pacific Ocean and the Far Eastern seas and an assessment of its impact on the active layer, in Dal’nevostochnye morya Rossii. Kn. 1: Okeanologicheskiye issledovaniya (Far Eastern Seas of Russia, Book 1: Oceanological research), Moscow: Nauka, 2007, pp. 60–96.
18. Hen, G.V. and Voronina, V.F., Interannual fluctuations of the southern boundary of cold shelf waters in the eastern part of the Bering Sea due to large-scale synoptic variability, Tr. Dal’nevost. Nauchno-Issled. Gidrometeorol. Inst., 1986, vol. 125, pp. 10–20.
19. Statisticheskiye metody dolgosrochnogo prognoza pogody (Statistical methods for long-term weather forecasting. Study guide for masters of the direction «Hydrometeorology»), Kazan: Kazan. gos. un-t, 2018.
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For citations:
Glebova S.Yu. Siberian High as an important factor for development of cyclonic activity in the Far Eastern region in winter, spring and summer seasons. Izvestiya TINRO. 2021;201(4):879-894. (In Russ.) https://doi.org/10.26428/1606-9919-2021-201-879-894
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