Abstract
The structure and interannual variability of the 30–50 day oscillation over the Indian region have been studied during the monsoon season. The power spectra of the zonal component of wind show large power in the 30–50 day time scale. The oscillation has a meridional wavelength of about 25° latitude and a slow northward phase speed of about 0.7° latitude per day. The oscillation also has some interannual variability. The periods are somewhat longer during the drought years.
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Alexander G, Keshavamurty R N, De U S, Chellapa R, Das S K and Pillai P V 1978 Fluctuations of monsoon activity;Indian J. Meteorol. Hydrol. Geophys. 29 76–87
Dakshinamurti J and Keshavamurty R N 1978 On oscillation of period around one month in the Indian summer monsoon;Indian J. Meteorol. Hydrol. Geophys. 27 201–208
Keshavamurty R N 1973On the maintenance of the mean Indian southwest monsoon circulation and the structure and energetics of monsoon disturbances; Ph.D. thesis, Mysore University, India
Krishnamurti T N, Jayakumar P K, Sheng J, Surgi N and Kumar A 1985 Divergent circulations on the 30–50 day time scale;J. Atmos. Sci. 42 364–375
Krishnamurti T N and Subramanyam D 1982 The 30–50 day mode at 850 mb during MONEX;J. Atmos. Sci. 39 2088–2095
Lorenc A C 1984 The evolution of planetary scale 200 mb divergent flow during the FGGE year;Q.J.R. Meteorol. Soc. 110 427–441
Murakami T, Nakawa and He J H 1983 40–50 day oscillations during the 1979 northern hemispheric summer; Tech. Rep. No. UHMET 83-02. Department of Meteorology, University of Hawaii, Honolulu, Hawaii
W M O Tech. Note No. 79 (1966)
Yasumari T 1979 Cloudiness fluctuations associated with the northern hemisphere summer monsoon over India;J. Meteorol. Soc. Jpn. 58 225–229
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Kasture, S.V., Keshavamurty, R.N. Some aspects of the 30–50 day oscillation. Proc. Indian Acad. Sci. (Earth Planet Sci.) 96, 49–58 (1987). https://doi.org/10.1007/BF02842637
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DOI: https://doi.org/10.1007/BF02842637