Role of Warming over the Tibetan Plateau in Early Onset of the Summer Monsoon over the Bay of Bengal and the South China Sea
Author:
Affiliation:
1. Institute of Geoscience, University of Tsukuba
2. Research Fellow of the Japan Society for Promotion of Science
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/76/1/76_1_1/_pdf
Reference36 articles.
1. Chen, T. -C. and J. -M. Chen, 1995: An observational study of the South China Sea monsoon during the 1979 summer: Onset and life cycle. Mon. Wea. Rev., 123, 2295-2318.
2. Chen, T. -C. and K. Takahashi, 1994: Diurnal variation of outgoing longwave radiation in the vicinity of the South China Sea: Effect of intraseasonal oscillation. Mon. Wea. Rev., 123, 566-577.
3. Chen, T. -C., M. -C. Yen and M. Murakami, 1988: The water vapor transport associated with the 30-50-day oscillation over the Asian monsoon regions during 1979 summer. Mon. Wea. Rev., 116, 1983-2002.
4. Chen, T. -C. and S. -P. Weng, 1996: Some effects of intraseasonal oscillation on the equatorial waves over the western tropical Pacific-South China Sea region during the Northern Summer. Mon. Wea. Rev., 124, 751-756.
5. Fu, C. and J. O. Fletcher, 1985: The relationship between Tibet-tropical ocean thermal contrast and interannual variability of Indian monsoon rainfall. J. Climate Appl. Meteor., 24, 841-847.
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