[1] Emanuel, K A,1987. An air-sea interaction model of intraseasonal oscillation in the tropics,J. ALmos. Sci.,44:2324-2340.
[2] Hayashi Y,1970. A theory of large-scale equatorial wave generated by condensation heat and accelerating the zonal wind,J. Meteor. Soc. Japan,48; 140-160.
[3] Lau K M,Peng L,1987. Origin of low-frequency oscillation in the tropical atmosphere,Part I .The basic theory, J. Atmos. Sci.,44:50-72.
[4] LauKM,Shen S H,1988. On the dynamics of intraseasonal oscillation and ENSO,J. Almos. Sci.,45; 1781-1797.
[5] Li Chongyin,1985. Actions of summer monsoon troughs (ridges) and tropical cyclones over south Asia and the moving CISK mode,ScienGia Sinica,28; 1197-1207.
[6] Li Chongyin,1990. Dynamical study on 30-50 day oscillation in the tropical atmosphere outside equator, Scientia Atmospherics Sinica,14; 101-112.
[7] Li Guolong,Liu Shikuo, 1993. Wave-CISK,evaporation-wind feedback and low-frequency oscillation, Scienlia AGmospherica Sinica,17:696-702.
[8] Liu Shikuo,Wang Jiyong,1990. A batoclinic semi-geosttophic model using the wave-CISK theory and low-frequency oscillation,Acla Meteor. Sinica,4:576-585.
[9] Neelin J D et al.,1987. Evaporation-wind feedback and low-frequency variability in the tropical atmosphere, J. Atoms. Sci.,44:2341-2348.
[10] T akahashi M,1987. A theory of low phase speed of the intraseasonal oscillation using the wave-CISK, J. Meteor. Soc. Japan,6:43-49.