[1] Bjerknes J, 1966. A possible response of the atmospheric Hardley circulation to the equatorial anomalies of ocean temperature. Tellus. 18: 820-829.
[2] Bjerknes J, 1969. Atmosphere teleconnection from the equatorial Pacific. Mon. Wea. Rev., 97: 163-172
[3] Gong Yuanfa, Ji Liren, 1998. Numerical experiment of medium-range change of the subtropical high 1. The influence of the heating source over Tibet Plateau. J Trop. Meteor.(English edition), 4: 148-154.
[4] Huang Ronghui, Lu Li, 1989. Numerical simulation of the relationship between the anomaly of subtropical high over east Asia and convection in the western tropical Pacific. Adv. Atmos. Sci., 6: 202-214.
[5] Keshavamurty R N; 1982. Response of the atmosphere to the sea surface temperature anomalies over the equato-rial Pacific and the teleconnection of the Southern Oscillation. J Atmos. Sci., 39: 1241-1259.
[6] Kershaw R, 1988. The effect of a sea surface temperature anomaly on a prediction of the onset of south-west monsoon over Indian. Quart. J. Roy. Meteor. Soc., 114: 325-345.
[7] Moura A D, Shukla J, 1981.On the dynamics of droughts in northeast Brazil: Observation, theory, and numerical experiments with a general circulation model. J Atmos. Sci., 38: 2653-2675.
[8] M.S.C. (Meteorological Satellite Center), 1979. Monthly report of meteorological satellite center. June: 38-183.
[9] Rowntree P R, 1972. The influence of tropical east Pacific ocean on the atmosphere. Quart. J Roy. Meteor. Soc., 98: 290-321.
[10] Rowntree P R, 1976. Response of the atmosphere to a tropical Atlantic ocean temperature anomaly. Quart. J Roy Meteor. Soc,102: 607-625.
[11] Shukla S, 1975. Effect of Arabian sea surface temperature anomaly on the Indian summer monsoon: A numerical experiment with GFDL model. J Atmos. Sci., 40: 503-511.
[12] Shukla S. Wallace J M, 1983. Numerical simulation of the atmosphere response to equatorial Pacific sea surface temperature anomalies. J Atmos. Sci,40: 1613-I1630.