Interaction among the East Asian Summer and Winter Monsoons, the Tropical Western Pacific and ENSO Cycle

  • Huang, Rong-Hui (LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences) ;
  • Lu, Ri-Yu (LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences) ;
  • Chen, Wen (LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences) ;
  • Chen, Ji-Rong (LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences)
  • Published : 2003.06.01

Abstract

Recent advances in the studies on the interaction between Asian monsoon and ENSO cycle are reviewed in this paper. Through the recent studies, the East Asian summer monsoon circulation system and the East Asian climate system have proposed. Moreover, different responses of the (winter and summer) monsoon circulation and summer rainfall anomalies in East Asia to ENSO cycle during its different stages have been understood further. Recently, the studies on the dynamical effect of East Asian monsoon on the thermal variability of the tropical western Pacific and ENSO cycle have been greatly advanced. These studies demonstrated further that ENSO cycle originates from the tropical western Pacific, and pointed out that the dynamical effect of East Asian winter and summer monsoons on ENSO cycle may be through the atmospheric circulation and zonal wind anomalies over the tropical western Pacific, which can excite the oceanic Kelvin wave and Rossby waves in the equatorial Pacific. Besides, the scientific problems in the interaction between Asian monsoon and ENSO cycle, which should be studied further in the near future, are also pointed out in this paper.

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