Abstract
The Asian monsoon circulation system can be divided into two subsystems, i.e., the East Asian monsoon system (EAMS) and the Indian monsoon system (IMS). In this paper the main elements including the Indian monsoon trough, the South Asian high. the upper easterly jet etc. and the interactions between EAMS and IMS are dealth with. The basic emphasis is put on the medium-range variations of the EAMS. Some significant results are obtained.
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