摘 要: | Primarily based on the 1979 FGGE data an analysis is made of the circuktion differences between the East-Asian and Indian summer monsoons together with their oscillation features and also the interplay between various monsoon systems originating from the fact that the Asian monsoon area is divided into the East-Asian and Indian regions, of which the former is demarcated into the Nanhai (the South China Sea) and the Mainland subregions.
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