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TAO LIWEN,WANG XIAODONG. 1984. VARIATIONS OF THE SUMMER MONSOON IN THE SOUTH CHINA SEA. Acta Oceanologica Sinica, (3):339-348
VARIATIONS OF THE SUMMER MONSOON IN THE SOUTH CHINA SEA
VARIATIONS OF THE SUMMER MONSOON IN THE SOUTH CHINA SEA
Received:November 11, 1982  Revised:August 10, 1983
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Author NameAffiliation
TAO LIWEN Bureau of Water Conservancy, Beijing 
WANG XIAODONG Beijing Municipal Insititute for Scientific and Technical Information 
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Abstract:
      In this paper we investigated the variations of summer montoon in the South China Sea.We found that there are two kinds of oscillations in the intensity of the monsoon, one has a period of forty days, the other, fourteen days.We also found that the oscillation of a period of forty days is caused by the alternative extension of the monsoon trough eastward in the South China Sea and the extension of the subtropical anticyclone westward in the West Pacific.
It is our opinion that the summer monsoon in the West Pacific and the South China Sea is a system which is independent of the Indian monsoon and that the dividing line between these two monsoon systems is at the longitude 100°E.
中文摘要:
      In this paper we investigated the variations of summer montoon in the South China Sea.We found that there are two kinds of oscillations in the intensity of the monsoon, one has a period of forty days, the other, fourteen days.We also found that the oscillation of a period of forty days is caused by the alternative extension of the monsoon trough eastward in the South China Sea and the extension of the subtropical anticyclone westward in the West Pacific.
It is our opinion that the summer monsoon in the West Pacific and the South China Sea is a system which is independent of the Indian monsoon and that the dividing line between these two monsoon systems is at the longitude 100°E.
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