| VARIATIONS OF THE SUMMER MONSOON IN THE SOUTH CHINA SEA |
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| 作者姓名： | 陶礼文 王晓东 |
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| 作者单位： | Bureau of Water Conservancy, Beijing;Beijing Municipal Insititute for Scientific and Technical Information |
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| 基金项目： | Presented at the Symposium on Monsoons in Kunming, October 16—21, 1982. |
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| 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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| 收稿时间： | 1982/11/11 0:00:00 |
| 修稿时间： | 1983/8/10 0:00:00 |
VARIATIONS OF THE SUMMER MONSOON IN THE SOUTH CHINA SEA |
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| TAO LIWEN and WANG XIAODONG.VARIATIONS OF THE SUMMER MONSOON IN THE SOUTH CHINA SEA[J].Acta Oceanologica Sinica,1984,3(3):339-348. |
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| Authors: | TAO LIWEN and WANG XIAODONG |
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| Affiliation: | 1.Bureau of Water Conservancy, Beijing2.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. |
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