| SEAWATER FLUX OF THE SOUTH CHINA SEA |
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| 作者姓名： | 韩舞鹰 林洪英 容荣贵 |
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| 作者单位： | South China Sea Institute of Oceanology，Chinese Academy of Sciences，Guangzhou，510301 |
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| 基金项目： | National Natural Science Foundation of China (49176274). |
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| 摘 要： | The South China Sea water can be divided according to depth into three boxes by the pycnoclineand a sill.Using a box model with matter balance,the net seawater fluxes were calculated to be317.9×10~4 m~3/s in box Ⅰ for the upper homogeneous layer outflowing to the adjoining oceans;67×10~4 m~3/s in box Ⅲ for the water entering the basin;240×10~4 m~3/s in box Ⅱ for water entering theSouth China Sea.The upward speed of basin water was calculated to be 8.4×10~(-5) cm/s and that ofseawater flowing up along the pycnocline was calculated to be 8.9×10~(-5) cm/s.
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| 收稿时间： | 20 June 1994 |
Seawater flux of the South China Sea |
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| Han Wu-ying,Lin Hong-ying,Rong Rong-gui.SEAWATER FLUX OF THE SOUTH CHINA SEA[J].Chinese Journal of Oceanology and Limnology,1994,12(4):339-342. |
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| Authors: | Han Wu-ying Lin Hong-ying Rong Rong-gui |
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| Institution: | (1) South China Sea Institute of Oceanology, Chinese Academy of Sciences, 510301 Guangzhou |
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| Abstract: | The South China Sea water can be divided according to depth into three boxes by the pycnocline and a sill. Using a box model
with matter balance, the net seawater fluxes were calculated to be 317.9×104 m3/s in box I for the upper homogeneous layer outflowing to the adjoining oceans; 67×104 m3/s in box III for the water entering the basin; 240×104 m3/s in box II for water entering the South China Sea. The upward speed of basin water was calculated to be 8.4×10−5 cm/s and that of seawater flowing up along the pycnocline was calculated to be 8.9×10−5 cm/s.
The Project Supported by National Natural Science Foundation of China (49176274). |
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| Keywords: | South China Sea seawater flux |
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