| JIANG Tao,LIU Yun,WANG Wenzhi.The Luzon Strait transport variations during 1997~2000[J].Acta Oceanologica Sinica,2004,(1):83-90 |
| The Luzon Strait transport variations during 1997~2000 |
| The Luzon Strait transport variations during 1997~2000 |
| 投稿时间：2003-09-03 修订日期：2003-12-20 |
| DOI： |
| 中文关键词: Luzon Strait volume transport heat transport salt transport |
| 英文关键词:Luzon Strait volume transport heat transport salt transport |
| 基金项目: |
| 作者 | 单位 | E-mail | | JIANG Tao | Key Laboratory of Tropical Marine Environment Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China | jiangtao@scsio.ac.cn | | LIU Yun | Key Laboratory of Tropical Marine Environment Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China | | | WANG Wenzhi | Key Laboratory of Tropical Marine Environment Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China | |
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| 摘要点击次数: 917 |
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| 中文摘要: |
| Based on the output data from 1997 to 2000 obtained by the MITgcm's (general circulation model) adjoint assimilation method, volume, heat and salt transports through the Luzon Strait are calculated. The results indicate that there are obvious different characteristics between 1997 and 1998~2000 on the transports through the Luzon Strait. During 1997, theLuzon Strait had a mean net westward transport of 3.93×106 m3/s with a maximum transport of 7.34×106 m3/s in October. During 1998~2000, the Luzon Strait possessed an annual mean eastward transport of 0.93×106, 1.80×106 and 1.00×106 m3/s respectively with a maximum eastward transport of 4.10×106/3.31×106 m3/s in July 1998/1999 and 2.06×106 m3/s in April 2000, respectively. Moreover, the transports in 1997 indicated a difference from the other years, i.e.,that the ranges of westward inflows expanded more obviously to north of the Luzon Strait and downwards exceedingthose of the other years. The westward inflows expanded horizontally to the north part of the Luzon Strait until 21°N. |
| 英文摘要: |
| Based on the output data from 1997 to 2000 obtained by the MITgcm's (general circulation model) adjoint assimilation method, volume, heat and salt transports through the Luzon Strait are calculated. The results indicate that there are obvious different characteristics between 1997 and 1998~2000 on the transports through the Luzon Strait. During 1997, theLuzon Strait had a mean net westward transport of 3.93×106 m3/s with a maximum transport of 7.34×106 m3/s in October. During 1998~2000, the Luzon Strait possessed an annual mean eastward transport of 0.93×106, 1.80×106 and 1.00×106 m3/s respectively with a maximum eastward transport of 4.10×106/3.31×106 m3/s in July 1998/1999 and 2.06×106 m3/s in April 2000, respectively. Moreover, the transports in 1997 indicated a difference from the other years, i.e.,that the ranges of westward inflows expanded more obviously to north of the Luzon Strait and downwards exceedingthose of the other years. The westward inflows expanded horizontally to the north part of the Luzon Strait until 21°N. |
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