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Characteristics of water exchange in the Luzon Strait during September 2006

文献类型：期刊论文

作者Zhou Hui2; Nan Feng1; Shi Maochong1; Zhou Liangming1; Guo Peifang1
刊名CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
出版日期2009-08-01
卷号27期号:3页码:650-657
关键词Luzon Strait Water Exchange Dynamic Calculation Volume Transport
ISSN号0254-4059
DOI10.1007/s00343-009-9175-2
文献子类Article
英文摘要The Luzon Strait is the only deep channel that connects the South China Sea (SCS) with the Pacific. The transport through the Luzon Strait is an important process influencing the circulation, heat and water budgets of the SCS. Early observations have suggested that water enters the SCS in winter but water inflow or outflow in summer is quite controversial. On the basis of hydrographic measurements from CTD along 120 degrees E in the Luzon Strait during the period from September 18 to 20 in 2006, the characteristics of temperature, salinity and density distributions are analyzed. The velocity and volume transport through the Luzon Strait are calculated using the method of dynamic calculation. The major observed results show that water exchanges are mainly from the Pacific to the South China Sea in the upper layer, and the flow is relatively weak and eastward in the deeper layer. The net volume transport of the Luzon Strait during the observation period is westward, amounts to about 3.25 Sv. This result is consistent with historical observations.; The Luzon Strait is the only deep channel that connects the South China Sea (SCS) with the Pacific. The transport through the Luzon Strait is an important process influencing the circulation, heat and water budgets of the SCS. Early observations have suggested that water enters the SCS in winter but water inflow or outflow in summer is quite controversial. On the basis of hydrographic measurements from CTD along 120 degrees E in the Luzon Strait during the period from September 18 to 20 in 2006, the characteristics of temperature, salinity and density distributions are analyzed. The velocity and volume transport through the Luzon Strait are calculated using the method of dynamic calculation. The major observed results show that water exchanges are mainly from the Pacific to the South China Sea in the upper layer, and the flow is relatively weak and eastward in the deeper layer. The net volume transport of the Luzon Strait during the observation period is westward, amounts to about 3.25 Sv. This result is consistent with historical observations.
学科主题Limnology ; Oceanography
URL标识查看原文
语种英语
WOS记录号WOS:000270742000033
公开日期2010-12-22
源URL[http://ir.qdio.ac.cn/handle/337002/2431]  
专题海洋研究所_海洋环流与波动重点实验室
作者单位1.Ocean Univ China, Coll Phys & Environm Oceanog, Qingdao 266100, Peoples R China
2.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Wave Studies, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714		 Zhou Hui,Nan Feng,Shi Maochong,et al. Characteristics of water exchange in the Luzon Strait during September 2006[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2009,27(3):650-657.
APA Zhou Hui,Nan Feng,Shi Maochong,Zhou Liangming,&Guo Peifang.(2009).Characteristics of water exchange in the Luzon Strait during September 2006.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,27(3),650-657.
MLA Zhou Hui,et al."Characteristics of water exchange in the Luzon Strait during September 2006".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 27.3(2009):650-657.

入库方式： OAI收割

来源：海洋研究所

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