Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Direct Measurements of the Luzon Undercurrent | |
Hu, Dunxin1,2; Hu, Shijian1,2,3; Wu, Lixin4; Li, Lei4; Zhang, Linlin1,2; Diao, Xinyuan1,5; Chen, Zhaohui4; Li, Yuanlong1,2,3; Wang, Fan1,2; Yuan, Dongliang1,2; Hu, DX | |
2013-07-01 | |
发表期刊 | JOURNAL OF PHYSICAL OCEANOGRAPHY |
ISSN | 0022-3670 |
卷号 | 43期号:7页码:1417-1425 |
文章类型 | Article |
摘要 | The Luzon Undercurrent (LUC) was discovered about 20 years ago by geostrophic calculation from conductivity-temperature-depth (CTD) data. But it was not directly measured until 2010. From November 2010 to July 2011, the LUC was first directly measured by acoustic Doppler current profiler (ADCP) from a subsurface mooring at 18.0 degrees N, 122.7 degrees E to the east of Luzon Island. A number of new features of the LUC were identified from the measurements of the current. Its depth covers a range from 400 m to deeper than 700 m. The observed maximum velocity of the LUC, centered at about 650 m, could exceed 27.5 cm s(-1), four times stronger than the one derived from previous geostrophic calculation with hydrographic data. According to the time series available, the seasonality of the LUC strength is in winter > summer > spring. Significant intraseasonal variability (ISV; 70-80 days) of the LUC is exposed. Evidence exists to suggest that a large portion of the intraseasonal variability in the LUC is related to the westward propagation of mesoscale eddies from the east of the mooring site.; The Luzon Undercurrent (LUC) was discovered about 20 years ago by geostrophic calculation from conductivity-temperature-depth (CTD) data. But it was not directly measured until 2010. From November 2010 to July 2011, the LUC was first directly measured by acoustic Doppler current profiler (ADCP) from a subsurface mooring at 18.0 degrees N, 122.7 degrees E to the east of Luzon Island. A number of new features of the LUC were identified from the measurements of the current. Its depth covers a range from 400 m to deeper than 700 m. The observed maximum velocity of the LUC, centered at about 650 m, could exceed 27.5 cm s(-1), four times stronger than the one derived from previous geostrophic calculation with hydrographic data. According to the time series available, the seasonality of the LUC strength is in winter > summer > spring. Significant intraseasonal variability (ISV; 70-80 days) of the LUC is exposed. Evidence exists to suggest that a large portion of the intraseasonal variability in the LUC is related to the westward propagation of mesoscale eddies from the east of the mooring site. |
关键词 | Pacific Ocean Ocean Circulation Eddies In Situ Oceanic Observations Intraseasonal Variability Seasonal Cycle |
学科领域 | Oceanography |
DOI | 10.1175/JPO-D-12-0165.1 |
URL | 查看原文 |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Oceanography |
WOS类目 | Oceanography |
WOS记录号 | WOS:000329778000012 |
WOS关键词 | NORTH EQUATORIAL CURRENT ; WATER MASS-DISTRIBUTION ; PACIFIC ; CURRENTS ; COUNTERCURRENT ; VARIABILITY ; CIRCULATION ; MINDANAO ; COAST ; EAST |
WOS标题词 | Science & Technology ; Physical Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/16400 |
专题 | 海洋环流与波动重点实验室 |
通讯作者 | Hu, DX |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Key Lab Ocean Circulat & Wave, Qingdao 266071, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China 4.Ocean Univ China, Phys Oceanog Lab, Qingdao, Peoples R China 5.Chinese Acad Sci, R&D Ctr Marine Environm Engn & Technol, Qingdao 266071, Peoples R China |
第一作者单位 | 中国科学院海洋研究所; 海洋环流与波动重点实验室 |
推荐引用方式 GB/T 7714 | Hu, Dunxin,Hu, Shijian,Wu, Lixin,et al. Direct Measurements of the Luzon Undercurrent[J]. JOURNAL OF PHYSICAL OCEANOGRAPHY,2013,43(7):1417-1425. |
APA | Hu, Dunxin.,Hu, Shijian.,Wu, Lixin.,Li, Lei.,Zhang, Linlin.,...&Hu, DX.(2013).Direct Measurements of the Luzon Undercurrent.JOURNAL OF PHYSICAL OCEANOGRAPHY,43(7),1417-1425. |
MLA | Hu, Dunxin,et al."Direct Measurements of the Luzon Undercurrent".JOURNAL OF PHYSICAL OCEANOGRAPHY 43.7(2013):1417-1425. |
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