Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Anti-cyclonic eddies northwest of Luzon in summer-fall observed by satellite altimeters | |
Yuan, Dongliang; Han, Weiqing; Hu, Dunxin | |
2007-07-12 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
卷号 | 34期号:13页码:L13610 |
文章类型 | Article |
摘要 | Anti-cyclonic eddies northwest of Luzon of the Philippines in summer-fall are identified in the merged data products of satellite altimeters of Topex/Poseidon, Jason-1 and European Research Satellites. The generation and propagation of the anti-cyclonic eddies, which are confirmed by satellite ocean color data, are found to be a seasonal phenomenon that is phase-locked to the onset of the southwesterly monsoon and the relaxation of the cyclonic wind curl in the northeastern South China Sea. The eddies originate from northwest of Luzon in summer, move across the northeastern South China Sea to reach the China continental slope in fall, and propagate southwestward along the continental slope in fall-winter, inducing shelfbreak current variations in the western South China Sea in fall-winter. The anti-cyclonic eddy discovered by Li et al. (1998) in the northern South China Sea is found to originate from northwest of Luzon and carry primarily the South China Sea waters. It does not appear to be an eddy shed from the Kuroshio in the Luzon Strait area as alluded by Li et al. (1998) and others.; Anti-cyclonic eddies northwest of Luzon of the Philippines in summer-fall are identified in the merged data products of satellite altimeters of Topex/Poseidon, Jason-1 and European Research Satellites. The generation and propagation of the anti-cyclonic eddies, which are confirmed by satellite ocean color data, are found to be a seasonal phenomenon that is phase-locked to the onset of the southwesterly monsoon and the relaxation of the cyclonic wind curl in the northeastern South China Sea. The eddies originate from northwest of Luzon in summer, move across the northeastern South China Sea to reach the China continental slope in fall, and propagate southwestward along the continental slope in fall-winter, inducing shelfbreak current variations in the western South China Sea in fall-winter. The anti-cyclonic eddy discovered by Li et al. (1998) in the northern South China Sea is found to originate from northwest of Luzon and carry primarily the South China Sea waters. It does not appear to be an eddy shed from the Kuroshio in the Luzon Strait area as alluded by Li et al. (1998) and others. |
关键词 | South China Sea Mesoscale Eddies Kuroshio Circulation Strait Ocean |
DOI | 10.1029/2007GL029401 |
URL | 查看原文 |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000248024300001 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/6252 |
专题 | 海洋环流与波动重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China 2.Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA |
推荐引用方式 GB/T 7714 | Yuan, Dongliang,Han, Weiqing,Hu, Dunxin. Anti-cyclonic eddies northwest of Luzon in summer-fall observed by satellite altimeters[J]. GEOPHYSICAL RESEARCH LETTERS,2007,34(13):L13610. |
APA | Yuan, Dongliang,Han, Weiqing,&Hu, Dunxin.(2007).Anti-cyclonic eddies northwest of Luzon in summer-fall observed by satellite altimeters.GEOPHYSICAL RESEARCH LETTERS,34(13),L13610. |
MLA | Yuan, Dongliang,et al."Anti-cyclonic eddies northwest of Luzon in summer-fall observed by satellite altimeters".GEOPHYSICAL RESEARCH LETTERS 34.13(2007):L13610. |
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