A study of internal solitary waves observed on the continental shelf in the northwestern South China Sea
文献类型:期刊论文
作者 | Xu Zhenhua1,2; Yin Baoshu1,2; Hou Yijun1,2; Fan Zhisong3; Liu, Antony K.4 |
刊名 | ACTA OCEANOLOGICA SINICA
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出版日期 | 2010-05-01 |
卷号 | 29期号:3页码:18-25 |
关键词 | Elevation Internal Solitary Waves Diurnal Internal Tide Northwestern South China Sea |
ISSN号 | 0253-505X |
DOI | 10.1007/s13131-010-0033-z |
文献子类 | Article |
英文摘要 | Based on in-situ time series data from the acoustic Doppler current profiler (ADCP) and thermistor chain in Wenchang area, a sequence of internal solitary wave (ISW) packets was observed in September 2005, propagating northwest on the continental shelf of the northwestern South China Sea (SCS). Corresponding to different stratification of the water column and tidal condition, both elevation and depression ISWs were observed at the same mooring location with amplitude of 35 m and 25 m respectively in different days. Regular arrival of the remarkable ISW packets at approximately the diurnal tidal period and the dominance of diurnal internal waves in the study area, strongly suggest that the main energy source of the waves is the diurnal tide. Notice that the wave packets were all riding on the troughs and shoulders of the internal tides, they were probably generated locally from the shelf break by the evolution of the internal tides due to nonlinear and dispersive effects.; Based on in-situ time series data from the acoustic Doppler current profiler (ADCP) and thermistor chain in Wenchang area, a sequence of internal solitary wave (ISW) packets was observed in September 2005, propagating northwest on the continental shelf of the northwestern South China Sea (SCS). Corresponding to different stratification of the water column and tidal condition, both elevation and depression ISWs were observed at the same mooring location with amplitude of 35 m and 25 m respectively in different days. Regular arrival of the remarkable ISW packets at approximately the diurnal tidal period and the dominance of diurnal internal waves in the study area, strongly suggest that the main energy source of the waves is the diurnal tide. Notice that the wave packets were all riding on the troughs and shoulders of the internal tides, they were probably generated locally from the shelf break by the evolution of the internal tides due to nonlinear and dispersive effects. |
学科主题 | Oceanography |
URL标识 | 查看原文 |
语种 | 英语 |
WOS记录号 | WOS:000279357100003 |
公开日期 | 2010-12-24 |
源URL | [http://ir.qdio.ac.cn/handle/337002/5313] ![]() |
专题 | 海洋研究所_海洋环流与波动重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, KLOCAW, Qingdao 266071, Peoples R China 3.Ocean Univ China, Coll Phys & Environm Oceanog, Qingdao 266100, Peoples R China 4.NASA, Goddard Space Flight Ctr, Ocean Sci Branch, Greenbelt, MD 20771 USA |
推荐引用方式 GB/T 7714 | Xu Zhenhua,Yin Baoshu,Hou Yijun,et al. A study of internal solitary waves observed on the continental shelf in the northwestern South China Sea[J]. ACTA OCEANOLOGICA SINICA,2010,29(3):18-25. |
APA | Xu Zhenhua,Yin Baoshu,Hou Yijun,Fan Zhisong,&Liu, Antony K..(2010).A study of internal solitary waves observed on the continental shelf in the northwestern South China Sea.ACTA OCEANOLOGICA SINICA,29(3),18-25. |
MLA | Xu Zhenhua,et al."A study of internal solitary waves observed on the continental shelf in the northwestern South China Sea".ACTA OCEANOLOGICA SINICA 29.3(2010):18-25. |
入库方式: OAI收割
来源:海洋研究所
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