Three-dimensional numerical simulation of internal tides that radiated from the Luzon Strait into the Western Pacific

doi:10.1007/s00343-017-5376-2

CORC > 海洋研究所 > 中国科学院海洋研究所 > 海洋环流与波动重点实验室

	Three-dimensional numerical simulation of internal tides that radiated from the Luzon Strait into the Western Pacific
	Liu Kun1,2,4 ; Xu Zhenhua 1,2,3; Yin Baoshu 1,2,3
刊名	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
	2017-11-01
卷号	35 期号:6 页码:1275-1286
关键词	internal tides numerical simulation Luzon Strait Western Pacific
ISSN号	0254-4059
DOI	10.1007/s00343-017-5376-2
通讯作者	Xu Zhenhua(xuzhenhua@qdio.ac.cn)
英文摘要	Recent satellite altimeter observations have indicated that internal tides (ITs) from the Luzon Strait (LS) propagate more than 2 500 km into the Western Pacific (WP). This study used a high-resolution three-dimensional numerical model to reproduce and examine the ITs radiation process. The propagation of diurnal and semidiurnal ITs showed different patterns and variations. Diurnal ITs with lower frequency were affected more by the earth's rotation and they were bent more toward the equator than semidiurnal ITs. ITs phase speeds are functions of latitude and diurnal ITs showed greater distinctions of phase speeds during propagation. For M-2 ITs, the wavelength remained nearly unchanged but the beam width increased significantly during propagation away from the LS. For diurnal ITs (K-1 and O-1), the wavelength decreased noticeably with latitude, while the beam width varied little during propagation because of blocking by land. Baroclinic energy was also examined as a complement to satellite results reported by Zhao (2014). The magnitude of the generated baroclinic energy flux reduced remarkably within 300 km from the generation site but it then decayed slowly when propagating into abyssal sea. Baroclinic energy of diurnal ITs was found to dissipate at a slower rate than semidiurnal ITs along the main propagation path in the WP.
资助项目	National Natural Science Foundation of China[41528601] ; National Natural Science Foundation of China[41376029] ; National Natural Science Foundation of China[U1406401] ; National Natural Science Foundation of China[41421005] ; CAS[XDA10020104] ; CAS[XDA10020101] ; CAS Interdisciplinary Innovation Team
WOS研究方向	Marine & Freshwater Biology ; Oceanography
语种	英语
出版者	SCIENCE PRESS
WOS记录号	WOS:000415810900002
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/157284]
专题	海洋研究所_海洋环流与波动重点实验室
通讯作者	Xu Zhenhua
作者单位	1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Key Lab Ocean Circulat & Waves KLOCAW, Qingdao 266071, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Ocean & Climate Dynam, Qingdao 266071, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式 GB/T 7714	Liu Kun,Xu Zhenhua,Yin Baoshu. Three-dimensional numerical simulation of internal tides that radiated from the Luzon Strait into the Western Pacific[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2017,35(6):1275-1286.
APA	Liu Kun,Xu Zhenhua,&Yin Baoshu.(2017).Three-dimensional numerical simulation of internal tides that radiated from the Luzon Strait into the Western Pacific.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,35(6),1275-1286.
MLA	Liu Kun,et al."Three-dimensional numerical simulation of internal tides that radiated from the Luzon Strait into the Western Pacific".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 35.6(2017):1275-1286.