The evolution of mode-2 internal solitary waves modulated by background shear currents

doi:10.5194/npg-25-441-2018

IOCAS-IR > 海洋环流与波动重点实验室

	The evolution of mode-2 internal solitary waves modulated by background shear currents
	Zhang, Peiwen1,3,4 ; Xu, Zhenhua 1,2,3,4; Li, Qun 5; Yin, Baoshu 1,2,3,4; Hou, Yijun 1,2,3,4; Liu, Antony K.6
	2018-06-25
发表期刊	NONLINEAR PROCESSES IN GEOPHYSICS
ISSN	1023-5809
卷号	25 期号:2 页码:441-455
通讯作者	Xu, Zhenhua([email protected]) ; Li, Qun([email protected])
摘要	The evolution of mode-2 internal solitary waves (ISWs) modulated by background shear currents was investigated numerically. The mode-2 ISW was generated by the "lock-release" method, and the background shear current was initialized after the mode-2 ISW became stable. Five sets of experiments were conducted to assess the sensitivity of the modulation process to the direction, polarity, magnitude, shear layer thickness and offset extent of the background shear current. Three distinctly different shear-induced waves were identified as a forward-propagating long wave, oscillating tail and amplitude-modulated wave packet in the presence of a shear current. The amplitudes of the forward-propagating long wave and the amplitude-modulated wave packet are proportional to the magnitude of the shear but inversely proportional to the thickness of the shear layer, as well as the energy loss of the mode-2 ISW during modulation. The oscillating tail and amplitude-modulated wave packet show symmetric variation when the background shear current is offset upward or downward, while the forward propagating long wave was insensitive to it. For comparison, one control experiment was configured according to the observations of Shroyer et al. (2010); in the first 30 periods, similar to 36% of total energy was lost at an average rate of 9Wm 1 in the presence of the shear current; it would deplete the energy of initial mode(-2) ISWs in similar to 4.5 h, corresponding to a propagation distance of similar to 5 km, which is consistent with in situ data.
DOI	10.5194/npg-25-441-2018
收录类别	SCI
语种	英语
资助项目	National Key Research and Development Program of China[2016YFC1401404]###1128; National Key Research and Development Program of China[2017YFA0604102]###333; QNLM[2016ASKJ12]###818; National Natural Science Foundation of China[41528601]###1129; National Natural Science Foundation of China[41676006]###1130; National Natural Science Foundation of China[41421005]###312; National Natural Science Foundation of China[41576189]###1990; Youth Innovation Promotion Association, CAS###1991; CAS Interdisciplinary Innovation Team Oceanic Mesoscale Processes and Ecology Effects###1992; Key Research Program of Frontier Science, CAS[QYZDB-SSW-DQC024]###1993; Strategic Pioneering Research Program of CAS[XDA11020104]###1988; Strategic Pioneering Research Program of CAS[XDA11020101]###1989; High Performance Computing Center at the IOCAS###1019; National Key Research and Development Program of China[2016YFC1401404]###1128; National Key Research and Development Program of China[2017YFA0604102]###333; QNLM[2016ASKJ12]###818; National Natural Science Foundation of China[41528601]###1129; National Natural Science Foundation of China[41676006]###1130; National Natural Science Foundation of China[41421005]###312; National Natural Science Foundation of China[41576189]###1990; Youth Innovation Promotion Association, CAS###1991; CAS Interdisciplinary Innovation Team Oceanic Mesoscale Processes and Ecology Effects###1992; Key Research Program of Frontier Science, CAS[QYZDB-SSW-DQC024]###1993; Strategic Pioneering Research Program of CAS[XDA11020104]###1988; Strategic Pioneering Research Program of CAS[XDA11020101]###1989; High Performance Computing Center at the IOCAS###1019; National Key Research and Development Program of China[2016YFC1401404]; National Key Research and Development Program of China[2017YFA0604102]; QNLM[2016ASKJ12]; National Natural Science Foundation of China[41528601]; National Natural Science Foundation of China[41676006]; National Natural Science Foundation of China[41421005]; National Natural Science Foundation of China[41576189]; Youth Innovation Promotion Association, CAS; CAS Interdisciplinary Innovation Team Oceanic Mesoscale Processes and Ecology Effects; Key Research Program of Frontier Science, CAS[QYZDB-SSW-DQC024]; Strategic Pioneering Research Program of CAS[XDA11020104]; Strategic Pioneering Research Program of CAS[XDA11020101]; High Performance Computing Center at the IOCAS
WOS研究方向	Geochemistry & Geophysics ; Meteorology & Atmospheric Sciences
WOS类目	Geochemistry & Geophysics ; Meteorology & Atmospheric Sciences
WOS记录号	WOS:000436122200001
出版者	COPERNICUS GESELLSCHAFT MBH
引用统计	被引频次：15[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/159478
专题	海洋环流与波动重点实验室
通讯作者	Xu, Zhenhua; Li, Qun
作者单位	1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Qingdao 266071, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China 5.Polar Res Inst China, Shanghai 200136, Peoples R China 6.Ocean Univ China, Qingdao 266100, Peoples R China
推荐引用方式 GB/T 7714	Zhang, Peiwen,Xu, Zhenhua,Li, Qun,et al. The evolution of mode-2 internal solitary waves modulated by background shear currents[J]. NONLINEAR PROCESSES IN GEOPHYSICS,2018,25(2):441-455.
APA	Zhang, Peiwen,Xu, Zhenhua,Li, Qun,Yin, Baoshu,Hou, Yijun,&Liu, Antony K..(2018).The evolution of mode-2 internal solitary waves modulated by background shear currents.NONLINEAR PROCESSES IN GEOPHYSICS,25(2),441-455.
MLA	Zhang, Peiwen,et al."The evolution of mode-2 internal solitary waves modulated by background shear currents".NONLINEAR PROCESSES IN GEOPHYSICS 25.2(2018):441-455.

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