Numerical Simulations of Internal Solitary Wave Evolution Beneath an Ice Keel

doi:10.1029/2020JC017068

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

	Numerical Simulations of Internal Solitary Wave Evolution Beneath an Ice Keel
	Zhang, Peiwen 6,7,8; Xu, Zhenhua 4,5,6,7,8; Li, Qun 3; You, Jia 6,7,8; Yin, Baoshu 4,5,6,7,8; Robertson, Robin 2; Zheng, Quanan 1
刊名	JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
	2022-02-01
卷号	127 期号:2 页码:21
关键词	Arctic ocean Sea ice Warming climate Internal wave Mixing Heat transfer
ISSN号	2169-9275
DOI	10.1029/2020JC017068
通讯作者	Xu, Zhenhua(xuzhenhua@qdio.ac.cn) ; Li, Qun(liqun@pric.org.cn)
英文摘要	The deformation and evolution of internal solitary waves (ISWs) beneath an ice keel can enable potential diapycnal mixing and facilitate upper ocean heat transport, despite a poor understanding of the underlying physics and energetics of ISWs in Polar environments. This study aims to understand the dynamic processes and mixing properties during the evolution of ISWs beneath ice keels in the Arctic Ocean using high-resolution, non-hydrostatic simulations. Ice keels can destabilize ISWs through overturning events. Consequently, the initial ISW disintegrates and transfers its energy into secondary smaller-scale waves. During the ISW-ice interaction, ISW-induced turbulent mixing can reach O(10(-3)) W/kg with a magnitude of resultant heat flux of O(10)W/m. Sensitivity experiments demonstrated that the ISW-ice interaction weakened as the ice keel depth decreased, and consequently, the resultant turbulent mixing and upward heat transfer also decreased. The ice keel depth was critical to the evolution and disintegration of an ISW beneath the ice keel, while the approximate ice keel shape had little effect. Our results provide an important but previously overlooked energy source for upper ocean heat transport in the Arctic Ocean.
资助项目	National Key Research and Development Program of China[2019YFE0105700] ; National Key Research and Development Program of China[2017YFA0604102] ; National Natural Science Foundation of China[92058202] ; National Natural Science Foundation of China[42176244] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42000000] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA22050202] ; CAS Key Research Program of Frontier Sciences[QYZDB-SSW-DQC024] ; CAS Key Deployment Project of Centre for Ocean Mega-Research of Science[COMS2020Q07] ; CAS-CSIRO Jointly Project[133244KYSB20190031] ; High Performance Computing Center at the IOCAS
WOS研究方向	Oceanography
语种	英语
出版者	AMER GEOPHYSICAL UNION
WOS记录号	WOS:000765614000011
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/178158]
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; Li, Qun
作者单位	1.Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA 2.Xiamen Univ Malaysia, China Asean Coll Marine Sci, Sepang, Malaysia 3.Polar Res Inst China, MNR Key Lab Polar Sci, Shanghai, Peoples R China 4.Chinese Acad Sci, Inst Oceanol, CAS Engn Lab Marine Ranching, Qingdao, Peoples R China 5.Pilot Natl Lab Marine Sci & Technol, Qingdao, Peoples R China 6.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China 7.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao, Peoples R China 8.Chinese Acad Sci, CAS Key Lab Ocean Circulat & Waves, Inst Oceanol, Qingdao, Peoples R China
推荐引用方式 GB/T 7714	Zhang, Peiwen,Xu, Zhenhua,Li, Qun,et al. Numerical Simulations of Internal Solitary Wave Evolution Beneath an Ice Keel[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2022,127(2):21.
APA	Zhang, Peiwen.,Xu, Zhenhua.,Li, Qun.,You, Jia.,Yin, Baoshu.,...&Zheng, Quanan.(2022).Numerical Simulations of Internal Solitary Wave Evolution Beneath an Ice Keel.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,127(2),21.
MLA	Zhang, Peiwen,et al."Numerical Simulations of Internal Solitary Wave Evolution Beneath an Ice Keel".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 127.2(2022):21.