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DOI: 10.1002/2016GL067812
论文题名:
Strong turbulent mixing induced by internal bores interacting with internal tide-driven vertically sheared flow
作者: Masunaga E.; Fringer O.B.; Yamazaki H.; Amakasu K.
刊名: Geophysical Research Letters
ISSN: 0094-9321
EISSN: 1944-9052
出版年: 2016
卷: 43, 期:5
起始页码: 2094
结束页码: 2101
语种: 英语
英文关键词: internal waves ; nonlinear internal bores ; turbulent mixing
Scopus关键词: Computational fluid dynamics ; Energy dissipation ; Kinetic energy ; Kinetics ; Shock tubes ; Tides ; Turbulent flow ; Internal bore ; Internal waves ; Iribarren numbers ; Mixing mechanisms ; Numerical results ; Topographic slope ; Turbulent kinetic energy ; Turbulent mixing ; Mixing
英文摘要: We observed the formation of an internal bore interacting with the vertically sheared flow generated during the previous phase of the internal tide, which resulted in strong turbulent mixing. The rate of turbulent kinetic energy dissipation reached on the order of 10-5 W kg-1 during the event. Numerical simulations reproduced the observed interaction of internal bores with the sheared flow and verified the hypothesized breaking and mixing mechanism. The numerical results indicated that the Iribarren number, or the ratio of the topographic slope to the internal wave slope, plays a major role in the mixing intensity and types of internal bores. It was found that waves with low Iribarren numbers lead to bores that interact with vertically sheared flows induced by the previous phase of the internal tide and are more likely to produce strong wave breaking and mixing. © 2016. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84959916670&doi=10.1002%2f2016GL067812&partnerID=40&md5=9ee405a0db51c4e7ccac157a6557ed2d
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/10284
Appears in Collections:科学计划与规划
气候变化与战略

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作者单位: Department of Ocean Sciences, Tokyo University of Marine Science and Technology, Tokyo, Japan

Recommended Citation:
Masunaga E.,Fringer O.B.,Yamazaki H.,et al. Strong turbulent mixing induced by internal bores interacting with internal tide-driven vertically sheared flow[J]. Geophysical Research Letters,2016-01-01,43(5).
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