Experimental study on transformation and energy properties of depression internal solitary wave over a bottom step

被引:11
作者
Zou, Li [1 ,2 ]
Wen, Zehua [1 ]
Sun, Tiezhi [1 ]
Ma, Xinyu [1 ]
Wang, Xueyu [1 ]
机构
[1] Dalian Univ Technol, State Key Lab Struct Anal Ind Equipment, Sch Naval Architecture, Dalian 116024, Peoples R China
[2] Collaborat Innovat Ctr Adv Ship & Deep Sea Explor, Shanghai 200240, Peoples R China
基金
中国国家自然科学基金;
关键词
CHINA SEA; PROPAGATION; BREAKING; GENERATION; EVOLUTION; SOLITONS; CONVERSION; FORCES; FLUID;
D O I
10.1063/5.0038875
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Waveform deformation and breaking are widespread phenomena when internal solitary waves (ISWs) encounter changing topographies, which have been observed in many parts of oceans. In this study, experiments are performed in a series of combinations of bottom step topographies with different heights and ISWs in different amplitudes within a two-layer stratified fluid system. According to experimental results, the evolution processes of ISWs over the bottom step are classified into four typical regimes as the wave-step interaction varying from weak to strong, which are the transmission regime, transitional regime, breaking regime, and reflection regime, corresponding to the evolution patterns of steady passage, deformation, breaking, and strong reflection, respectively. To describe the intensity of wave-step interaction, a new improved interaction parameter is proposed, which takes both relative amplitude of ISWs and relative topography changes into consideration, and achieved better effectiveness in defining the boundaries between different regimes. In terms of energy properties, with the wave-step interaction becoming stronger, the transmission ratio keeps decreasing throughout all regimes, while the reflection wave starts to appear since the breaking regime and its energy keeps increasing. At the critical point between the breaking regime and reflection regime, the reflection ratio equals the transmission ratio, and the energy loss ratio reaches its maximum. Published under license by AIP Publishing.
引用
收藏
页数:18
相关论文
共 46 条
[1]  
Alpers W, 2005, INT GEOSCI REMOTE SE, P4784
[2]   The degeneration of internal waves in lakes with sloping topography [J].
Boegman, L ;
Ivey, GN ;
Imberger, J .
LIMNOLOGY AND OCEANOGRAPHY, 2005, 50 (05) :1620-1637
[3]   An experimental study of stratified mixing caused by internal solitary waves in a two-layered fluid system over variable seabed topography [J].
Chen, Chen-Yuan .
OCEAN ENGINEERING, 2007, 34 (14-15) :1995-2008
[4]   Experimental investigation of internal solitary wave forces on a semi-submersible [J].
Chen, Min ;
Chen, Ke ;
You, Yun-Xiang .
OCEAN ENGINEERING, 2017, 141 :205-214
[5]   Laboratory observations on internal solitary wave evolution on steep and inverse uniform slopes [J].
Chen, -Yuan Chen ;
Hsu, John Rong-Chung ;
Chen, Hsin-Hsun ;
Kuo, Ching-Feng ;
Cheng, Min-Hung .
OCEAN ENGINEERING, 2007, 34 (01) :157-170
[6]   An investigation on internal solitary waves in a two-layer fluid: Propagation and reflection from steep slopes [J].
Chen, -Yuan Chen ;
Hsu, John Rong-Chung ;
Cheng, Min-Hung ;
Chen, Hsin-Hsun ;
Kuo, Ching-Feng .
OCEAN ENGINEERING, 2007, 34 (01) :171-184
[7]   Effect of porosity on an internal solitary wave propagating over a porous trapezoidal obstacle [J].
Cheng, Ming-Hung ;
Hsieh, Chih-Min ;
Hsu, John R-C. ;
Hwang, Robert R. .
OCEAN ENGINEERING, 2017, 130 :126-141
[8]   Effect of frontal slope on waveform evolution of a depression interfacial solitary wave across a trapezoidal obstacle [J].
Cheng, Ming-Hung ;
Hsu, John R. C. .
OCEAN ENGINEERING, 2013, 59 :164-178
[9]   Laboratory experiments on depression interfacial solitary waves over a trapezoidal obstacle with horizontal plateau [J].
Cheng, Ming-Hung ;
Hsu, John R. C. .
OCEAN ENGINEERING, 2010, 37 (8-9) :800-818
[10]   Numerical investigation of an internal solitary wave interaction with horizontal cylinders [J].
Ding, Weiye ;
Ai, Congfang ;
Jin, Sheng ;
Lin, Jinbo .
OCEAN ENGINEERING, 2020, 208