Internal wave attractors in three-dimensional geometries: trapping by oblique reflection

被引:24
作者
Pillet, G. [1 ]
Ermanyuk, E. V. [2 ,3 ]
Maas, L. R. M. [4 ]
Sibgatullin, I. N. [5 ]
Dauxois, T. [1 ]
机构
[1] Univ Lyon, CNRS, ENS Lyon, UCBL,Lab Phys, F-69342 Lyon, France
[2] Lavrentyev Inst Hydrodynam, Av Lavrentyev 15, Novosibirsk 630090, Russia
[3] Novosibirsk State Univ, Pirogova Str 2, Novosibirsk 630090, Russia
[4] Univ Utrecht, Inst Marine & Atmospher Res, NL-3584 CC Utrecht, Netherlands
[5] Lomonosov Moscow State Univ, Moscow 119991, Russia
关键词
geophysical and geological flows; internal waves; stratified flows; EMPIRICAL MODE DECOMPOSITION; ONE SLOPING BOUNDARY; INERTIAL WAVES; RECTANGULAR BASIN; PROPAGATION; SPECTRUM; ENERGY; FLUID; OCEAN; INSTABILITY;
D O I
10.1017/jfm.2018.236
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
We study experimentally the propagation of internal waves in two different three-dimensional (3D) geometries, with a special emphasis on the refractive focusing due to the 3D reflection of obliquely incident internal waves on a slope. Both studies are initiated by ray tracing calculations to determine the appropriate experimental parameters. First, we consider a 3D geometry, the classical set-up to get simple, two-dimensional (2D) parallelogram-shaped attractors in which waves are forced in a direction perpendicular to a sloping bottom. Here, however, the forcing is of reduced extent in the along-slope, transverse direction. We show how the refractive focusing mechanism explains the formation of attractors over the whole width of the tank, even away from the forcing region. Direct numerical simulations confirm the dynamics, emphasize the role of boundary conditions and reveal the phase shifting in the transverse direction. Second, we consider a long and narrow tank having an inclined bottom, to simply reproduce a canal. In this case, the energy is injected in a direction parallel to the slope. Interestingly, the wave energy ends up forming 2D internal wave attractors in planes that are transverse to the initial propagation direction. This focusing mechanism prevents indefinite transmission of most of the internal wave energy along the canal.
引用
收藏
页码:203 / 225
页数:23
相关论文
共 53 条
[21]   A novel internal waves generator [J].
Gostiaux, L. ;
Didelle, H. ;
Mercier, S. ;
Dauxois, T. .
EXPERIMENTS IN FLUIDS, 2007, 42 (01) :123-130
[22]   Numerical simulation of a two-dimensional internal wave attractor [J].
Grisouard, Nicolas ;
Staquet, Chantal ;
Pairaud, Ivane .
JOURNAL OF FLUID MECHANICS, 2008, 614 :1-14
[23]   Internal wave attractors over random, small-amplitude topography [J].
Guo, Yuan ;
Holmes-Cerfon, Miranda .
JOURNAL OF FLUID MECHANICS, 2016, 787 :148-174
[24]   Observations on the wavenumber spectrum and evolution of an internal wave attractor [J].
Hazewinkel, Jeroen ;
Van Breevoort, Pieter ;
Dalziel, Stuart B. ;
Maas, Leo R. M. .
JOURNAL OF FLUID MECHANICS, 2008, 598 :373-382
[25]   Tomographic reconstruction of internal wave patterns in a paraboloid [J].
Hazewinkel, Jeroen ;
Maas, Leo R. M. ;
Dalziel, Stuart B. .
EXPERIMENTS IN FLUIDS, 2011, 50 (02) :247-258
[26]   Observations on the robustness of internal wave attractors to perturbations [J].
Hazewinkel, Jeroen ;
Tsimitri, Chrysanthi ;
Maas, Leo R. M. ;
Dalziel, Stuart B. .
PHYSICS OF FLUIDS, 2010, 22 (10)
[27]   The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationary time series analysis [J].
Huang, NE ;
Shen, Z ;
Long, SR ;
Wu, MLC ;
Shih, HH ;
Zheng, QN ;
Yen, NC ;
Tung, CC ;
Liu, HH .
PROCEEDINGS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1998, 454 (1971) :903-995
[28]  
JIA W, 1991, J GEOPHYS RES-OCEANS, V96, P16859, DOI 10.1029/91JC01580
[29]  
Kunze E., 2004, OCEANOGRAPHY, V17, P55, DOI DOI 10.5670/OCEANOG.2004.67
[30]   Internal wave focusing revisited; a reanalysis and new theoretical links [J].
Lam, Frans-Peter A. ;
Maas, Leo R. M. .
FLUID DYNAMICS RESEARCH, 2008, 40 (02) :95-122