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Frontal collision of internal solitary waves of first mode
Institution:1. Institute of Mathematical Machine and System Problems, Glushkov av., 42, Kiev 03187, Ukraine;2. Korea Institute of Ocean Science and Technology, 787, Haean-ro, Ansan, 426-744, Republic of Korea;1. Acoustics Division, U.S. Naval Research Laboratory, Stennis Space Ctr., MS 39529, USA;2. Dipartimento di Ingegneria, Università degli Studi di Perugia, 06125 Perugia, Italy;1. Department of Marine Biology and Aquaculture, College of Marine Science, Gyeongsang National University, 38 Cheondaegukchi-Gil, Tongyeong, Gyeongnam 650-160, Republic of Korea;2. Pathology Division, National Fisheries Research and Development Institute, Busan 619-900, Republic of Korea;1. Laboratoire Ondes et Milieux Complexes (LOMC) UMR CNRS 6294, Université Le Havre Normandie, France;2. Département de Mathématiques, Université de Lomé, Togo;1. Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA, USA;2. Institute for Mathematical and Computational Engineering, School of Engineering and Faculty of Mathematics, Pontificia Universidad Católica de Chile, Chile;3. INGMAT R&D Centre, José Miguel de la Barra 412, 4to piso, Santiago, Chile
Abstract:The dynamics and energetics of a frontal collision of internal solitary waves (ISW) of first mode in a fluid with two homogeneous layers separated by a thin interfacial layer are studied numerically within the framework of the Navier–Stokes equations for stratified fluid. It was shown that the head-on collision of internal solitary waves of small and moderate amplitude results in a small phase shift and in the generation of dispersive wave train travelling behind the transmitted solitary wave. The phase shift grows as amplitudes of the interacting waves increase. The maximum run-up amplitude during the wave collision reaches a value larger than the sum of the amplitudes of the incident solitary waves. The excess of the maximum run-up amplitude over the sum of the amplitudes of the colliding waves grows with the increasing amplitude of interacting waves of small and moderate amplitudes whereas it decreases for colliding waves of large amplitude. Unlike the waves of small and moderate amplitudes collision of ISWs of large amplitude was accompanied by shear instability and the formation of Kelvin–Helmholtz (KH) vortices in the interface layer, however, subsequently waves again become stable. The loss of energy due to the KH instability does not exceed 5%–6%. An interaction of large amplitude ISW with even small amplitude ISW can trigger instability of larger wave and development of KH billows in larger wave. When smaller wave amplitude increases the wave interaction was accompanied by KH instability of both waves.
Keywords:Internal solitary waves  Head-on collision  Numerical modelling  Phase shift  Kelvin–Helmholtz instability
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