Dynamics of internal solitary waves in shallow water were studied with a strongly nonlinear internal long wave model in a three-layer fluid system. It is an extension of the two-layer MCC (Miyata, Choi, and Camassa) model, which is derived under the assumption that the characteristic wavelength is long in comparison to the thickness of each fluid layer. Phase velocity was assessed to understand the stability of solitary waves when they propagate. The instability mechanism turns out to be a Kelvin-Helmholtz type instability that is similar to the twolayer MCC model. We numerically investigated the three-layer model in terms of the effects of the middle layer and non-uniform bottom topography, and examined the generation of solitary waves to demonstrate the rich dynamics of the three-layer model.
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Univ N Carolina, Dept Math, Chapel Hill, NC 27599 USAUniv N Carolina, Dept Math, Chapel Hill, NC 27599 USA
Camassa, R.
Rusas, P. -O.
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Ostfold Univ Coll, Fac Comp Sci, N-1757 Halden, NorwayUniv N Carolina, Dept Math, Chapel Hill, NC 27599 USA
Rusas, P. -O.
Saxena, A.
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Los Alamos Natl Lab, Div Theoret, Los Alamos, NM 87545 USA
Los Alamos Natl Lab, Ctr Nonlinear Studies, Los Alamos, NM 87545 USAUniv N Carolina, Dept Math, Chapel Hill, NC 27599 USA
Saxena, A.
Tiron, R.
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Univ N Carolina, Dept Math, Chapel Hill, NC 27599 USAUniv N Carolina, Dept Math, Chapel Hill, NC 27599 USA
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Volodymyr Vynnychenko Cent Ukrainian State Pedag, Fac Math & Phys, Kropyvnytskyi, UkraineVolodymyr Vynnychenko Cent Ukrainian State Pedag, Fac Math & Phys, Kropyvnytskyi, Ukraine
Naradovyi, V.
Kharchenko, D.
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Volodymyr Vynnychenko Cent Ukrainian State Pedag, Fac Math & Phys, Kropyvnytskyi, UkraineVolodymyr Vynnychenko Cent Ukrainian State Pedag, Fac Math & Phys, Kropyvnytskyi, Ukraine