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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Department of Mathematical Sciences, Univesity of Bath, Bath,BA2 7AY, United KingdomDepartment of Mathematical Sciences, Univesity of Bath, Bath,BA2 7AY, United Kingdom
Doak, A.
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Barros, R.
Milewski, P.A.
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Department of Mathematical Sciences, Univesity of Bath, Bath,BA2 7AY, United KingdomDepartment of Mathematical Sciences, Univesity of Bath, Bath,BA2 7AY, United Kingdom
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College of Science,Inner Mongolia University of Technology
Teaching Department of Basic Sciences,Shanxi Water Technical Professional CollegeCollege of Science,Inner Mongolia University of Technology
郭志萍
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宋金宝
赫晓东
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Chemical Engineering College,Inner Mongolia University of TechnologyCollege of Science,Inner Mongolia University of Technology
赫晓东
郭军明
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College of Science,Inner Mongolia University of TechnologyCollege of Science,Inner Mongolia University of Technology
郭军明
包曙红
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College of Science,Inner Mongolia University of TechnologyCollege of Science,Inner Mongolia University of Technology
包曙红
崔巍
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College of Science,Inner Mongolia University of TechnologyCollege of Science,Inner Mongolia University of Technology