Results 101 to 110 of about 10,752 (148)
Shallow water equations for equatorial tsunami waves. [PDF]
Geyer A, Quirchmayr R.
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A Formulation for Fluid-Structure Interactions in febio Using Mixture Theory. [PDF]
Shim JJ, Maas SA, Weiss JA, Ateshian GA.
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Numerical study of interfacial solitary waves propagating under an elastic sheet. [PDF]
Wang Z +3 more
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Modelling cavitation erosion using fluid-material interaction simulations. [PDF]
Chahine GL, Hsiao CT.
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Bioinspired Morphing in Aerodynamics and Hydrodynamics: Engineering Innovations for Aerospace and Renewable Energy. [PDF]
Shahid F +6 more
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Atmosphere
This paper presents a mathematical model that describes the propagation of internal inertia–gravity waves in a stratified atmosphere under the approximations of an incompressible fluid and a traditional β-plane.
R. Zakinyan +2 more
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This paper presents a mathematical model that describes the propagation of internal inertia–gravity waves in a stratified atmosphere under the approximations of an incompressible fluid and a traditional β-plane.
R. Zakinyan +2 more
semanticscholar +1 more source
Various approximations of mathematical models of internal gravity waves in the stratified atmosphere
The Physics of FluidsTwo new mathematical models describing the propagation of internal gravity waves (IGWs) in a stratified atmosphere are proposed in this paper. The first model is called the non-Boussinesq gas approximation.
R. Zakinyan +3 more
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Internal solitary waves with a free surface generated by gravity collapse
The Physics of FluidsInternal solitary waves and their surface signatures generated by gravity collapse method are investigated through numerical simulations. The incompressible multiphase Navier–Stokes equations with three phases are solved, and the Volume of Fluid method ...
Zhenhua Lin
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Stokes waves in rotational flows: internal stagnation and overhanging profiles
Journal of Fluid MechanicsPeriodic travelling waves at the free surface of an incompressible inviscid fluid in two dimensions under gravity are numerically computed for an arbitrary vorticity distribution.
A. Doak, V. M. Hur, J. Vanden-Broeck
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