The evolution of a localized nonlinear wave of the Kelvin―Helmholtz instability with gravity

At the interface between two fluids of different density and in the presence of gravity, there are well known periodic surface waves which can propagate for long distances with little attenuation, as it is for instance the case at the surface of the sea. If wind is present, these waves progressively...

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Published inPhysics of fluids (1994) Vol. 24; no. 11
Main Authors ORAZZO, Annagrazia, HOEPFFNER, Jérôme
Format Journal Article
LanguageEnglish
Published Melville, NY American Institute of Physics 01.11.2012
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Abstract At the interface between two fluids of different density and in the presence of gravity, there are well known periodic surface waves which can propagate for long distances with little attenuation, as it is for instance the case at the surface of the sea. If wind is present, these waves progressively accumulate energy as they propagate and grow to large sizes-this is the Kelvin-Helmholtz instability. On the other hand, we show in this paper that for a given wind strength, there is potential for the growth of a localized nonlinear wave. This wave can reach a size such that the hydrostatic pressure drop from top to bottom equals the stagnation pressure of the wind. This process for the disruption of the flat interface is localized and nonlinear. We study the properties of this wave using numerical simulations of the Navier-Stokes equations.
AbstractList At the interface between two fluids of different density and in the presence of gravity, there are well known periodic surface waves which can propagate for long distances with little attenuation, as it is for instance the case at the surface of the sea. If wind is present, these waves progressively accumulate energy as they propagate and grow to large sizes-this is the Kelvin-Helmholtz instability. On the other hand, we show in this paper that for a given wind strength, there is potential for the growth of a localized nonlinear wave. This wave can reach a size such that the hydrostatic pressure drop from top to bottom equals the stagnation pressure of the wind. This process for the disruption of the flat interface is localized and nonlinear. We study the properties of this wave using numerical simulations of the Navier-Stokes equations.
Author ORAZZO, Annagrazia
HOEPFFNER, Jérôme
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Issue 11
Keywords Wave propagation
Kelvin Helmholtz instability
Wind effect
digital simulation
Modeling
Surface gravity wave
Non linear wave
Language English
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Snippet At the interface between two fluids of different density and in the presence of gravity, there are well known periodic surface waves which can propagate for...
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SubjectTerms Computational fluid dynamics
Density
Earth, ocean, space
Exact sciences and technology
External geophysics
Fluid flow
Fluids
Gravitation
Mathematical analysis
Navier-Stokes equations
Nonlinearity
Physics of the oceans
Sea-air exchange processes
Title The evolution of a localized nonlinear wave of the Kelvin―Helmholtz instability with gravity
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