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Proceedings of the European Wave and Tidal Energy Conference, 2023
Internal waves are ubiquitous oceanographic features that occur in various forms across the world’s oceans. They manifest themselves as interface waves across ocean density layers that represent the interplay between buoyancy and gravitational forces, and are typically classified as linear and nonlinear internal waves.
Kaustubha Raghukumar +3 more
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Internal waves are ubiquitous oceanographic features that occur in various forms across the world’s oceans. They manifest themselves as interface waves across ocean density layers that represent the interplay between buoyancy and gravitational forces, and are typically classified as linear and nonlinear internal waves.
Kaustubha Raghukumar +3 more
openaire +2 more sources
ISPH wave simulation by using an internal wave maker
Coastal Engineering, 2015 Peng-zhi Lin, Songdong Shao
exaly +2 more sources
Acta Astronautica, 2020
The shock wave/boundary-layer interaction is a common phenomenon, and it occurs in the internal and external flow fields of the hypersonic vehicle. Then, the separation, the oscillatory flow structures, the heat transfer localization and the pressure ...
Wei Huang, Yan-Guang Yang, Li Yan
exaly +2 more sources
The shock wave/boundary-layer interaction is a common phenomenon, and it occurs in the internal and external flow fields of the hypersonic vehicle. Then, the separation, the oscillatory flow structures, the heat transfer localization and the pressure ...
Wei Huang, Yan-Guang Yang, Li Yan
exaly +2 more sources
2013
This chapter focuses on internal gravity waves in a stable thermal stratification. When the amplitude of the fluid velocity is small relative to the amplitude of the phase velocity, a linear analysis, which neglects advection, provides insight to the relation between the wavelength and frequency of internal gravity waves.
B. Sutherland
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This chapter focuses on internal gravity waves in a stable thermal stratification. When the amplitude of the fluid velocity is small relative to the amplitude of the phase velocity, a linear analysis, which neglects advection, provides insight to the relation between the wavelength and frequency of internal gravity waves.
B. Sutherland
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Studies in Applied Mathematics, 1992
The expansion procedure introduced by Benney (1966) for weakly nonlinear, planar shallow‐water waves is used to provide an alternative derivation of the more general results of Benjamin (1966) for shallow fluid layers possessing arbitrary vertical stratification and horizontal shear.
Weidman, P. D., Velarde, M. G.
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The expansion procedure introduced by Benney (1966) for weakly nonlinear, planar shallow‐water waves is used to provide an alternative derivation of the more general results of Benjamin (1966) for shallow fluid layers possessing arbitrary vertical stratification and horizontal shear.
Weidman, P. D., Velarde, M. G.
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The Physics of Fluids, 1978
A numerical solution of the Benjamin–Ono equation for internal waves shows soliton behavior. Two and three Lorentzian solitons pass through one another unscathed. An initial Lorentzian with larger than soliton amplitude decays into solitons, with velocities predicted by the five conservation laws.
Meiss, J. D., Pereira, N. R.
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A numerical solution of the Benjamin–Ono equation for internal waves shows soliton behavior. Two and three Lorentzian solitons pass through one another unscathed. An initial Lorentzian with larger than soliton amplitude decays into solitons, with velocities predicted by the five conservation laws.
Meiss, J. D., Pereira, N. R.
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1997
The basic theory of internal solitary waves is developed, with the main emphasis on environmental situations, such as the many occurrences of such waves in shallow coastal seas and in the atmospheric boundary layer. Commencing with the equations of motion for an inviscid, incompressible density-stratified fluid, we describe asymptotic reductions to ...
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The basic theory of internal solitary waves is developed, with the main emphasis on environmental situations, such as the many occurrences of such waves in shallow coastal seas and in the atmospheric boundary layer. Commencing with the equations of motion for an inviscid, incompressible density-stratified fluid, we describe asymptotic reductions to ...
openaire +1 more source