Decay of an internal tide due to random topography in the ocean
From MaRDI portal
Publication:2891685
DOI10.1017/jfm.2011.115zbMath1241.76107OpenAlexW2321779422MaRDI QIDQ2891685
Miranda C. Holmes-Cerfon, Oliver Bühler
Publication date: 15 June 2012
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://semanticscholar.org/paper/38c37b43cec07c7f4b7a54ab492e662e2920f5d3
Hydrology, hydrography, oceanography (86A05) Internal waves for incompressible inviscid fluids (76B55)
Related Items (14)
Resonant and near-resonant internal wave triads for non-uniform stratifications. Part 2. Vertically bounded domain with mild-slope bathymetry ⋮ Baroclinic tidal conversion: note on a paper of L.R.M. Maas ⋮ On functional equations leading to exact solutions for standing internal waves ⋮ Sensitivity of internal wave energy distribution over seabed corrugations to adjacent seabed features ⋮ Internal wave resonant triads in finite-depth non-uniform stratifications ⋮ Instabilities in internal gravity waves ⋮ On the appearance of internal wave attractors due to an initial or parametrically excited disturbance ⋮ Inherently unstable internal gravity waves due to resonant harmonic generation ⋮ Wave propagation in rotating shallow water in the presence of small-scale topography ⋮ Internal wave attractors over random, small-amplitude topography ⋮ Oblique internal-wave chain resonance over seabed corrugations ⋮ Parametric instability and wave turbulence driven by tidal excitation of internal waves ⋮ Energy budget in internal wave attractor experiments ⋮ Scattering of internal tides by irregular bathymetry of large extent
Cites Work
- Unnamed Item
- Topological methods in hydrodynamics
- Internal tide generation by arbitrary two-dimensional topography
- Waves and Mean Flows
- Particle dispersion by random waves in rotating shallow water
- Water waves in shallow channels of rapidly varying depth
- Tidal conversion at a very steep ridge
- Asymptotic theory of mixing stochastic ordinary differential equations
- Geometric focusing of internal waves
- Instability and focusing of internal tides in the deep ocean
- Two alternatives for solving hyperbolic boundary value problems of geophysical fluid dynamics
- On the reflexion of wave characteristics from rough surfaces
- V<scp>ERTICAL</scp> M<scp>IXING</scp>, E<scp>NERGY</scp>, <scp>AND THE</scp> G<scp>ENERAL</scp> C<scp>IRCULATION OF THE</scp> O<scp>CEANS</scp>
This page was built for publication: Decay of an internal tide due to random topography in the ocean
