Tidal flow over three-dimensional topography in a stratified fluid

DOI10.1063/1.3253692zbMath1183.76283OpenAlexW2005978983MaRDI QIDQ5304916

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Publication date: 18 March 2010

Published in: Physics of Fluids (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1063/1.3253692

zbMATH Keywords

water wavesflow simulationnumerical analysistidesfluid oscillationsstratified flow

Mathematics Subject Classification ID

Fluid mechanics (76-XX)

Related Items (14)

Soliton generation by internal tidal beams impinging on a pycnocline: laboratory experiments ⋮ Internal wave energy flux from density perturbations in nonlinear stratifications ⋮ On generation and evolution of seaward propagating internal solitary waves in the northwestern South China Sea ⋮ Instabilities in internal gravity waves ⋮ Reflection of oscillating internal shear layers: nonlinear corrections ⋮ Near-field internal wave beams in two dimensions ⋮ Internal wave focusing by a horizontally oscillating torus ⋮ Nonlinear aspects of focusing internal waves ⋮ Boundary integrals for oscillating bodies in stratified fluids ⋮ Internal wave boluses as coherent structures in a continuously stratified fluid ⋮ Internal wave generation by oscillation of a sphere, with application to internal tides ⋮ Spatial structure of first and higher harmonic internal waves from a horizontally oscillating sphere ⋮ Added mass: a complex facet of tidal conversion at finite depth ⋮ Forcing of oceanic mean flows by dissipating internal tides

Cites Work

• A numerical method for large eddy simulation in complex geometries
• Large-Eddy Simulation of Reacting Turbulent Flows in Complex Geometries
• Laboratory experiments on the generation of internal tidal beams over steep slopes
• Internal gravity waves generated by oscillations of a sphere
• The generation of internal waves by vibrating elliptic cylinders. Part 2. Approximate viscous solution
• Tidal conversion at a very steep ridge
• Internal wave excitation by a vertically oscillating sphere
• Experimental study of internal gravity waves generated by supercritical topography
• Instability and focusing of internal tides in the deep ocean
• 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>

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