Tidal conversion at a very steep ridge

DOI10.1017/S0022112003006098zbMath1053.76010OpenAlexW1969169565MaRDI QIDQ4465459

Stefan G. Llewellyn Smith, William R. Young

Publication date: 9 June 2004

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/s0022112003006098

zbMATH Keywords

internal gravity wavesnon-uniform buoyancy frequency

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Internal waves for incompressible inviscid fluids (76B55) Stratification effects in inviscid fluids (76B70)

Related Items (24)

Decay of an internal tide due to random topography in the ocean ⋮ Direct and large-eddy simulations of internal tide generation at a near-critical slope ⋮ Large-amplitude topographic waves in 2D stratified flow ⋮ A conundrum in conversion ⋮ Experimental study of internal gravity waves generated by supercritical topography ⋮ Tidal flow over three-dimensional topography in a stratified fluid ⋮ Internal wave energy flux from density perturbations in nonlinear stratifications ⋮ Modal decomposition of polychromatic internal wave fields in arbitrary stratifications ⋮ Internal tide generation from non-uniform barotropic body forcing ⋮ Reflection of oscillating internal shear layers: nonlinear corrections ⋮ Near-field internal wave beams in two dimensions ⋮ Internal wave focusing by a horizontally oscillating torus ⋮ Boundary integrals for oscillating bodies in stratified fluids ⋮ Tidal conversion and turbulence at a model ridge: direct and large eddy simulations ⋮ Internal gravity waves, boundary integral equations and radiation conditions ⋮ Can barotropic tide–eddy interactions excite internal waves? ⋮ Stratified tidal flow over a tall ridge above and below the turning latitude ⋮ Internal tide generation by arbitrary two-dimensional topography ⋮ Internal wave attractors over random, small-amplitude topography ⋮ Internal wave generation by oscillation of a sphere, with application to internal tides ⋮ Tidally generated internal-wave attractors between double ridges ⋮ Added mass: a complex facet of tidal conversion at finite depth ⋮ Lagrangian coherent structures and internal wave attractors ⋮ Forcing of oceanic mean flows by dissipating internal tides

This page was built for publication: Tidal conversion at a very steep ridge