Forcing of oceanic mean flows by dissipating internal tides

DOI10.1017/jfm.2012.303zbMath1275.76060OpenAlexW2114397409MaRDI QIDQ2863320

Oliver Bühler, Nicolas Grisouard

Publication date: 21 November 2013

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

Full work available at URL: https://doi.org/10.1017/jfm.2012.303

zbMATH Keywords

internal wavestopographic effectsocean processes

Mathematics Subject Classification ID

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

Related Items (9)

Boundary streaming by internal waves ⋮ Internal tide generation from non-uniform barotropic body forcing ⋮ Internal wave focusing by a horizontally oscillating torus ⋮ Mean flow generation by three-dimensional nonlinear internal wave beams ⋮ Long-time dynamics of internal wave streaming ⋮ Meridional trapping and zonal propagation of inertial waves in a rotating fluid shell ⋮ The energy flux spectrum of internal waves generated by turbulent convection ⋮ On the interaction of an internal wavepacket with its induced mean flow and the role of streaming ⋮ Interactions of internal tides with a heterogeneous and rotational ocean

Uses Software

• DLMF

Cites Work

• Unnamed Item
• Unnamed Item
• Wave-driven currents and vortex dynamics on barred beaches
• Wave–Vortex Interactions in Fluids and Superfluids
• Dissipative wave-mean interactions and the transport of vorticity or potential vorticity
• Internal tide generation by arbitrary two-dimensional topography
• Waves and Mean Flows
• Tide-topography interactions in a stratified shelf sea I. Basic equations for quasi-nonlinear internal tides
• Tide-topography interactions in a stratified shelf sea II. Bottom trapped internal tides and baroclinic residual currents
• Lee waves in stratified flows with simple harmonic time dependence
• Topographic generation of residual circulation by oscillatory (tidal) currents
• On non-dissipative wave–mean interactions in the atmosphere or oceans
• Tidal conversion at a very steep ridge
• Remote recoil: a new wave–mean interaction effect
• On the vorticity transport due to dissipating or breaking waves in shallow-water flow
• Tidal flow over three-dimensional topography in a stratified fluid
• Instability and focusing of internal tides in the deep ocean
• On the mean motion induced by internal gravity waves

This page was built for publication: Forcing of oceanic mean flows by dissipating internal tides