Forcing of oceanic mean flows by dissipating internal tides
From MaRDI portal
Publication:2863320
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
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
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