Stratified tidal flow over a tall ridge above and below the turning latitude
From MaRDI portal
Publication:5740075
DOI10.1017/jfm.2016.150zbMath1382.86011OpenAlexW2321779737MaRDI QIDQ5740075
No author found.
Publication date: 8 July 2016
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/jfm.2016.150
Hydrology, hydrography, oceanography (86A05) Internal waves for incompressible inviscid fluids (76B55) Stratification effects in inviscid fluids (76B70)
Related Items
Near-field internal wave beams in two dimensions ⋮ Boundary integrals for oscillating bodies in stratified fluids
Cites Work
- High order one-step monotonicity-preserving schemes for unsteady compressible flow calculations.
- Topographies lacking tidal conversion
- 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
- Analytic Results in (2+1)-Dimensional Finite Temperature LGT
- Tidal conversion at a very steep ridge
- Near-inertial waves in the ocean: beyond the ‘traditional approximation’
- The response of a continuously stratified fluid to an oscillating flow past an obstacle
- Tidal conversion and turbulence at a model ridge: direct and large eddy simulations
- On the trapping of waves along a discontinuity of depth in a rotating ocean
