Tide-topography interactions in a stratified shelf sea I. Basic equations for quasi-nonlinear internal tides

DOI10.1080/03091928908208891zbMath0667.76154OpenAlexW2089653024MaRDI QIDQ3820315

Leo R. M. Maas, J. T. F. Zimmerman

Publication date: 1989

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091928908208891

zbMATH Keywords

shallow water equationsmultiple-scale analysisnormal modesmodal dampingfree modessmall-amplitude topographyquasi-nonlinear advectionstratified shelf seatide-topography interactionuniformly rotating, stratified fluid, subject to a time-periodic advection

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Reaction effects in flows (76V05)

Related Items (4)

Rectified flow of a rotating fluid along a vertical sidewall ⋮ Tide-topography interactions in a stratified shelf sea II. Bottom trapped internal tides and baroclinic residual currents ⋮ Stratified tidal flow over a tall ridge above and below the turning latitude ⋮ Forcing of oceanic mean flows by dissipating internal tides

Cites Work

• On the exact shape of the horizontal profile of a topographically rectified tidal flow
• Tide-topography interactions in a stratified shelf sea II. Bottom trapped internal tides and baroclinic residual currents
• On mass transports generated by tides and long waves
• Lee waves in stratified flows with simple harmonic time dependence
• The generation of internal tides over steep continental slopes
• On topographic generation and coupling of internal waves
• Topographic generation of residual circulation by oscillatory (tidal) currents
• The vertical structure of tidal currents

This page was built for publication: Tide-topography interactions in a stratified shelf sea I. Basic equations for quasi-nonlinear internal tides