Tide-topography interactions in a stratified shelf sea II. Bottom trapped internal tides and baroclinic residual currents

DOI10.1080/03091928908208892zbMath0667.76155OpenAlexW2026236225MaRDI QIDQ3820316

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/10.1080/03091928908208892

zbMATH Keywords

weak dampinglinearly stratified fluidbaroclinic residual currentsgeneration of topographically bounded internal tidesinternal Rossby deformation radiuslimit of small-amplitude topographyquasi-nonlinear 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 (5)

Topographies lacking tidal conversion ⋮ Internal tide generation from non-uniform barotropic body forcing ⋮ Tide-topography interactions in a stratified shelf sea I. Basic equations for quasi-nonlinear internal tides ⋮ Stratified tidal flow over a tall ridge above and below the turning latitude ⋮ Forcing of oceanic mean flows by dissipating internal tides

Cites Work

• Unnamed Item
• A depth-dependent study of the topographic rectification of tidal currents
• On the exact shape of the horizontal profile of a topographically rectified tidal flow
• Tide-topography interactions in a stratified shelf sea I. Basic equations for quasi-nonlinear internal tides
• On mass transports generated by tides and long waves
• Topographic generation of residual circulation by oscillatory (tidal) currents

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