A depth-dependent study of the topographic rectification of tidal currents

DOI10.1080/03091928508219269zbMath0583.76118OpenAlexW2169007543WikidataQ114640471 ScholiaQ114640471MaRDI QIDQ3706763

Daniel G. Wright, John W. Loder

Publication date: 1985

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

Full work available at URL: https://doi.org/10.1080/03091928508219269

zbMATH Keywords

tidal currentshomogeneous rotating fluidfrictional parametersbottom stress lawconstant stress layerdeapth-dependent modeldepth-dependent solutioninteraction of mean and tidal currentsisobathsmean Lagrangian velocityrectified mean flowtopographic rectificationvertically-uniform, time-independent vertical eddy viscosityweak frictionzero depth-averaged mean flow

Mathematics Subject Classification ID

Multiphase and multicomponent flows (76T99) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Basic methods in fluid mechanics (76M99)

Related Items (3)

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 ⋮ Instabilities of the flow around a cylinder and emission of vortex dipoles

Cites Work

• Unnamed Item
• On mass transports generated by tides and long waves
• Topographic generation of residual circulation by oscillatory (tidal) currents
• Mass transport in water waves

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