On mass transports generated by tides and long waves

DOI10.1017/S0022112081002693zbMath0463.76032OpenAlexW2119683223MaRDI QIDQ3914629

John M. Huthnance

Publication date: 1981

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/s0022112081002693

zbMATH Keywords

shallow rotating fluidmass transportsanticyclonic mean circulationtides and long waves

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Incompressible inviscid fluids (76B99) Jets and cavities, cavitation, free-streamline theory, water-entry problems, airfoil and hydrofoil theory, sloshing (76B10)

Related Items (max. 100)

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 ⋮ Tidal rectification in lateral viscous boundary layers of a semi-enclosed basin ⋮ 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 ⋮ On the steady mass transport induced by wave motions in a viscous rotating fluid

Cites Work

• Two-dimensional turbulence above topography
• Effects of horizontally two-dimensional bodies on the mass transport near the sea bottom
• On the mean motion induced by internal gravity waves
• Steady currents induced by oscillations round islands
• ON THE THEORETICAL FORM OF OCEAN SWELL. ON A ROTATING EARTH

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