Attenuated wave-induced drift in a viscous rotating ocean
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Publication:3701044
DOI10.1017/S0022112083002311zbMath0578.76018OpenAlexW2109553139MaRDI QIDQ3701044
Publication date: 1983
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112083002311
Lagrangian descriptionMean drift currentssecondary mean flowspatially periodic surface wavestime-decaying Stokes driftviscous rotating fluid
Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) General theory of rotating fluids (76U05) Foundations of thermodynamics and heat transfer (80A05)
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Cites Work
- A double boundary-layer model of mass transport in progressive interfacial waves
- Mass transport in the boundary layer at a free oscillating surface
- An exact theory of nonlinear waves on a Lagrangian-mean flow
- Viscous attenuation of mean drift in water waves
- Effects of horizontally two-dimensional bodies on the mass transport near the sea bottom
- ON THE THEORETICAL FORM OF OCEAN SWELL. ON A ROTATING EARTH
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