A double boundary-layer model of mass transport in progressive interfacial waves

DOI10.1007/BF00052539zbMath0393.76014MaRDI QIDQ1252103

B. D. Dore

Publication date: 1978

Published in: Journal of Engineering Mathematics (Search for Journal in Brave)

zbMATH Keywords

2-Dimensional Gravity WavesAir-Water InterfaceDouble Boundary-Layer ModelHomogeneous FluidsMass TransportProgressive Interfacial WavesStokes Drift Velocity

Mathematics Subject Classification ID

Multiphase and multicomponent flows (76T99) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Boundary-layer theory, separation and reattachment, higher-order effects (76D10)

Related Items

Attenuated wave-induced drift in a viscous rotating ocean ⋮ Observations of transient wave-induced mean drift profiles caused by virtual wave stresses in a two-layer system ⋮ Shear-flow instability due to a wall and a viscosity discontinuity at the interface ⋮ Virtual wave stress and transient mean drift in spatially damped long interfacial waves ⋮ Mass transport induced by standing interfacial waves

Cites Work

• Unnamed Item
• On a differential equation of boundary-layer theory
• Viscous attenuation of mean drift in water waves
• Double boundary layers in standing interfacial waves
• ON MASS TRANSPORT VELOCITY DUE TO PROGRESSIVE WAVES
• Double boundary layers in oscillatory viscous flow
• Oscillatory Viscous Flows. Review and Extension
• Mass transport in layered fluid systems
• Mass transport in water waves

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