The effect of dissipative processes on mean flows induced by internal gravity-wave packets

DOI10.1017/S0022112082000792zbMath0488.76027OpenAlexW1968636019MaRDI QIDQ3950166

R. H. J. Grimshaw

Publication date: 1982

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

Full work available at URL: https://doi.org/10.1017/s0022112082000792

zbMATH Keywords

group velocitywave packetdissipative effectsstably stratifiedbounded below by rigid plane boundaryLagrangean-mean formulationpropagating in shear flow

Mathematics Subject Classification ID

Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) Boundary-layer theory, separation and reattachment, higher-order effects (76D10) Internal waves for incompressible inviscid fluids (76B55) Stability and instability of geophysical and astrophysical flows (76E20)

Related Items (1)

Vertical momentum fluxes induced by weakly nonlinear internal waves on the shelf

Cites Work

• A contribution to the theory of viscous damping of stratified wave flows
• Mean motions and impulse of a guided internal gravity wave packet
• Mass transport in the boundary layer at a free oscillating surface
• On the normal modes of parallel flow of inviscid stratified fluid
• The Modulation of an Internal Gravity-Wave Packet, and the Resonance with the Mean Motion
• Progressive internal waves on slopes
• Mass transport in layered fluid systems
• Wave-induced boundary layers in a stratified fluid

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