Steady-state nonlinear internal gravity-wave critical layers satisfying an upper radiation condition

DOI10.1017/S0022112092001757zbMath0775.76018OpenAlexW2130445119WikidataQ60369946 ScholiaQ60369946MaRDI QIDQ3993611

K. G. Lamb, Raymond T. Pierrehumbert

Publication date: 13 August 1992

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

Full work available at URL: https://doi.org/10.1017/s0022112092001757

Mathematics Subject Classification ID

Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15)

Related Items (1)

A steady nonlinear and singular vortex Rossby wave within a rapidly rotating vortex. Part II: Application to geophysical vortices

Cites Work

• Do Rossby-wave critical layers absorb, reflect, or over-reflect?
• On the nonlinear reflexion of a gravity wave at a critical level. Part 1
• On the steady-state relations between disturbances above and below a critical level
• Finite-amplitude waves in inviscid shear flows
• On the nonlinear reflection of a gravity wave at a critical level. Part 2
• The critical layer for internal gravity waves in a shear flow
• A New Class of Nonlinear Waves in Parallel Flows
• The Nonlinear Critical Layer in a Slightly Stratified Shear Flow
• Critical Layers m Parallel Flows

This page was built for publication: Steady-state nonlinear internal gravity-wave critical layers satisfying an upper radiation condition