A simplified Fourier method for computing the internal wavefield generated by an oscillating source in a horizontally moving, depth-dependent background
From MaRDI portal
Publication:3554650
DOI10.1063/1.1785140zbMath1187.76068OpenAlexW1964480389MaRDI QIDQ3554650
James W. Rottman, Dave Broutman
Publication date: 22 April 2010
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.1785140
Fourier transformseigenvalues and eigenfunctionsray tracingfluid oscillationsstratified flowsurface waves (fluid)
Related Items (4)
Beyond ray tracing for internal waves. I. Small-amplitude anelastic waves ⋮ Synthetic aperture radar image simulation of the internal waves excited by a submerged object in a stratified ocean ⋮ Analytic properties of solutions to the equation of internal gravity waves with flows for critical modes of wave generation ⋮ A WKB derivation for internal waves generated by a horizontally moving body in a thermocline
Cites Work
- Studies on Magneto-Hydrodynamic Waves and other Anisotropic wave motions
- Surface effects of vertically propagating gravity waves in a stratified fluid
- Internal waves generated by a translating oscillating body
- Internal wave generation in uniformly stratified fluids. Part 2. Moving point sources
- Limit states of internal wave beams
- The Maslov integral representation of slowly varying dispersive wavetrains in inhomogeneous moving media.
This page was built for publication: A simplified Fourier method for computing the internal wavefield generated by an oscillating source in a horizontally moving, depth-dependent background
