Finite-amplitude topographic Rossby waves in a channel
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Publication:3536187
DOI10.1063/1.869906zbMath1147.76364OpenAlexW1994369291MaRDI QIDQ3536187
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Publication date: 17 November 2008
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.869906
Related Items (3)
Component-based formal modeling of PLC systems ⋮ Coastal outflow currents into a buoyant layer of arbitrary depth ⋮ Numerical simulation of wave propagation along a discontinuity in depth in a rotating annulus
Cites Work
- A simple model of Rossby-wave hydraulic behaviour
- The low-frequency scattering of Kelvin waves by stepped topography
- Dynamics of vorticity fronts
- The structure of organized vortices in a free shear layer
- The touching pair of equal and opposite uniform vortices
- The topographic control of planetary-scale flow
- A numerical and theoretical study of certain nonlinear wave phenomena
- Maintenance of continental boundary-layer shear through counter-gradient vorticity flux in a barotropic model
- Topographically forced long waves on a sheared coastal current. Part 1. The weakly nonlinear response
- Low-frequency scattering of Kelvin waves by continuous topography
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