Kelvin wave

A Kelvin wave is a wave in the ocean, a large lake or the atmosphere that balances the Earth's Coriolis force against a topographic boundary such as a coastline, or a waveguide such as the equator. A feature of a Kelvin wave is that it is non-dispersive, i.e., the phase speed of the wave crests is equal to the group speed of the wave energy for all frequencies. This means that it retains its shape as it moves in the alongshore direction over time.

A Kelvin wave (fluid dynamics) is also a long scale perturbation mode of a vortex in superfluid dynamics; in terms of the meteorological or oceanographical derivation, one may assume that the meridional velocity component vanishes (i.e. there is no flow in the north–south direction, thus making the momentum and continuity equations much simpler). This wave is named after the discoverer, Lord Kelvin (1879).^[1]^[2]

^ Thomson, W. (Lord Kelvin) (1879), "On gravitational oscillations of rotating water", Proc. R. Soc. Edinburgh, 10: 92–100, doi:10.1017/S0370164600043467
^ Gill, Adrian E. (1982), Atmosphere–ocean dynamics, International Geophysics Series, vol. 30, Academic Press, pp. 378–380, ISBN 978-0-12-283522-3

[1] Thomson, W. (Lord Kelvin) (1879), "On gravitational oscillations of rotating water", Proc. R. Soc. Edinburgh, 10: 92–100, doi:10.1017/S0370164600043467

[2] Gill, Adrian E. (1982), Atmosphere–ocean dynamics, International Geophysics Series, vol. 30, Academic Press, pp. 378–380, ISBN 978-0-12-283522-3

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