1979
DOI: 10.1007/bf02108281
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Non-hydrostatic Kelvin waves in the ocean

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“…In the range of ω ≤ 1.90 rad/s, we find that the wavenumber k is about one order in magnitude larger than the damping coefficient α [33][34][35][36], meaning that viscous effects are weak for these waves. The dispersion relation for coastal Kelvin wave can be solved in a inviscid two-layer model [37] (also see supplementary materials [32]):…”
mentioning
confidence: 99%
“…In the range of ω ≤ 1.90 rad/s, we find that the wavenumber k is about one order in magnitude larger than the damping coefficient α [33][34][35][36], meaning that viscous effects are weak for these waves. The dispersion relation for coastal Kelvin wave can be solved in a inviscid two-layer model [37] (also see supplementary materials [32]):…”
mentioning
confidence: 99%