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- W2085349071 abstract "First class (inertio-gravity) edge waves in water of finite depth are not trapped at frequencies below a certain critical value. This critical frequency is usually much greater than the Coriolis parameter of the earth's rotation and as a consequence tthe effect of the earth's rotation on these waves is insignificant. The zero order waves (i.e tthose with no nodal lines parallel to the coast) are an important exception. There is no restriction on the frequency of those that travel from left to right for an observer looking out to sea; at high frequency they are first class in cat low fow frequency they are second class (quasi-geostrophic). The zero order waves that travel in the other direction are always first class in character and their cut-off frequency is strongly dependent on the rotation. Higher order second class waves are not greatly affected by the finite depth of the liquid." @default.
- W2085349071 created "2016-06-24" @default.
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- W2085349071 date "1967-02-01" @default.
- W2085349071 modified "2023-10-14" @default.
- W2085349071 title "Edge waves in an ocean of finite depth" @default.
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- W2085349071 doi "https://doi.org/10.1016/0011-7471(67)90030-7" @default.
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