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Free Content Double Kelvin waves in a two-layer sea

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It is shown that a depth change such as a fault line acts as a wave guide to long period waves in a two-layer rotating sea, in a similar way to the Double Kelvin waves of Longuet-Higgins (1968a, b) for a homogeneous sea. For a sea with a step discontinuity in depth, the effect of an extra layer leads to only small changes in the dispersion characteristics.

For a continuous monotonic depth change taking place over a width l it is found that as l increases the Double Kelvin wave period increases, and the elevation at the interface decreases relative to the free surface elevation.

Finally the effect of a time periodic wind stress suddenly applied is considered for step discontinuity in depth. For a maximum wind stress of 1 dyne the free surface wave amplitudes of the Double Kelvin wave are significantly less than those given by Mysak (1968). The corresponding interface amplitudes are about 10 cm. It is suggested, unlike their one-layer counterparts, that it may be possible to detect the two-layer waves successfully in practice, since they are predicted to have relatively large elevations at the interface.

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Document Type: Research Article

Publication date: February 1, 1984

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  • The Journal of Marine Research, one of the oldest journals in American marine science, publishes peer-reviewed research articles covering a broad array of topics in physical, biological and chemical oceanography. Articles that deal with processes, as well as those that report significant observations, are welcome. Biological studies involving coupling between ecological and physical processes are preferred over those that report systematics. The editors strive always to serve authors and readers in the academic oceanographic community by publishing papers vital to the marine research in the long and rich tradition of the Sears Foundation for Marine Research. We welcome you to the Journal of Marine Research.
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