Abstract
The generation of internal waves by the barotropic tide in a two-layer ocean of variable depth is studied within the framework of the linear theory of long waves in view of the Coriolis force. A barotropic wave climbs at an arbitrary angle to the axis of the extensive ridge with constantly varying profile. The relationships between the amplitudes of the generated internal waves, the location of the ridge, and the angle of climb of the barotropic tide are studied. The analogous research is given in refs 1 and 2.
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References
Dovgaya, S. V. and Cherkesov, L. V. Generation of the inertial waves by a barotropic tide near the oceanic ridge.Mar. Hydrophys. J. (1991)5, 3–8.
Efimov, V. V. (Ed.).Waves in the Ocean's Boundary Areas. Leningrad: Gidrometeoizdat (1984).
Additional information
Translated by Mikhail M. Trufanov. UDK 532.59.
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Dovgaya, S.V., Cherkesov, L.V. The generation of internal waves by the diurnal barotropic tide in the area of extensive irregularity of the bottom topography. Phys. Oceanogr. 4, 339–348 (1993). https://doi.org/10.1007/BF02198497
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DOI: https://doi.org/10.1007/BF02198497