Abstract
The structure of the Eulerian streaming induced by inertial standing waves over a flat plate perpendicular to the rotating axis is investigated by using the matched asymptotic technique. It is shown that the Eulerian streaming driven by the divergence of the Reynolds stress in the Stokes layer vanishes outside the Stokes and the Ekman layer due to the role of Coriolis force.
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Yamagata, T. Wave-induced boundary layers in a rotating homogeneous fluid. Journal of the Oceanographical Society of Japan 34, 97–104 (1978). https://doi.org/10.1007/BF02109259
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DOI: https://doi.org/10.1007/BF02109259