Lagrangian drift in a permeable bottom layer induced by internal gravity waves
The mean drift in a permeable homogeneous bottom layer caused by internal gravity waves in an overlying stratified fluid, is investigated theoretically. We apply a Lagrangian formulation, together with the long-wave approximation, for the motion in the fluid and the fluid-saturated permeable layer....
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Formato: | article |
Lenguaje: | EN |
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Taylor & Francis Group
2021
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Acceso en línea: | https://doaj.org/article/b71b4af4e4834205951b0b0d9a6f3b0c |
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