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....
| 出版年: | Tellus: Series A, Dynamic Meteorology and Oceanography |
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| 第一著者: | |
| フォーマット: | 論文 |
| 言語: | 英語 |
| 出版事項: |
Stockholm University Press
2021-01-01
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| 主題: | |
| オンライン･アクセス: | http://dx.doi.org/10.1080/16000870.2021.1877461 |