Abstract
The strongly nonlinear Miyata-Choi-Camassa model, a two-layer internal-wave model that includes the free-surface effect (MCC-FS model), has shown excellent performance on simulating large-amplitude internal waves. In this study, we are interested in assessing whether the MCC-FS model can be applied to study problems involving surface waves, and how the model performs. For this purpose, we apply the two-layer MCC-FS model to a time-varying bottom to simulate surface water-waves by setting the same densities of the upper- and lower-fluid layers. Although densities of the upper and lower fluid layers are the same, it is found that the depth ratio of the two layers plays a remarkable role in the solution. By analyzing the linear dispersion relations of the MCC-FS model with three different depth ratios (h1/h2 = 1/9, 3/7 and 5/5, where h1 and h2 are the depths of the upper- and lower-fluid layers, respectively), we determine that the MCC-FS model with the depth ratio 3/7 has the better performance on simulating surface water waves. Under this configuration, we apply the MCC-FS model to simulate the surface solitary waves on a flat bottom and the surface water-waves generated by a bottom disturbance. By comparing with the laboratory measurements, the accuracy of the results provided by the MCC-FS model is validated.
Original language | English |
---|---|
Pages (from-to) | 725-741 |
Number of pages | 17 |
Journal | Ocean Dynamics |
DOIs | |
Publication status | Published - 25 Jul 2024 |
Keywords
- MCC-FS model
- time-varying bottom
- solitary wave
- bottom disturbance