Abstract
We study the propagation of water waves over a ridge structured at the subwavelength scale using homogenization techniques able to account for its finite extent. The calculations are conducted in the time domain considering the full three-dimensional problem to capture the effects of the evanescent field in the water channel over the structured ridge and at its boundaries. This provides an effective two-dimensional wave equation which is a classical result but also non-intuitive transmission conditions between the region of the ridge and the surrounding regions of constant immersion depth. Numerical results provide evidence that the scattering properties of a structured ridge can be strongly influenced by the evanescent fields, a fact which is accurately captured by the homogenized model.
| Original language | English |
|---|---|
| Pages (from-to) | 350-376 |
| Number of pages | 27 |
| Journal | Journal of Fluid Mechanics |
| Volume | 871 |
| DOIs | |
| Publication status | Published - 25 Jul 2019 |
Keywords
- shallow water flows
- surface gravity waves
- wave-structure interactions