We consider three-dimensional free-boundary problem on the propagation of incompressible, homogeneous and inviscid fluid with zero surface tension confined in a channel of variable depth. Since for large-scale flows the fluid motion is affected by the rotation of the earth, the model is considered i
Three-dimensional gravity waves in a channel of variable depth
β Scribed by Ranis N. Ibragimov; Dmitry E. Pelinovsky
- Publisher
- Elsevier Science
- Year
- 2008
- Tongue
- English
- Weight
- 194 KB
- Volume
- 13
- Category
- Article
- ISSN
- 1007-5704
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β¦ Synopsis
We consider existence of three-dimensional gravity waves traveling along a channel of variable depth. It is well known that the long-wave small-amplitude expansion for such waves results in the stationary Korteweg-de Vries equation, coefficients of which depend on the transverse topography of the channel. This equation has a single-humped solitary wave localized in the direction of the wave propagation. We show, however, that there exists an infinite set of resonant Fourier modes that travel at the same speed as the solitary wave does. This fact suggests that the solitary wave confined in a channel of variable depth is always surrounded by small-amplitude oscillatory disturbances in the far-field profile.
π SIMILAR VOLUMES
Results are presented from a numerical simulation of three-dimensional Β―ow hydraulics around a mid-channel bar carried out using the FLUENT/UNS computational Β―uid dynamics (CFD) software package. FLUENT/ UNS solves the three-dimensional Reynolds-averaged form of the NavierΒ±Stokes equations. Turbulen