4.7 Article

Analytical and numerical investigation of trapped ocean waves along a submerged ridge

期刊

JOURNAL OF FLUID MECHANICS
卷 915, 期 -, 页码 -

出版社

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2020.1039

关键词

topographic effects; shallow water flows; surface gravity waves

资金

  1. National Key Research and Development Program of China [2017YFC1404205]
  2. National Natural Science Foundation of China [52071128, 51579090]
  3. Fundamental Research Funds for the Central Universities [2019B12214]

向作者/读者索取更多资源

This study presents new analytical solutions for trapped waves over a ridge with a hyperbolic-cosine squared cross-sectional profile based on the linear shallow-water equations. The free surface of the trapped waves is described using Legendre functions, and new algebraic equations are derived to depict wave dispersion relationships. The numerical experiments confirm the validity of the new analytical framework for trapped waves over a general type of oceanic ridges.
Based on the linear shallow-water equations, new analytical solutions are derived for trapped waves over a ridge with a hyperbolic-cosine squared cross-sectional profile which may be used to idealize many real-world ocean ridges. In the new analytical formulation, the free surface of the trapped waves is described using the combination of the first and second kinds of the associated Legendre functions, which is further analysed to reveal the existence of both symmetrical and anti-symmetrical trapped waves on the ridge under consideration. New algebraic equations are also derived to depict the wave dispersion relationships, allowing explicit quantification of their sensitivity to the topographic profile. Furthermore, a ray-tracing method is applied to interpret the propagation paths of trapped waves over the ridge and better understand the excitation mechanisms. Finally, an extensively validated Boussinesq wave model is used to conduct numerical experiments for trapped waves induced by tsunamis. The numerical predictions are consistent with the new analytical solutions, which effectively confirms the validity of the new analytical framework for trapped waves over a more general type of oceanic ridges.

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