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Oblique wave scattering by undulating porous bottom in a two-layer fluid: Fourier transform approach

机译:通过使两层流体中的多孔底部起伏来进行斜波散射:傅立叶变换方法

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摘要

The problem involving scattering of oblique waves by small undulation on the porous ocean bed in a two-layer fluid is investigated within the framework of linearised theory of water waves where the upper layer is free to the atmosphere. In such a two-layer fluid, there exist waves with two different wave numbers (modes): wave with lower wave number propagates along the free surface whilst that with higher wave number propagates along the interface. When an oblique incident wave of a particular mode encounters the undulating bottom, it gets reflected and transmitted into waves of both modes so that some of the wave energy transferred from one mode to another mode. Perturbation analysis in conjunction with Fourier transform technique is used to derive the first-order corrections of velocity potentials, reflection and transmission coefficients at both modes due to oblique incident waves of both modes. One special type of undulating bottom topography is considered as an example to evaluate the related coefficients in detail. These coefficients are shown in graphical forms to demonstrate the transformation of water wave energy between the two modes. Comparisons between the present results with those in the literature are made for particular cases and the agreements are found to be satisfactory. In addition, energy identity, an important relation in the study of water wave theory, is derived with the help of the Green's integral theorem.
机译:在上层不受大气影响的水波线性化理论框架内,研究了由两层流体中的多孔海床上小波动引起的斜波散射问题。在这样的两层流体中,存在具有两种不同波数(模式)的波:具有低波数的波沿自由表面传播,而具有高波数的波沿界面传播。当特定模式的斜入射波遇到起伏的底部时,它会被反射并传输为两种模式的波,因此某些波能会从一种模式转移到另一种模式。结合傅立叶变换技术的摄动分析被用来导出由于两种模式的倾斜入射波引起的两种模式下的速度势,反射和透射系数的一阶校正。以一种特殊类型的起伏底部地形为例,详细评估了相关系数。这些系数以图形形式显示,以演示两种模式之间水波能量的转换。在特定情况下,将本结果与文献中的结果进行比较,发现协议令人满意。此外,借助格林积分定理,导出了能量同一性,这是水波理论研究中的重要关系。

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