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FLEXURAL GRAVITY WAVE SCATTERING DUE TO VARIATIONS IN BOTTOM TOPOGRAPHY

机译:底部地形变化引起的弯曲重力波散射

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Oblique flexural gravity wave scattering due to abrupt change in bottom topography is investigated under the assumption of linearized theory of water waves. The problem is studied first for single step in case of finite water depth whose solution is obtained based on the expansion formulae for flexural gravity wavemaker problem and corresponding orthogonal mode-coupling relation. The results for the multiple step topography are obtained from the result of single step using the method of wide-spacing approximation. Energy relation for oblique flexural gravity wave scattering due to change in bottom topography is used to check the accuracy of the computation. Using shallow water approximation the wave scattering due to multiple step topography is derived considering the continuity of mass and energy flux. In this case also the result for single step topography is obtained and then using the wide-spacing approximation the result for multiple steps are derived. Numerical results for reflection and transmission coefficients and deflection of ice sheet are obtained to analyze the effect of multiple step topography on the propagation of flexural gravity waves.
机译:在水波线性化理论的假设下,研究了由于底部地形突变而引起的斜向弯曲重力波的散射。首先研究有限水深情况下的单步问题,该问题的解是根据弯曲重力波发生器问题的展开公式和相应的正交模式耦合关系获得的。多步形貌的结果是使用宽步距近似方法从单步结果中获得的。由于底部地形的变化而引起的斜向弯曲重力波散射的能量关系用于检查计算的准确性。使用浅水近似,考虑到质量和能量通量的连续性,得出了由于多步形貌引起的波散射。在这种情况下,还可以获得单步形貌的结果,然后使用宽步距近似得出多步形的结果。获得了冰盖反射和透射系数以及挠度的数值结果,以分析多步形貌对弯曲重力波传播的影响。

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