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Wave transformation by axisymmetric three-dimensional bathymetric anomalies with gradual transitions in depth

机译:深度逐渐过渡的轴对称三维测深异常的波变换

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摘要

The development of an analytic model (Axisymmetric 3-D Step Model) for the propagation of linear water waves over an axisymmetric bathymetric anomaly in arbitrary water depth is presented. The Axisymmetric 3-D Step Model is valid in a region of uniform depth containing an axisymmetric bathymetric anomaly with gradual transitions in depth allowed as a series of steps approximating arbitrary slopes. The velocity potential is calculated by applying matching conditions at the interface between regions of constant depth. The velocity potential obtained determines the wave field in the domain for monochromatic incident waves of linear form. A second analytic model (3-D Shallow Water Exact Model) is developed for comparison within the shallow water limit. The Axisymmetric 3-D Step Model determines the wave transformation caused by the processes of wave refraction, diffraction and reflection. Wave transformation is demonstrated in plots of the relative amplitude for bathymetric anomalies in the form of pit or a shoal, highlighting areas of wave sheltering and wave focusing. Anomalies of constant volume, but variable cross-section are employed to isolate the effect of the transition slope on the wave transformation. Comparisons to a shallow water model, numerical models, and experimental data verify the results of the Axisymmetric 3-D Step Model for several bathymetries including both pits and shoals. Also included are estimates of the energy reflection induced by an axisymmetric depth anomaly. The 3-D Axisymmetric Step Model has been applied previously to account for nearshore transformation (sloping bathymetry) and associated shoreline changes [CJ. Bender, R.G. Dean, Coastal Engineering 51 (2004) 1143].
机译:提出了一种解析模型(轴对称3-D步长模型)的开发,该模型用于在任意水深下在轴对称测深异常上传播线性水波。轴对称3-D阶跃模型在均匀深度的区域中有效,该区域包含轴对称测深异常,深度逐渐过渡为一系列近似任意斜率的台阶。通过在恒定深度的区域之间的界面处应用匹配条件来计算速度势。所获得的速度势确定线性形式的单色入射波在域中的波场。开发了第二种分析模型(3-D浅水精确模型),用于在浅水范围内进行比较。轴对称3-D阶跃模型确定由波的折射,衍射和反射过程引起的波变换。在海深或浅滩形式的测深异常的相对振幅图上显示了波变换,突出了波遮挡和波聚焦的区域。使用恒定体积但横截面可变的异常来隔离过渡斜率对波变换的影响。与浅水模型,数值模型和实验数据的比较验证了轴对称3-D阶跃模型对包括深坑和浅滩在内的多个测深的结果。还包括由轴对称深度异常引起的能量反射的估计。 3-D轴对称步长模型先前已被应用来说明近岸转换(倾斜测深)和相关的海岸线变化[CJ。本德尔院长,《海岸工程》 51(2004)1143]。

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