Modeling a Wave on Mild Sloping Bottom Topography and Its Dispersion Relation Approximation

F. Abdullah, Elvi Syukrina Erianto
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Abstract

Linear wave theory is a simple theory that researchers and engineers often use to study a wave in deep, intermediate, and shallow water regions. Many researchers mostly used it over the horizontal flat seabed, but in actual conditions, sloping seabed always exists, although mild. In this research, we try to model a wave over a mild sloping seabed by linear wave theory and analyze the influence of the seabed’s slope on the solution of the model. The model is constructed from Laplace and Bernoulli equations together with kinematic and dynamic boundary conditions. We used the result of the analytical solution to find the relation between propagation speed, wavelength, and bed slope through the dispersion relation. Because of the difference in fluid dispersive character for each water region, we also determined dispersion relation approximation by modifying the hyperbolic tangent form into hyperbolic sine-cosine and exponential form, then approximated it with Padé approximant. As the final result, exponential form modification with Padé approximant had the best agreement to exact dispersion relation equation then direct hyperbolic tangent form.
缓坡底地形上波浪的模拟及其频散关系逼近
线性波浪理论是一种简单的理论,研究人员和工程师经常使用它来研究深水、中水和浅水区域的波浪。许多研究人员大多将其用于水平平坦的海底,但在实际条件下,倾斜的海底虽然温和,但始终存在。在本研究中,我们尝试用线性波浪理论来模拟缓倾斜海床上的波浪,并分析海床的坡度对模型解的影响。该模型由拉普拉斯方程和伯努利方程以及运动学和动力学边界条件构成。利用解析解的结果,通过色散关系找出传播速度、波长和河床斜率之间的关系。由于各水域的流体色散特性不同,我们还将双曲正切形式修改为双曲正弦余弦和指数形式,确定了色散关系近似,然后用pad近似进行近似。结果表明,指数型修正与精确色散关系方程的拟合性优于直接双曲正切型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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