Numerical Simulation for One-Dimensional (1D) Wave Propagation by Solving the Shallow Water Equations using the Preissmann Implicit Scheme

Prilla Lidyana, B. Ginting, D. Yudianto
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引用次数: 1

Abstract

This research simulated one-dimensional wave propagation by solving the shallow water equations using the Preissman implicit numerical scheme due to its ability to maintain simplicity and stability at a larger time step value. This numerical model was fundamentally developed to satisfy the shallow water condition, where the water depth or horizontal-length scale is much smaller than the free-surface disturbance wavelength or vertical-length scale, and to comprehensively test the accuracy of the model. Consequently, three different types of waves were considered and these include (1) tidal, (2) roll, and (3) solitary. In the first case, the model was proven to be robust and accurate due to its relatively-small errors for both water-surface elevation and velocity indicating that the Preismann scheme is suitable for longwave simulations. In the second case, it was fairly accurate in capturing the periodic permanent roll waves despite showing a higher water-surface elevation than the one observed and this discrepancy is due to the neglect of the turbulent Reynold stress in the model. Meanwhile, the last case showed remarkable discrepancies in the water-surface elevation because the dispersion effect is quite significant during the wave propagation. This indicates that the Preismann scheme underestimated the wave crest along with time when the dispersion term was neglected. All simulations were performed using the tridiagonal matrix algorithm, thereby eliminating the need for iterations for the solution of the Preismann scheme. The findings of this study are beneficial to the next generation of the Preissmann-scheme models which can be designed to include turbulence and dispersion terms.
用Preissmann隐式格式求解浅水方程的一维波传播数值模拟
由于Preissman隐式数值格式在较大时阶值下保持简单性和稳定性,本研究采用Preissman隐式数值格式求解浅水方程组,模拟一维波的传播。该数值模型从根本上是为了满足水深或水平长度尺度远小于自由水面扰动波长或垂直长度尺度的浅水条件,并综合检验模型的准确性。因此,我们考虑了三种不同类型的波浪,包括(1)潮汐,(2)翻滚和(3)孤立。在第一种情况下,模型对水面高程和速度的误差较小,证明了模型的鲁棒性和准确性,表明Preismann格式适用于长波模拟。在第二种情况下,尽管显示的水面高度比观测到的高,但它在捕获周期性永久滚动波方面相当准确,这种差异是由于模型中忽略了湍流雷诺应力。最后一种情况由于波在传播过程中弥散效应非常显著,导致水面高程差异显著。这表明当忽略色散项时,Preismann格式低估了波峰随时间的变化。所有模拟均采用三对角矩阵算法进行,从而消除了求解Preismann格式的迭代。本研究的发现有助于下一代preissmann格式模型的设计,这些模型可以包含湍流和色散项。
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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15 weeks
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