A Method to Reduce the Calculation Time of Sediment Simulation by Controlling the Number of Long-term Wave Data

Gweon-su Kim, Ha-sang Ryu, Sanghuk Kim
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Abstract

In order to solve the difficulty of performing a numerical model using a long-term wave time series, a method of reducing wave time series was considered. And Numerical simulation of the sediment by the Delft3d model at the Maengbang Beach was conducted to verify the validity of the method. NOAA wave data were collected for about 40 years from January 1979 to May 2019. Among them, waves, which are judged to have insignificant effect on the beach, were removed and the wave time series was reduced. To this end, the entire wave time series was graded at intervals of 0.5m, period 2sec, and wave direction 10° to generate a total of 749 representative waves, and a numerical simulation of sediment was performed for each representative wave for 1 day. When the maximum sediment height was less than 0.01m/day, it was assumed that the influence of the representative wave on the area was negligible. As a result of conducting numerical simulation of the sediment using the 23-month real-time waves and the wave by the reduced time series, the difference between the two simulation results indicates a local sedimentation difference of 0.1 to 0.5 m near Deokbongsan. There is a difference in sedimentation of 0.01 to 0.1m overall, and the pattern of repeated erosion and sedimentation along the entire coast is very similar to both real-time waves and reduced time series waves.
一种通过控制长期波浪数据数来缩短泥沙模拟计算时间的方法
为了解决利用长时波时间序列进行数值模拟的困难,提出了一种对长时波时间序列进行简化的方法。并利用Delft3d模型对孟邦滩涂沉积物进行了数值模拟,验证了该方法的有效性。NOAA收集了1979年1月至2019年5月约40年的波浪数据。其中,去除被认为对海滩影响不显著的波浪,对波浪时间序列进行约简。为此,将整个波浪时间序列以0.5m间隔、2sec周期、波浪方向为10°进行分级,共生成749个代表波,并对每个代表波进行1 d的泥沙数值模拟。当最大泥沙高度小于0.01m/d时,假设代表波对面积的影响可以忽略不计。利用23个月的实时波浪和简化时间序列的波浪进行泥沙数值模拟的结果表明,德峰山附近的局部泥沙差异为0.1 ~ 0.5 m。整体沉积差异为0.01 ~ 0.1m,整个海岸的反复侵蚀和沉积模式与实时波和简化时间序列波都非常相似。
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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