Prelimenary Modeling for Assessing Tidal Stream Energy Potential at the Alas Strait, Indonesia

M. Mukhtasor, Luli Bangkit Sugito, Sujantoko Sujantoko
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Abstract

This study is on ocean current prelimenary modelling in Alas Strait, Indonesia, to be compared with the field observation data. The model maps coordinate for ocean current so that the potential energy resource can be identified. The model simulation is established with two different scenarios; the first scenario is using windspeed factor and the second without using that factor. Complementary variables such as bathymetry, water elevation, bottom friction, and eddy viscosity have the same value for both scenarios. This ocean current modelling use finite element method with flexible mesh. This method use two dimension numerical solution from the average incompressible Reynolds Navier – Stokes equation with the assumption from Boussinesq dan hydrostatic pressure. This model consists of continuity equation and momentum which closed by turbulen scheme. This study concludes the first scenario is a success and valid with the water surface elevation mean error is 4.2% and water current speed mean error is 10.7%. The second scenario is unseccesful as indicated by the water surface elevation mean error of 13.4% and the water current speed mean error of 11,7%, and also the phase and the trend of current speed is verging the field observation data.
评估印尼阿拉斯海峡潮汐流能量潜力的前期模拟
本研究以印尼阿拉斯海峡的海流初潮模式为研究对象,并与实地观测资料进行比较。该模型绘制海流坐标,从而可以识别潜在的能源资源。建立了两种不同场景下的模型仿真;第一种情况是使用风速因素,第二种情况是不使用风速因素。互补变量,如水深、水面高度、底部摩擦和涡流粘度,在两种情况下具有相同的值。该模型采用柔性网格有限元法对海流进行建模。该方法采用平均不可压缩Reynolds - Navier - Stokes方程的二维数值解,并以Boussinesq和静水压力为假设。该模型由连续方程和动量组成,并由湍流格式封闭。研究结果表明,第一种方案是成功有效的,水面高程平均误差为4.2%,水流速度平均误差为10.7%。第二种情景的水面高程均值误差为13.4%,水流速度均值误差为11.7%,且水流速度的相位和趋势与野外观测数据趋近。
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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