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Simulating Water and Sediment Flow Using SWE-Convection Diffusion Model on OpenMP Platform

机译:在OpenMP平台上使用SWE - 对流扩散模型模拟水和沉积物流量

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In this paper, 1D SWE - convection reaction diffusion using semi implicit staggered scheme for approximating underwater landslide has been done. The numerical results is shown close enough to the experiment data by Centre National du Machinisme Agricole du Génie Rural des Eaux et des Forêts (CEMEGREF) laboratory, on December 1994. Here, two scenarios using different parameters in convection diffusion equation are elaborated. Using sediment speed 0.25 and diffusion coefficient of sediment 0.005, the water and sediment error are observed 0.49 and 0.507 respectively at time t = 0.4. Moreover, in this paper, the parallel computing using OpenMP platform is elaborated in the simulation. As the result, computer I with AMD Rayzen(TM) 2400 has the best result for speedup and efficiency with 3.602396 times and 90.0599 % when the final time at t = 0.8s and Nx = 6400 points.
机译:在本文中,已经完成了使用半隐式交错方案的1D - 对流反应扩散,用于近似水下滑坡。数值结果如1994年12月,由中心国家du Machinisme Agricole DuGénieury(Cemegref)实验室的实验数据所示。这里,详细说明了使用对流扩散方程中使用不同参数的两个场景。使用沉积物速度0.25和沉积物的扩散系数0.005,在时间t = 0.4分别观察到0.49和0.507的水和沉积物误差。此外,在本文中,在模拟中详细阐述了使用OpenMP平台的并行计算。结果,带有AMD Rayzen(TM)2400的计算机I具有最佳的加速和效率,在T = 0.8s和n的最后一次时,快速和效率的加速和效率为3.602396倍和90.0599% x = 6400点。

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