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Vertically nested LES for high-resolution simulation of the surface layer in PALM (version 5.0)

机译:垂直嵌套LES,用于Palm(版本5.0)的表面层的高分辨率模拟

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Large-eddy simulation (LES) has become a well-established tool in the atmospheric boundary layer research community to study turbulence. It allows three-dimensional realizations of the turbulent fields, which large-scale models and most experimental studies cannot yield. To resolve the largest eddies in the mixed layer, a moderate grid resolution in the range of 10 to 100m is often sufficient, and these simulations can be run on a computing cluster with a few hundred processors or even on a workstation for simple configurations. The desired resolution is usually limited by the computational resources. However, to compare with tower measurements of turbulence and exchange fluxes in the surface layer, a much higher resolution is required. In spite of the growth in computational power, a high-resolution LES of the surface layer is often not feasible: to fully resolve the energy-containing eddies near the surface, a grid spacing of O(1m) is required. One way to tackle this problem is to employ a vertical grid nesting technique, in which the surface is simulated at the necessary fine grid resolution, and it is coupled with a standard, coarse, LES that resolves the turbulence in the whole boundary layer. We modified the LES model PALM (Parallelized Large-eddy simulation Model) and implemented a two-way nesting technique, with coupling in both directions between the coarse and the fine grid. The coupling algorithm has to ensure correct boundary conditions for the fine grid. Our nesting algorithm is realized by modifying the standard third-order Runge–Kutta time stepping to allow communication of data between the two grids. The two grids are concurrently advanced in time while ensuring that the sum of resolved and sub-grid-scale kinetic energy is conserved. We design a validation test and show that the temporally averaged profiles from the fine grid agree well compared to the reference simulation with high resolution in the entire domain. The overall performance and scalability of the nesting algorithm is found to be satisfactory. Our nesting results in more than 80% savings in computational power for 5 times higher resolution in each direction in the surface layer.
机译:大型仿真(LES)已成为大气边界层研究界的良好工具,以研究湍流。它允许湍流领域的三维实现,这是大规模模型和大多数实验研究不能产生的。要解决混合层中最大的漩涡,则在10到100米范围内的中等网格分辨率通常足够,并且这些模拟可以在具有几百个处理器的计算集群上运行,甚至可以在工作站上进行简单配置。所需分辨率通常受计算资源的限制。然而,为了与表面层的湍流和交换通量的塔式测量比较,需要更高的分辨率。尽管计算能力的增长,但表面层的高分辨率LES通常是不可行的:为了完全解决表面附近的含能的漩涡,需要O(1M)的网格间隔。解决这个问题的一种方法是采用垂直电网嵌套技术,其中表面以必要的细网分辨率模拟,并且它与标准,粗糙的LES耦合,该标准粗糙的LES可以解析整个边界层中的湍流。我们修改了LES模型手掌(并行化大涡模拟模型)并实现了双向嵌套技术,在粗略和细网格之间的两个方向上耦合。耦合算法必须确保细网格的正确边界条件。通过修改标准的三阶runge-kutta时间踩踏来实现我们的嵌套算法,以允许在两个网格之间通信数据。两种网格在时间上同时提升,同时确保解决的分辨率和子网格级动能的总和是节省的。我们设计验证测试,并表明,与整个域中具有高分辨率的参考仿真相比,来自Fine Grid的时间平均概况很好。发现嵌套算法的整体性能和可扩展性是令人满意的。我们的嵌套在表面层中每个方向上的计算功率节省了80%以上的计算功率,在每个方向上升高了5倍。

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