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首页> 外文期刊>Monthly Weather Review >The Spectral Element Atmosphere Model (SEAM): High-Resolution Parallel Computation and Localized Resolution of Regional Dynamics
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The Spectral Element Atmosphere Model (SEAM): High-Resolution Parallel Computation and Localized Resolution of Regional Dynamics

机译:光谱元素大气模型(SEAM):高分辨率的并行计算和区域动力学的局部分辨率

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Fast, accurate computation of geophysical fluid dynamics is often very challenging. This is due to the complexity of the PDEs themselves and their initial and boundary conditions. There are several practical advantages to using a relatively new numerical method, the spectral-element method (SEM), over standard methods. SEM combines spectral-method high accuracy with the geometric flexibility and computational efficiency of finite-element methods. This paper is intended to augment the few descriptions of SEM that aim at audiences besides numerical-methods specialists. Advantages of SEM with regard to flexibility, accuracy, and efficient parallel performance are explained, including sufficient details that readers may estimate the benefit of applying SEM to their own computations. The spectral element atmosphere model (SEAM) is an application of SEM to solving the spherical shallow-water or primitive equations. SEAM simulated decaying Jovian atmospheric shallow-water turbulence up to resolution T1067, producing jets and vortices consistent with Rhines theory. SEAM validates the Held-Suarez primitive equations test case and exhibits excellent parallel performance. At T171L20, SEAM scales up to 292 million floating-point operations per second (Mflops) per processor (29% of supercomputer peak) on 32 Compaq ES40 processors (93% efficiency over using 1 processor), allocating 49 spectral elements/processor. At T533L20, SEAM scales up to 130 billion floating-point operations per second (Gflops) (8% of peak) and 9 wall clock minutes per model day on 1024 IBM POWER3 processors (48% efficiency over 16 processors), allocating 17 spectral elements per processor. Local element-mesh refinement with 300% stretching enables conformally embedding T480 within T53 resolution, inside a region containing 73% of the forcing but 6% of the area. Thereby the authors virtually reproduced a uniform-mesh T363 shallow-water computation, at 94% lower cost.
机译:快速,准确地计算地球物理流体动力学通常非常困难。这是由于PDE本身及其初始条件和边界条件的复杂性。与标准方法相比,使用相对较新的数值方法(光谱元素法(SEM))有许多实际优势。 SEM将光谱方法的高精度与有限元方法的几何灵活性和计算效率结合在一起。本文旨在增加针对SEM的一些针对读者的描述,除了数字方法专家。解释了SEM在灵活性,准确性和高效并行性能方面的优势,其中包括足够的详细信息,读者可以估算将SEM应用于自己的计算的好处。光谱元素大气模型(SEAM)是SEM在求解球形浅水或原始方程式中的应用。 SEAM模拟了衰减至约T1067的Jovian大气浅水湍流,产生了与莱茵河理论一致的射流和涡流。 SEAM验证了Held-Suarez基本方程测试用例,并具有出色的并行性能。在T171L20上,SEAM在32台Compaq ES40处理器上,每处理器每秒可扩展多达2.92亿个浮点运算(Mflops)(超级计算机峰值的29%)(使用1个处理器的效率为93%),每个处理器分配49个频谱元素。在T533L20上,SEAM可在1024个IBM POWER3处理器上扩展至每秒1300亿浮点操作(Gflops)(峰值的8%)和每个模型日9壁钟分钟(在16个处理器上效率为48%),分配了17个频谱元素每个处理器。通过300%拉伸的局部元素网格细化,可以将T480共形嵌入T53分辨率内,即在包含73%的受力但6%的面积的区域内。因此,作者虚拟地再现了均匀网格的T363浅水计算,成本降低了94%。

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