PETSc环境下的全并行多网格时间算法研究——以海洋模型为例

L. Carracciuolo, L. D’Amore, Valeria Mele
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引用次数: 8

摘要

我们考虑由进化模型离散化产生的线性系统。通常,求解算法基于时间步进方法,一个时间步接着另一个时间步求解。并行性仅限于空间维度。因为时间本质上是连续的,沿着时间步长同时求解的想法并不直观。在时间方向上实现并行的一种方法是基于多网格约简(MGR)技术的MGRIT算法[7]。这里我们把这种方法称为mri - 1d。另一种方法是时空多重网格,其中时间只是网格中的另一个维度。类似地,我们把这种方法称为mri - 4d。在这项工作中,由于需要最大限度地提高气候科学新算法的可用性,我们提出了一种新的并行方法,该方法混合了mri - 1d思想和经典的空间多网格方法。我们称之为MGR3D+1方法。此外,我们讨论了它们在高性能科学库PETSc中的实现,作为开发更有效和可扩展的海洋模型算法的起点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Toward a fully parallel multigrid in time algorithm in PETSc environment: A case study in ocean models
We consider linear systems that arise from the discretization of evolutionary models. Typically, solution algorithms are based on a time-stepping approach, solving for one time step after the other. Parallelism is limited to the spatial dimension only. Because time is sequential in nature, the idea of simultaneously solving along time steps is not intuitive. One approach to achieve parallelism in time direction is MGRIT algorithm [7], based on multigrid reduction (MGR) techniques. Here we refer to this approach as MGR-1D. Other kind of approach is the space-time multigrid, where time is simply another dimension in the grid. Analougsly, we refer to this approach as MGR-4D. In this work, motivated by the need of maximizing the availability of new algorithms to climate science, we propose a new parallel approach that mixes both the MGR-1D idea and classical space multigrid methods. We refer to it as the MGR3D+1 approach. Moreover, we discuss their implementation in the high performance scientific library PETSc, as starting point to develope more efficient and scalable algorithms in ocean models.
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