p-csi v1.0, an accelerated barotropic solver for the high-resolution ocean model component in the community earth system model v2.0

Clicks: 112
ID: 203960
2016
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Abstract
In the Community Earth System Model (CESM), the ocean model is computationally expensive for high-resolution grids and is often the least scalable component for high-resolution production experiments. The major bottleneck is that the barotropic solver scales poorly at high core counts. We design a new barotropic solver to accelerate the high-resolution ocean simulation. The novel solver adopts a Chebyshev-type iterative method to reduce the global communication cost in conjunction with an effective block preconditioner to further reduce the iterations. The algorithm and its computational complexity are theoretically analyzed and compared with other existing methods. We confirm the significant reduction of the global communication time with a competitive convergence rate using a series of idealized tests. Numerical experiments using the CESM 0.1° global ocean model show that the proposed approach results in a factor of 1.7 speed-up over the original method with no loss of accuracy, achieving 10.5 simulated years per wall-clock day on 16 875 cores.
Reference Key
huang2016geoscientificp-csi Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;X. Huang;X. Huang;Q. Tang;Y. Tseng;Y. Hu;A. H. Baker;F. O. Bryan;J. Dennis;H. Fu;G. Yang
Journal international journal of quantum chemistry
Year 2016
DOI
10.5194/gmd-9-4209-2016
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