SIMUG–基于局部笛卡尔坐标的三角形网格上的海冰动力学有限元模型

Pub Date : 2023-06-01 DOI:10.1515/rnam-2023-0012
Sergey S. Petrov, N. Iakovlev
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引用次数: 0

摘要

提出了基于球面局部元的A型和cd型非结构化三角形网格海冰模型SIMUG (sea ice model on Unstructured Grid)的动力学核心。与CICE、FESOM、MITgcm和ICON-O等其他海冰模式相比,模拟线性运动特征(LKFs)的三个标准化箱试验和具有真实大气和海洋强迫的真实北冰洋几何形状的短期预报证明了模式的质量。该模型的显著特点是具有广泛的传输方案选择,以及采用串行和并行c++编码和INMOST、Ani2D和Ani3D软件包处理非结构化网格的新数值实现。进行了代码分析和可伸缩性评估。一般来说,a版本的冰漂移模型工作得更快,但在同一网格上的自由度更少。由于自由度的增加,CD网格上的模型给出了LKFs的超分辨率,但对稳定性的要求更严格。
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SIMUG – finite element model of sea ice dynamics on triangular grid in local Cartesian basis
Abstract The paper presents the dynamical core of the new sea ice model SIMUG (Sea Ice Model on Unstructured Grid) on the A- and CD-types of unstructured triangular grids in the local-element basis on sphere. Three standardized box tests to reproduce the Linear Kinematic Features (LKFs), and the short-term forecast in the real Arctic Ocean geometry with the realistic atmosphere and ocean forcing demonstrate the model quality compared to other sea ice models like CICE, FESOM, MITgcm, and ICON-O. The distinctive features of the model presented are a wide choice of transport schemes, and the new numerical implementation with the serial and parallel C++ coding and INMOST, Ani2D, and Ani3D packages to deal with unstructured grids. Code profiling and scalability assessment are carried out. In general, the A-version of the ice drift model works faster, but has fewer degrees of freedom on the same grid. Due to the increase in the degrees of freedom, the model on the CD grid gives ultra-resolution of LKFs, but requires more strict conditions for stability.
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