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Computational properties of a new horizontal staggered grid

机译:新的水平交错网格的计算属性

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This paper presents a new horizontal staggered grid (LE grid), which defines h at a gridpoint, and both u and v at the same mid-gridpoint along the x and y directions. A general method is used to deduce the dispersion relationships of describing inertia gravity waves on LE grid and Arakawa A-E grids, which are then compared with the analytical solution (AS) in resolved or under-resolved cases, using two-order central difference or four-order compact difference scheme from the frequency and group velocity. Results show that in both resolved and under-resolved cases, no matter whether two-order central difference or four-order compact difference scheme is used, the frequency and group velocity discrete errors on LE grid in describing inertia gravity waves are smaller than those of Arakawa A-E grids. At the same time, it is only on LE or Arakawa grid C that the employment of a compact difference scheme of higher difference precision can improve their accuracy in describing inertia gravity waves. However, as for the other four grids (Arakawa A,B,D and E), when the difference precision increases, the accuracy of simulating inertia gravity waves decreases.
机译:本文提出了一个新的水平交错网格(LE网格),它定义了一个网格点处的h,并且u和v都沿着x和y方向位于同一中间网格点。使用通用方法推导描述LE网格和Arakawa AE网格上的惯性重力波的色散关系,然后使用二阶中心差或四阶与解决方案或欠解决方案的分析解决方案(AS)进行比较频率和群速度的二阶紧致差分方案。结果表明,无论是求解还是未求解,无论采用二阶中心差分还是四阶紧致差分方案,在描述惯性重力波时,LE网格上的频率和群速度离散误差都小于荒川AE网格。同时,只有在LE或Arakawa网格C上,采用更高差分精度的紧凑差分方案才能提高其描述惯性重力波的准确性。但是,对于其他四个栅格(荒川A,B,D和E),当差值精度增加时,模拟惯性重力波的精度会降低。

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