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A semi-implicit non-hydrostatic dynamical kernel using finite elements

机译:使用有限元的半隐式非静液压动力学核

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This work is a first step in the direction of implementing a high-order finite-element discretization in the vertical in the non-hydrostatic version of the HARMONIE model. The present dynamical core of the HARMONIE model is shared with the ECMWF and the ALADIN models and uses a horizontal spectral discretization and a semi-implicit semi-Lagrangian time stepping scheme, all of which are maintained in this work. Trying to implement a finite-element discretization in the non-hydrostatic version of the HARMONIE model has been found to be very difficult due to the set of prognostic variables used and the mass-based vertical coordinate. A different set of prognostic variables and a hybrid vertical coordinate based on height are tested here on a vertical slice non-hydrostatic kernel. A stability analysis of the linear model has been done. To evaluate the model stability and accuracy, a set of test cases from the literature are presented in the linear and nonlinear regimes, with and without orography. An iterative centred-implicit scheme can be applied to avoid instability related to steep orography, although this reduces the efficiency of the model. The novel aspects with respect to existing non-hydrostatic model kernels are the use of cubic finite elements in the vertical discretization, the use of a height-based vertical coordinate in conjunction with a spectral discretization in the horizontal, and the coordinate-independent formulation of each element of the model including the semi-Lagrangian advection. Copyright (c) 2011 Royal Meteorological Society
机译:这项工作是在非静水模型的HARMONIE模型的垂直方向上实现高阶有限元离散化的第一步。 HARMONIE模型的当前动力学核心与ECMWF和ALADIN模型共享,并使用水平频谱离散化和半隐式半拉格朗日时间步长方案,所有这些工作均在此工作中得以保留。由于使用了一组预后变量和基于质量的垂直坐标,在HARMONIE模型的非静液压版本中尝试实现有限元离散化非常困难。在垂直切片非静水内核上测试了一组不同的预后变量和基于高度的混合垂直坐标。线性模型的稳定性分析已经完成。为了评估模型的稳定性和准确性,在线性和非线性状态下(无论有无地形),都提供了一组来自文献的测试案例。可以应用迭代中心隐式方案来避免与陡峭地形有关的不稳定性,尽管这会降低模型的效率。关于现有的非静水模型内核的新颖方面是在垂直离散化中使用立方有限元,在水平方向使用基于高度的垂直坐标以及频谱离散化以及与坐标无关的公式化模型的每个元素都包括半拉格朗日对流。版权所有(c)2011皇家气象学会

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