潮湿浅水方程的兼容有限元离散化

Nell Hartney, Thomas M. Bendall, Jemma Shipton
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引用次数: 0

摘要

没有湿气物理,传统的浅水方程是大气运动方程的简化形式,因此计算成本低,但保留了大气的许多相关动力学特征。在浅水模式中引入湿度物理,为在简化动力学模式中试验物理-动力学耦合的数值技术提供了工具。在本文中,我们通过将一些不同的潮湿浅水模型写入一般公式来对它们进行比较。一般公式包括三种现有的潮湿浅水方程形式,以及第四种以前未曾探索过的公式。这些方程与三态潮湿物理方案耦合,通过源项与解析流相互作用,产生物理-动力学双向反馈。我们提出了一种新的兼容有限元离散化方程,并在三个测试案例中将其应用于湿润浅水方程的不同公式。结果表明,模型捕捉到了云和雨的生成以及物理-动力的相互作用,并证明了潮湿浅水公式之间的一些差异以及这些不同建模选择的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A compatible finite element discretisation for moist shallow water equations
The moist shallow water equations offer a promising route for advancing understanding of the coupling of physical parametrisations and dynamics in numerical atmospheric models, an issue known as 'physics-dynamics coupling'. Without moist physics, the traditional shallow water equations are a simplified form of the atmospheric equations of motion and so are computationally cheap, but retain many relevant dynamical features of the atmosphere. Introducing physics into the shallow water model in the form of moisture provides a tool to experiment with numerical techniques for physics-dynamics coupling in a simple dynamical model. In this paper, we compare some of the different moist shallow water models by writing them in a general formulation. The general formulation encompasses three existing forms of the moist shallow water equations and also a fourth, previously unexplored formulation. The equations are coupled to a three-state moist physics scheme that interacts with the resolved flow through source terms and produces two-way physics-dynamics feedback. We present a new compatible finite element discretisation of the equations and apply it to the different formulations of the moist shallow water equations in three test cases. The results show that the models capture generation of cloud and rain and physics-dynamics interactions, and demonstrate some differences between moist shallow water formulations and the implications of these different modelling choices.
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