A generalized curvilinear solver for spherical shell Rayleigh-Bénard convection

IF 2.8 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Souvik Naskar, Karu Chongsiripinyo, Siddhant Mishra, Anikesh Pal, Akshay Jananan
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引用次数: 0

Abstract

Summary A three-dimensional finite-difference solver has been developed and implemented for Boussinesq convection in a spherical shell. The solver transforms any complex curvilinear domain into an equivalent Cartesian domain using Jacobi transformation and solves the governing equations in the latter. This feature enables the solver to account for the effects of the non-spherical shape of the convective regions of planets and stars. Apart from parallelization using MPI, implicit treatment of the viscous terms using a pipeline alternating direction implicit scheme and HYPRE multigrid accelerator for pressure correction makes the solver efficient for high-fidelity direct numerical simulations. We have performed simulations of Rayleigh-Bénard convection at two Rayleigh numbers Ra = 105 and 107 while keeping the Prandtl number fixed at unity (Pr = 1). The average radial temperature profile and the Nusselt number match very well, both qualitatively and quantitatively, with the existing literature. Closure of the turbulent kinetic energy budget, apart from the relative magnitude of the grid spacing compared to the local Kolmogorov scales, ensures sufficient spatial resolution.
球壳雷利-贝纳德对流的广义曲线求解器
摘要 针对球壳中的布西内斯克对流,开发并实现了一种三维有限差分求解器。该求解器利用雅可比变换将任何复杂的曲线域转换为等效的笛卡尔域,并在后者中求解支配方程。这一功能使求解器能够考虑到行星和恒星对流区域非球形形状的影响。除了使用 MPI 进行并行化之外,还使用管道交替方向隐式方案和用于压力校正的 HYPRE 多网格加速器对粘性项进行隐式处理,从而使求解器能够高效地进行高保真直接数值模拟。我们在两个瑞利数 Ra = 105 和 107 的条件下进行了瑞利-贝纳德对流模拟,同时将普朗特数固定为 1(Pr = 1)。平均径向温度曲线和努塞尔特数在定性和定量方面都与现有文献非常吻合。湍流动能预算的封闭性,除了网格间距相对于局部科尔莫哥罗夫尺度的大小外,还确保了足够的空间分辨率。
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来源期刊
Geophysical Journal International
Geophysical Journal International 地学-地球化学与地球物理
CiteScore
5.40
自引率
10.70%
发文量
436
审稿时长
3.3 months
期刊介绍: Geophysical Journal International publishes top quality research papers, express letters, invited review papers and book reviews on all aspects of theoretical, computational, applied and observational geophysics.
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