论文标题

具有质量和能量的垂直图形校正(VIC)方案的全球非静态大气模型

A Global Non-Hydrostatic Atmospheric Model with a Mass and Energy Conserving Vertically-Implicit-Correction (VIC) Scheme

论文作者

Ge, Huazhi, Li, Cheng, Zhang, Xi, Lee, Dongwook

论文摘要

全球非静态大气模型对于研究行星和系外行星的气候变得越来越重要。但是,由于水平和垂直方向之间的较高纵横比,此类模型遭受了计算困难。为了克服这个问题,我们使用垂直图形校正(VIC)方案开发了一个全局模型,在该方案中,积分时间步长不再受垂直声波传播的限制。我们证明了我们的模型,基于$ \ rm athena^{++} $框架及其在行星氛围中的扩展 - 快照(在行星上模拟非静态气氛),严格地保存质量和能量,以有限体积模拟。我们发现,使用VIC方案时,不需要传统的数值稳定器,例如高粘度和差异,这极大地简化了数值实现并提高了稳定性。我们提出的模拟结果范围从1D线性波到有和没有VIC方案的3D全局循环。这些测试表明,我们的配方正确跟踪局部湍流运动,产生kelvin-helmholtz的不稳定性,并在热木星上产生超旋转的射流。与显式模型相比,采用这种VIC方案将全球模拟的计算效率提高了两个以上的数量级,并促进了在区域和全球范围内模拟各种行星大气的能力。

Global non-hydrostatic atmospheric models are becoming increasingly important for studying the climates of planets and exoplanets. However, such models suffer from computational difficulties due to the large aspect ratio between the horizontal and vertical directions. To overcome this problem, we developed a global model using a vertically-implicit-correction (VIC) scheme in which the integration time step is no longer limited by the propagation of acoustic waves in the vertical. We proved that our model, based on the $\rm Athena^{++}$ framework and its extension for planetary atmospheres - SNAP (Simulating Non-hydrostatic Atmosphere on Planets), rigorously conserves mass and energy in finite volume simulations. We found that traditional numerical stabilizers such as hyper-viscosity and divergence damping are not needed when using the VIC scheme, which greatly simplifies the numerical implementation and improves stability. We present simulation results ranging from 1D linear waves to 3D global circulations with and without the VIC scheme. These tests demonstrate that our formulation correctly tracks local turbulent motions, produces Kelvin-Helmholtz instability, and generates a super-rotating jet on hot Jupiters. Employing this VIC scheme improves the computational efficiency of global simulations by more than two orders of magnitude compared to an explicit model and facilitates the capability of simulating a wide range of planetary atmospheres both regionally and globally.

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