论文标题

部分可观测时空混沌系统的无模型预测

Impact of radial truncation on global 2D hydrodynamic simulations for a Sun-like model

论文作者

Vlaykov, D. G., Baraffe, I., Constantino, T., Goffrey, T., Guillet, T., Saux, A. Le, Morison, A., Pratt, J.

论文摘要

恒星对流是负责热和化学物种运输的非本地过程。通过对流边界处的内部重力波(IGW)激发对流过度旋转和激发,它可能导致加强混合。这些过程之间的关系仍未得到充分理解,需要全球流体动力学模拟来捕获重要的大规模动力学。恒星内部内部的陡峭分层表明,这种模拟的径向范围会影响对流动力学,稳定分层的辐射区域中的IGW和过度旋转层的深度。我们使用使用完全可压缩的恒星流体动力学音乐进行的二维全球模拟研究了这些效果。我们比较了在大约400个对流周转时间中演变的相同太阳样恒星模型的八个不同的径向截断。我们发现,内边界的位置对对流动力学,对流过射和行进的IGW具有无关紧要的影响。我们将其与较低的对流边界处的背景条件相关联,而截断层不受截断的影响,只要在模拟域中包括一个显着的辐射层即可。但是,我们发现,将外边界延伸的恒星半径的几%显着增加了对流区域中IGWS的速度和温度扰动。该效果与外边界处的背景条件有关,这本质上是由静液压分层和给定的发光度确定的。

Stellar convection is a non-local process responsible for the transport of heat and chemical species. It can lead to enhanced mixing through convective overshooting and excitation of internal gravity waves (IGWs) at convective boundaries. The relationship between these processes is still not well understood and requires global hydrodynamic simulations to capture the important large-scale dynamics. The steep stratification in stellar interiors suggests that the radial extent of such simulations can affect the convection dynamics, the IGWs in the stably stratified radiative zone, and the depth of the overshooting layer. We investigate these effects using two-dimensional global simulations performed with the fully compressible stellar hydrodynamics code MUSIC. We compare eight different radial truncations of the same solar-like stellar model evolved over approximately 400 convective turnover times. We find that the location of the inner boundary has an insignificant effect on the convection dynamics, the convective overshooting and the travelling IGWs. We relate this to the background conditions at the lower convective boundary which are unaffected by the truncation, as long as a significantly deep radiative layer is included in the simulation domain. However, we find that extending the outer boundary by only a few percent of the stellar radius significantly increases the velocity and temperature perturbations in the convection zone, the overshooting depth, the power and the spectral slope of the IGWs. The effect is related to the background conditions at the outer boundary, which are determined in essence by the hydrostatic stratification and the given luminosity.

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