论文标题
带有氢离子交换和大规模动力学(SHIELD)模型的太阳风:外动力学的自洽动力学MHD模型
The Solar-wind with Hydrogen Ion Exchange and Large-scale Dynamics (SHIELD) model: A Self-Consistent Kinetic-MHD Model of the Outer Heliosphere
论文作者
论文摘要
已显示中性氢会极大地影响Heliopshere的血浆流量和地球层边界的位置。我们通过氢离子交换和大规模动力学(SHIELD)模型介绍了太阳能的结果,这是一种在空间天气建模框架内的新型,自洽的动力学MHD模型。电荷交换平均自由路径是在地球球的大小上的阶。因此,中性原子不能描述为流体。屏蔽模型将单个等离子体流体的MHD溶液耦合到从系统中中性氢原子的动力学溶液。动力学代码基于自适应网状粒子模拟器(AMP),这是一种用于求解Boltzmann方程的Monte Carlo方法。盾牌模型准确地预测了星际中性的过滤增加到地球圈中。为了验证模型中的正确实现,我们将盾牌模型的结果与其他良好的动力学MHD模型进行比较。盾牌模型与这些研究的中性氢解相匹配,以及与中性氢原子的多流体处理相比,所有地球层边界的变化都与太阳更接近太阳。总体而言,盾牌模型与这些模型显示出极好的一致性,并且对星际氢的流体处理是显着改善。
Neutral hydrogen has been shown to greatly impact the plasma flow in the heliopshere and the location of the heliospheric boundaries. We present the results of the Solar-wind with Hydrogen Ion Exchange and Large-scale Dynamics (SHIELD) model, a new, self-consistent, kinetic-MHD model of the outer heliosphere within the Space Weather Modeling Framework. The charge-exchange mean free path is on order of the size of the heliosphere; therefore, the neutral atoms cannot be described as a fluid. The SHIELD model couples the MHD solution for a single plasma fluid to the kinetic solution from for neutral hydrogen atoms streaming through the system. The kinetic code is based on the Adaptive Mesh Particle Simulator (AMPS), a Monte Carlo method for solving the Boltzmann equation. The SHIELD model accurately predicts the increased filtration of interstellar neutrals into the heliosphere. In order to verify the correct implementation within the model, we compare the results of the SHIELD model to other, well-established kinetic-MHD models. The SHIELD model matches the neutral hydrogen solution of these studies as well as the shift in all heliospheric boundaries closer to the Sun in comparison the the multi-fluid treatment of the neutral hydrogen atoms. Overall the SHIELD model shows excellent agreement to these models and is a significant improvement to the fluid treatment of interstellar hydrogen.