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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Modeling extreme “Carrington-type” space weather events using three-dimensional global MHD simulations
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Modeling extreme “Carrington-type” space weather events using three-dimensional global MHD simulations

机译:使用三维全球MHD模拟为极端“卡灵顿型”太空天气事件建模

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摘要

There is a growing concern over possible severe societal consequences related to adverse space weather impacts on man-made technological infrastructure. In the last two decades, significant progress has been made toward the first-principles modeling of space weather events, and three-dimensional (3-D) global magnetohydrodynamics (MHD) models have been at the forefront of this transition, thereby playing a critical role in advancing our understanding of space weather. However, the modeling of extreme space weather events is still a major challenge even for the modern global MHD models. In this study, we introduce a specially adapted University of Michigan 3-D global MHD model for simulating extreme space weather events with a Dst footprint comparable to the Carrington superstorm of September 1859 based on the estimate by Tsurutani et. al., (2003). Results are presented for a simulation run with “very extreme” constructed/idealized solar wind boundary conditions driving the magnetosphere. In particular, we describe the reaction of the magnetosphere-ionosphere system and the associated induced geoelectric field on the ground to such extreme driving conditions. The model setup is further tested using input data for an observed space weather event of Halloween storm October 2003 to verify the MHD model consistence and to draw additional guidance for future work. This extreme space weather MHD model setup is designed specifically for practical application to the modeling of extreme geomagnetically induced electric fields, which can drive large currents in ground-based conductor systems such as power transmission grids. Therefore, our ultimate goal is to explore the level of geoelectric fields that can be induced from an assumed storm of the reported magnitude, i.e., Dst ~= ?1600 nT.
机译:人们越来越担心与不利的太空天气对人造技术基础设施的影响有关的严重社会后果。在过去的二十年中,在空间天气事件的第一性原理建模方面已经取得了重大进展,而三维(3-D)全球磁流体动力学(MHD)模型一直处于这一过渡的前沿,因此发挥了至关重要的作用在增进我们对太空天气的理解方面的作用。但是,即使对于现代全球MHD模型,极端空间天气事件的建模仍然是一个重大挑战。在本研究中,我们根据Tsurutani等人的估计,介绍了一种经过特殊调整的密歇根大学3D全球MHD模型,用于模拟Dst足迹与1859年9月的卡灵顿超级风暴相当的极端太空天气事件。等人,(2003)。给出了在“非常极端”构造/理想化太阳风边界条件驱动磁层的模拟运行中得出的结果。特别是,我们描述了磁层-电离层系统和地面上相关的感应地电场对这种极端行驶条件的反应。使用输入数据对观察到的2003年10月万圣节风暴的太空天气事件进行进一步测试,以验证MHD模型的一致性并为以后的工作提供更多指导。这种极端空间天气MHD模型设置是专门为实际应用而设计的,用于对极端地磁感应电场的建模,该电场可以在诸如输电网格之类的地面导体系统中驱动大电流。因此,我们的最终目标是探索假定的报告风暴幅度,即Dst〜=?1600 nT,可以诱发的地电场水平。

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