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First-principles modeling of geomagnetically induced electromagnetic fields and currents from upstream solar wind to the surface of the Earth

机译:地磁感应电磁场和从上游太阳风到地球表面的电流的第一性原理建模

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摘要

Our capability to model the near-space physical phenomena has graduallyreached a level enabling module-based first-principles modeling ofgeomagnetically induced electromagnetic fields and currents from upstreamsolar wind to the surface of the Earth. As geomagnetically induced currents(GIC) pose a real threat to the normal operation of long conductor systems onthe ground, such as high-voltage power transmission systems, it is quiteobvious that success in accurate predictive modeling of the phenomenon wouldopen entirely new windows for operational space weather products.Here we introduce a process for obtaining geomagnetically inducedelectromagnetic fields and currents from the output of global magnetosphericMHD codes. We also present metrics that take into account both the complexnature of the signal and possible forecasting applications of the modelingprocess. The modeling process and the metrics are presented with the help ofan actual example space weather event of 24–29 October 2003. Analysis of theevent demonstrates that, despite some significant shortcomings, some centralfeatures of the overall ionospheric current fluctuations associated with GICcan be captured by the modeling process. More specifically, the basicspatiotemporal morphology of the modeled and "measured" GIC is quitesimilar. Furthermore, the presented user-relevant utility metrics demonstratethat MHD-based modeling can outperform simple GIC persistence models.
机译:我们对近空间物理现象进行建模的能力已逐步达到一种水平,从而能够基于模块的第一原理对地磁感应电磁场和从上游太阳风到地球表面的电流进行建模。由于地磁感应电流(GIC)对地面上的长导体系统(例如高压输电系统)的正常运行构成了真正的威胁,因此很明显,成功地对该现象进行准确的预测建模将为操作空间打开全新的窗口天气产品。在这里,我们介绍一种从全球磁层MHD代码的输出中获取地磁感应的电磁场和电流的过程。我们还提出了既考虑信号复杂度又考虑建模过程可能的预测应用的指标。借助2003年10月24日至29日的实际示例空间天气事件介绍了建模过程和度量。对事件的分析表明,尽管存在一些重大缺陷,但GIC可以捕获与GIC相关的整体电离层电流波动的一些中心特征。建模过程。更具体地说,建模和“测量”的GIC的基本时空形态非常相似。此外,所提出的与用户相关的效用指标表明,基于MHD的建模可以胜过简单的GIC持久性模型。

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