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首页> 外文期刊>Annales Geophysicae >GUMICS-4 analysis of interplanetary coronal mass ejection impact on Earth during low and typical Mach number solar winds
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GUMICS-4 analysis of interplanetary coronal mass ejection impact on Earth during low and typical Mach number solar winds

机译:GUMICS-4分析低马赫数和典型马赫数太阳风期间行星际日冕物质抛射对地球的影响

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We study the response of the Earth's magnetosphere to fluctuating solar wind conditions during interplanetary coronal mass ejections (ICMEs) using the Grand Unified Magnetosphere-Ionosphere Coupling Simulation (GUMICS-4). The two ICME events occurred on 15-16 July 2012 and 29-30 April 2014. During the strong 2012 event, the solar wind upstream values reached up to 35 particles cm(-3), speeds of up to 694 km s(-1), and an interplanetary magnetic field of up to 22 nT, giving a Mach number of 2.3. The 2014 event was a moderate one, with the corresponding upstream values of 30 particles cm(-3), 320 km s(-1) and 10 nT, indicating a Mach number of 5.8. We examine how the Earth's space environment dynamics evolves during both ICME events from both global and local perspectives, using well-established empirical models and in situ measurements as references. We show that on the large scale, and during moderate driving, the GUMICS-4 results are in good agreement with the reference values. However, the local values, especially during high driving, show more variation: such extreme conditions do not reproduce local measurements made deep inside the magnetosphere. The same appeared to be true when the event was run with another global simulation. The cross-polar cap potential (CPCP) saturation is shown to depend on the Alfven-Mach number of the upstream solar wind. However, care must be taken in interpreting these results, as the CPCP is also sensitive to the simulation resolution.
机译:我们使用大统一磁层-电离层耦合模拟(GUMICS-4)研究了行星际冠状物质抛射(ICME)期间地球磁层对太阳风条件波动的响应。两次ICME事件分别于2012年7月15日至16日和2014年4月29日至30日发生。在2012年强事件期间,太阳风的上游值达到35粒子cm(-3),速度达到694 km s(-1) )和高达22 nT的行星际磁场,马赫数为2.3。 2014年事件为中度事件,相应的上游值为30个粒子cm(-3),320 km s(-1)和10 nT,表明马赫数为5.8。我们以完善的经验模型和现场测量为参考,从全球和地方的角度考察了ICME事件期间地球空间环境动力学的演变。我们显示,在大规模驾驶和中等驾驶过程中,GUMICS-4的结果与参考值非常吻合。但是,局部值(尤其是在高速行驶时)显示出更大的变化:这种极端条件无法重现磁层内部的局部测量值。当事件与另一个全局模拟一起运行时,似乎也是如此。极极帽电位(CPCP)饱和度显示取决于上游太阳风的Alfven-Mach数。但是,在解释这些结果时必须小心,因为CPCP对模拟分辨率也很敏感。

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