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首页> 外文期刊>Geophysical Research Letters >Particle entry into the inner magnetosphere during duskward IMF B-y: Global three-dimensional electromagnetic full particle simulations
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Particle entry into the inner magnetosphere during duskward IMF B-y: Global three-dimensional electromagnetic full particle simulations

机译:在IMF B-y黄昏期间粒子进入内部磁层:全局三维电磁全粒子模拟

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摘要

The change of the interplanetary magnetic field ( IMF) direction from northward to duskward has an important impact on the inner magnetosphere. This impact is analyzed with the help of a new parallel version of the global three-dimensional full particle simulation code. For northward IMF, bands of weak magnetic field ( sash) form poleward of the cusp at high latitudes in each hemisphere. These sashes move to the equator ( within opposite quadrants) as the IMF rotates duskward and merge into one another to form the characteristic "Crosstail-S'' within the neutral sheet of the magnetotail. These macroscopic magnetic patterns ( sashes and Crosstail-S) evidenced herein are in a good agreement with results of previous 3D MHD simulations and experimental observations. Moreover, the analysis of particle fluxes shows that "sashes'' and "Crosstail-S'' act as magnetic groove to facilitate the entry and injection of magnetosheath particles into the inner magnetosphere. Injected particles are accelerated after the IMF changes its direction from northward to duskward.
机译:行星际磁场(IMF)方向从北向黄昏变化对内部磁层具有重要影响。在全局三维三维全粒子模拟代码的新并行版本的帮助下分析了这种影响。对于北向IMF,在每个半球的高纬度处,弱磁场(窗扇)带在尖端处形成极点。当IMF黄昏旋转时,这些窗扇移至赤道(在相对的象限内)并彼此融合,从而在磁尾的中性片内形成特征性的“ Crosstail-S”。这些宏观的磁模式(窗扇和Crosstail-S)此处的证据与先前的3D MHD模拟结果和实验观察结果非常吻合,而且,对粒子通量的分析表明,“窗扇”和“ Crosstail-S”充当磁槽,有助于磁石的进入和注入。粒子进入内部磁层后,IMF的方向从北变到黄昏后,注入的粒子就会加速。

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