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Minute-scale period oscillations of the magnetosphere

机译:磁层的微小尺度周期振荡

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Oscillations with periods on the order of 5-10min have been observed by instrumented spacecrafts in the Earth's magnetosphere. These oscillations often follow sudden impacts related to coronal mass ejections. It is demonstrated that a simple model is capable of explaining these oscillations and give a scaling law for their basic characteristics in terms of the basic parameters of the problem. The period of the oscillations and their anharmonic nature, in particular, are accounted for. The model has no free adjustable numerical parameters. The results agree well with observations. The analysis is supported by numerical simulations solving the Magneto-Hydro-Dynamic (MHD) equations in two spatial dimensions, where we let a solar wind interact with a magnetic dipole representing a magnetized Earth. We consider two tilt-angles of the magnetic dipole axis. We find the formation of a magnetosheath with the magnetopause at a distance corresponding well to the analytical results. Sudden pulses in the model solar wind sets the model magnetosphere into damped oscillatory motions and quantitatively good agreement with the analytical results is achieved.
机译:地球磁层中的仪器化航天器观测到周期为5-10分钟的振荡。这些振荡通常跟随与冠状物质抛射有关的突然冲击。证明了一个简单的模型能够解释这些振荡,并根据问题的基本参数给出其基本特征的缩放定律。尤其要考虑振荡的周期及其非谐特性。该模型没有自由的可调整数值参数。结果与观察结果非常吻合。数值模拟支持在两个空间维度上求解磁水动力(MHD)方程,其中我们让太阳风与代表磁化地球的磁偶极相互作用,从而为该分析提供了支持。我们考虑了磁偶极子轴的两个倾斜角。我们发现磁石顶的形成与磁石顶的距离与分析结果相当吻合。模型太阳风中的突然脉冲将模型磁层设置为阻尼振荡运动,并且在定量上与分析结果吻合良好。

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