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Ground magnetic perturbations associated with the standing toroidal mode oscillations in the magnetosphere-ionosphere system

机译:与磁层-电离层系统中站立的环形模式振荡相关的地磁扰动

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The behavior of toroidal mode oscillations of standing Alfvén waves (refer to as standing Alfvén oscillations) in the coupled magnetosphere-ionosphere system is investigated using a trapezoid-shape magnetosphere model. It is found that the magnetic perturbation is transmitted across the ionosphere differently in the two cases where the ionospheric electric field perturbation is static (Pedersen conductivity > Hall conductivity) and where it is inductive (Pedersen conductivity < Hall conductivity). It is noted that the ionospheric Hall current for the inductive condition shields the magnetic field perturbation. The north-south asymmetry of the conjugate ground magnetic perturbations is calculated by using a trapezoid model with the ionospheric and magnetospheric parameters based on the IGRF and IRI. It is revealed that the ionospheric electric field is almost static for the fundamental mode oscillation, whereas inductive for the higher harmonic ones. It is also found that the north-south asymmetry of the ground magnetic perturbations depends not only on the L-value but also on magnetic longitude; this is because the ionosphere and magnetic field conditions are not uniform as a function of longitude.
机译:使用梯形磁层模型研究了耦合磁层-电离层系统中驻Alfvén波的环形模式振荡(称为驻Alfvén振荡)的行为。发现在电离层电场扰动是静态(皮德森电导率>霍尔电导率)和电感应层电场感应(皮德森电导率<霍尔电导率)的两种情况下,磁扰动在电离层中的传播方式不同。注意,感应条件下的电离层霍尔电流屏蔽了磁场的扰动。通过使用具有基于IGRF和IRI的电离层和磁层参数的梯形模型,计算共轭地面磁扰动的南北不对称性。结果表明,电离层电场对于基模振荡几乎是静态的,而对于高次谐波则是感应性的。还发现,地面磁扰动的南北不对称不仅取决于L值,而且还取决于磁经度。这是因为电离层和磁场条件随经度的变化而不一致。

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