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Propagation of a Fast Magnetoacoustic Shock Wave in the Magnetosphere of an Active Region

机译:快速磁声冲击波在有源区磁层中的传播

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摘要

The propagation of a fast magnetoacoustic shock wave the magnetosphere of a solar active region is considered the nonlinear geometrical acoustics approximation. The magnetic field is modeled as a subphotospheric magnetic dipole embedded in the radial field of the quiet corona. The initial parameters of the wave are specified at a spherical surface in the depths of the active region. The wave propagates asymmetrically and is reflected from regions of the strong magnetic field, which results in the radiation of the wave energy predominantly upwards. Substantial gradients in the Alfvén speed facilitate appreciable growth in the wave intensity. Non-linear damping of the wave and divergence of the wave front lead to the opposite effect. Analysis of the joint action of these factors shows that a fast magnetoacoustic perturbation outgoing from an active region can correspond to a shock wave of moderate intensity. This supports the scenario in which the primary source of the coronal wave is an eruptive filament that impulsively expands in the magnetosphere of an active region.
机译:快速磁声冲击波在太阳活动区域的磁层中的传播被认为是非线性几何声学近似。磁场被建模为嵌入在安静电晕的径向场中的亚光层磁偶极子。波的初始参数在有效区域深度的球形表面上指定。该波不对称传播,并从强磁场区域反射,这导致波能的辐射主要向上传播。 Alfvén速度的实质性梯度促进了波强度的显着增长。波的非线性阻尼和波前的发散导致相反的效果。对这些因素共同作用的分析表明,从活动区域发出的快速磁声扰动可以对应于中等强度的冲击波。这支持了冠状波的主要来源是在活动区域​​的磁层中冲动扩张的喷发丝的情况。

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