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A global MHD simulation of the Jovian magnetosphere interacting with/without the interplanetary magnetic field

机译:行星磁场与/不存在行星际磁场相互作用的全球MHD模拟

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摘要

A global model of the Jovian magnetosphere is presented based on magnetohydrodynamic (MHD) simulation that takes into account the interaction between a rapidly rotating magnetosphere and external plasma flow. In this study, a steady solar wind with, as well as without, the interplanetary magnetic field (IMF) is applied to the inflow boundary. The results clearly indicate that the global structure of the magnetic field lines of force is strongly affected by the rotation of Jupiter as well as by the solar wind. It is also found that magnetic reconnection at the tail region generates the plasma outflow and greatly modifies the corotational structure of the plasmas in the magnetosphere. Especially, when a relatively high-speed solar wind or a solar wind with a northward IMF collides with the magnetosphere, strong magnetic reconnection at the tail induces the tail-dusk flow, which is against the corotation. On the other hand, the evident tail-dusk flow does not appear in the case of a low-speed solar wind or in the case with a southward IMF. Thus the internal structure of the rotating magnetosphere could be altered qualitatively in response to changes in the solar wind parameters. [References: 46]
机译:基于磁流体动力学(MHD)仿真,提出了木星磁层的全局模型,该模型考虑了快速旋转的磁层与外部等离子体流之间的相互作用。在这项研究中,在有或没有行星际磁场(IMF)的情况下,将稳定的太阳风应用于入流边界。结果清楚地表明,磁力线的整体结构受木星旋转以及太阳风的强烈影响。还发现在尾部区域的磁重新连接产生等离子体流出,并极大地改变了磁层中等离子体的配偶结构。尤其是,当相对高速的太阳风或具有北向IMF的太阳风与磁层碰撞时,尾部的强磁重连会引起尾黄昏流动,这与同向旋转相反。另一方面,在低速太阳风或IMF向南的情况下,不会出现明显的尾流。因此,可以响应于太阳风参数的变化而定性地改变旋转磁层的内部结构。 [参考:46]

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