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Response of the Earth's Magnetosphere and Ionosphere to Solar Wind Driver and Ionosphere Load: Results of Global MHD Simulations

机译:地球磁层和电离层对太阳风驱动器和电离层负荷的响应:全球MHD模拟的结果

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摘要

Three-dimensional global magnetohydrodynamic simulations of the solar wind-magnetosphere-ionosphere system are carried out to explore the dependence of the magnetospheric reconnection voltage, the ionospheric transpolar potential, and the field aligned currents (FACs) on the solar wind driver and ionosphere load for the cases with pure southward interplanetary magnetic field (IMF). It is shown that the reconnection voltage and the transpolar potential increase monotonically with decreasing Pedersen conductance (Sigma(P)), increasing southward IMF strength (B-s) and solar wind speed (upsilon(sw)). Moreover, both regions 1 and 2 FACs increase when B-s and upsilon(sw) increase, whereas the two currents behave differently in response to Sigma(P). As Sigma(P) increases, the region 1 FAC increases monotonically, but region 2 FAC shows a non-monotonic response to the increase of Sigma(P): it first increases in the range of (0,5) Siemens and then decreases for Sigma(P) > 5 Siemens.
机译:进行了太阳风-磁层-电离层系统的三维全球磁流体动力学模拟,以探索磁层重新连接电压,电离层跨极电势以及场对准电流(FAC)对太阳风驱动器和电离层负载的依赖性。带有纯南向星际磁场(IMF)的情况。结果表明,重新连接电压和跨极电势随着Pedersen电导(Sigma(P))的减小而单调增加,向南的IMF强度(B-s)和太阳风速(upsilon(sw))增大。此外,当B-s和upsilon(sw)增加时,区域1和2 FAC都会增加,而两个电流响应Sigma(P)的行为却有所不同。随着Sigma(P)的增加,区域1 FAC单调增加,但是区域2 FAC对Sigma(P)的增加表现出非单调响应:它首先在(0,5)Siemens范围内增加,然后减小Sigma(P)> 5西门子。

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