Abstract:Abstract. For a long time, the interactions of the solar wind with the Earth’s magnetosphere have been analyzed with the help of three-dimensional (3D) global particle-in-cell (PIC) simulation where the interplanetary magnetic field (IMF) is steadily northward. Yet the Earth’s magnetosphere and the Kelvin-Helmholtz Instability (KHI) in a global, dayside and nightside magnetotail configuration using the 3D PIC simulations has not been well examined. In this work, we compared the simulation results for both high… Show more
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