Global Hybrid Simulation of the Magnetopause Boundary Layer in Low- and High-Latitude Magnetic Reconnections
A 2-D global hybrid simulation is carried out to study the structure of the dayside magnetopause in the noon-midnight meridian plane associated with magnetic reconnection. In the simulation the bow shock, magnetosheath, and magnetopause are formed self-consistently by supersonic solar wind passing the geomagnetic field. The reconnection events at
Xie, H. et al.
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2001