“…Another method is the magnetogram inversion technique [ Mishin , ; Kamide and Baumjohann , ], which calculates electric potential, field‐aligned current, and equivalent current using the long‐period variable geomagnetic field in the polar region as input. In this method, the high‐latitude boundary of Region‐1 FAC is considered as the OCB [e.g., Mishin et al , , ]. In addition, the sophisticated MHD simulations can be used to describe the solar wind‐magnetosphere interaction, thus can also make it possible to look at the character of the OCB in global scales [e.g., Lopez et al , ; Kabin et al , ; Rae et al , , ; Wang et al , ].…”