Flux ropes (FRs) are magnetic structures composed of helical magnetic field lines, which are universal in space. The FRs act as flux transfer events (FTEs) at the Earth's magnetopause (e.g., Russell & Elphic, 1978), plasmoids in the magnetotail (Zong et al., 2004), and coronal mass ejection in the heliosphere (Ruffenach et al., 2012). Earth's magnetopause FRs play an important role in the transfer of energy and plasma from the solar wind into the magnetosphere during the southward interplanetary magnetic field (IMF). Russell and Elphic (1978) first observed the FTEs, and they believe that FTEs are elbow-shaped magnetopause flux tubes formed by magnetopause reconnection. Lee and Fu (1985) proposed that magnetopause multiple X line reconnection can form FTEs as magnetic FRs with helical internal structure. In the following decades, based on the spacecraft observations and theories, the configuration, size, evolution, and inner structure of the magnetopause FRs were studied extensively (e.g.,