Magnetic reconnection, the process in which magnetic fields of opposite polarity annihilate and reconnect converting magnetic energy into kinetic energy, has long been a classic topic of research in plasma physics. In addition to its ubiquity and explosive energy release, at the magnetopause, the change in magnetic field topology during magnetic reconnection allows particles from the solar wind and the magnetosphere to mix. Such mixing, as well as the topological change itself, is believed to be the major channel for mass and momentum exchange on a global scale. On the day side of the magnetosphere, magnetic reconnection is often associated with a commonly observed phenomenon called the flux transfer event (FTE), characterized by the magnetic field in the form of a magnetic flux rope (Russell & Elphic, 1979). Four different theories have been proposed to reconstruct/generate their global topologies, and it is not yet observationally settled which mechanism is operative. Three mechanisms are summarized by Fear et al. (2008) and Figure 1: The original connected flux rope model (Russell & Elphic, 1979); the magnetic island model, often called the multiple X-line model (Lee & Fu, 1985); and the outflow-region bubble model requiring a single x-line (Scholer, 1988; Southwood et al., 1988), which is later associated with "crater" FTEs when spacecraft encounters the separatrix of reconnection (Trenchi et al., 2019). A fourth type is the proposed magnetic reconnection induced by flow vortices, such as modeled