Earth's magnetosphere is constantly dynamical during its interaction with the solar wind and involves a global convection cycle of mass, energy and magnetic flux (Dungey, 1961). Such cycle has been suggested to be driven primarily by magnetic reconnection both at regions along the magnetopause (e.g., Burch et al., 2016) and in the magnetotail (e.g., Øieroset et al., 2001). Magnetic reconnection, during which magnetic field lines "break" and "reconnect," has been thought to be capable of efficiently converting electromagnetic energy accumulated during the interaction between Earth and the solar wind into thermal and kinetic energy of particles in the magnetosphere, generating high-speed plasma flows, that is, bursty bulk flows (e.g.,