“…Magnetic reconnection, for which localized changes in magnetic topology result in rapid transfer of energy from fields to particles, has been observed in detail by Magnetospheric Multiscale (MMS) at Earth's magnetopause and more recently in the turbulent magnetosheath (Phan et al, 2018). In the standard model, reconnection occurs within an electron-scale diffusion region (Bohdan et al, 2017;Vasyliunas, 1975), while at ion scales coupled ions are ejected from the diffusion region as bidirectional jets (Gosling et al, 2005;Paschmann et al, 1979;Phan et al, 2000). In the standard model, reconnection occurs within an electron-scale diffusion region (Bohdan et al, 2017;Vasyliunas, 1975), while at ion scales coupled ions are ejected from the diffusion region as bidirectional jets (Gosling et al, 2005;Paschmann et al, 1979;Phan et al, 2000).…”