Ganymede-Jupiter's largest moon-is the only known moon in the Solar System to generate its own internal magnetic field (Gurnett et al., 1996;Kivelson et al., 1996) and therefore its space environment is of high scientific interest. In part, what makes Ganymede so interesting is that its magnetic field forms a mini-magnetosphere, with field lines connected to both hemispheres, that is, "closed," embedded deep within (semi-major axis = 14.97 Jovian radii or R J ) Jupiter's magnetosphere where the Alfvénic Mach number (M A ) is < 1. Classified as a sub-Alfvénic (and thus also sub-fast-magnetosonic by definition) interaction (e.g., Saur, 2021), no bow shock develops around the moon. Additionally, another aspect that makes Ganymede particularly interesting is the phenomenon of magnetic reconnection. Unlike Earth, and other planetary magnetospheric environments, which are embedded in dynamic solar wind conditions, the upstream conditions near Ganymede are relatively steady compared to plasma convection through Ganymede's magnetospheric system (Kivelson et al., 1998), therefore, making it possible to probe the nature of magnetic reconnection under relatively steady driving conditions (Ebert