The global structure and dynamics of the Jovian magnetosphere are mainly controlled by the planet's fast rotation (e.g., Vasyliunas, 1983), while the solar wind interaction is generally recognized to play a secondary role, mostly limited to the outer magnetosphere (e.g., Bagenal et al., 2017;Cowley et al., 2003; Khurana et al., 2004 and references therein). The planetary fast rotation along with the dominance of internal plasma source make the solar wind secondarily important relative to the planetary rotation, up to about 40-50 R J , and even more so within the inner magnetosphere (L < 20 R J ) threaded by closed dipole-like magnetic field lines (e.g., Bagenal et al., 2017;Khurana et al., 2004;Krupp et al., 2004).Jupiter's Galilean moon Io is the most geologically active object in the Solar system. Its volcanism produces and maintains Io's thick atmosphere, filled with abundant sulfur dioxide (SO 2 ), from which atmospheric particles are constantly injected along Io's orbit, creating a neutral cloud centered at L = ∼5.9 R J . Ionization of these neutrals by electron collisions or charge-exchanges produces iogenic ions trapped in Jupiter's strong magnetic field, forming a dense plasma region named the Io plasma torus (Bagenal & Dols, 2020;Thomas et al., 2004). Io is the dominant plasma source of the Jovian magnetosphere. While the total plasma loading rate is typically on the order of 1 ton/s, this value is quite uncertain and highly variable in both time and longitudes (e.g., Thomas et al., 2004).