The source of protons in the Jovian magnetosphere has been historically difficult to determine experimentally. The volcanic moon Io is the primary source of plasma in the magnetosphere, inputting ∼10 3 kg s −1 of heavy ions (e.g., Bagenal & Delamere, 2011). Approximately 10% of the total magnetospheric number density is attributed to protons (e.g., Dougherty et al., 2017), which are not sourced by Io. The proton influx necessary to account for this population from 5 to 30 R J (Jovian radii) has been estimated to be 2.5-13 kg s −1 (Bodisch et al., 2017). There are at least three possible sources of protons in Jupiter's magnetosphere: solar wind, icy moons, and ionospheric outflow. Solar wind leakage across the magnetopause boundary is one possible source (e.g., Delamere et al., 2015), yet it is difficult to explain how such protons would be transported to the inner magnetosphere via this mechanism. Since Jupiter is likely not undergoing standard a Dungey cycle (McComas & Bagenal, 2007), it is also difficult to attribute magnetospheric protons to the solar wind, particularly in the innermost regions. Of the icy moons, Europa sustains a neutral torus of many species including hydrogen (e.g., Smith et al., 2019), which can charge exchange with the local plasma environment, however, at much lower quantities than necessary to source the magnetospheric proton population (e.g., Bagenal & Dols, 2020). The focus of this study is to constrain the ionospheric outflow source of protons. The outflow has been previously estimated to be 35 kg s −1 (Nagy et al., 1986) integrating over the entire polar region, and 18.7-31.7 kg s −1 (Martin et al., 2020) at high latitudes between Io's M-Shell and up to and including the auroral oval, with 4.3-8.5 kg s −1 estimated to specifically outflow from the auroral oval. Both theoretical estimates are sufficient to explain the source of protons in Jupiter's magnetosphere, but the mechanisms of ionospheric outflow have not been previously observed.