Though comparable to Earth in its size, internal structure, and distance from the Sun, Venus lacks an intrinsic magnetic field, thus allowing the solar wind to closely interact with its atmosphere and generate interesting plasma phenomena (Futaana et al., 2017). For example, as the solar wind is diverted around Venus, the interplanetary magnetic field (IMF) drapes around the planet and generates currents in the ionosphere, resulting in an induced magnetosphere. The extent of this magnetosphere is much smaller (∼0.05 Venus radii at the subsolar point) than that of Earth's magnetosphere (∼10 Earth radii) (Russell et al., 2016), but still provides a dayside magnetic barrier that diverts the solar wind's flow, causes the IMF field lines to pile up, and forms an upstream bow shock (Luhmann, 1986;Zhang et al., 1991). Studying such phenomena at Venus provides insight into how other unmagnetized atmospheric bodies interact with magnetized plasma flows, either in our Solar System (e.g., Mars