“…The hybrid approach is well‐documented and has been used to investigate the plasma interactions of many solar system objects. Examples include Earth’s Moon (e.g., Holmström et al., 2012; Liuzzo et al., 2021), the moons of Jupiter (e.g., Fatemi et al., 2016; Lipatov & Combi, 2006; Lipatov et al., 2010, 2013; Liuzzo et al., 2015, 2016; 2017, 2018; 2019a, 2019b; 2020; Lindkvist et al., 2015; Poppe et al., 2018; Sittler et al., 2013) and Saturn (e.g., Kriegel et al., 2009, 2011, 2014; Ledvina et al., 2012; Lipatov et al., 2012; Sillanpää et al., 2006; Sillanpää & Johnson, 2015), as well as Mercury (e.g., Exner et al., 2018; Kallio & Janhunen, 2003), Venus (e.g., Kallio et al., 2006; Martinecz et al., 2009), Mars (e.g., Kallio & Janhunen, 2001; Modolo et al., 2016), and Pluto (e.g., Barnes et al., 2019; Delamere, 2009; Feyerabend et al., 2017).…”