“…Chen et al., 2015; Izutsu et al., 2012; Yao et al., 2011). Indeed, the magnetosheath is filled by a wide range of ion‐kinetic scale waves (Anderson & Fuselier, 1993; Rakhmanova et al., 2021; Sahraoui et al., 2003; Song et al., 1994; Zimbardo et al., 2010) generated either by local instabilities of anisotropic ion populations (Anderson et al., 1994; Gary & Lee, 1994; Schwartz et al., 1996) or by mode conversion from large‐scale magnetohydrodynamic (MHD) waves to ion‐kinetic scale waves (C. C. Chaston et al., 2007; Cheng et al., 2020; Johnson et al., 2001; Kim et al., 2022; Lin et al., 2012; Shi et al., 2013).…”