“…At ion kinetic scales magnetic spectra steepen, due to some combination of dispersive and dissipative effects, leading to a sub‐ion scale energy cascade (Alexandrova et al., 2008, 2009, 2012; Sahraoui et al., 2009, 2010). Kinetic spectra with approximate k −2.7 scaling characterize the solar wind at 1 AU and the inner heliosphere (Alexandrova et al., 2012; Bowen, Mallet, Bale, et al., 2020; Chen et al., 2010; Sahraoui et al., 2009, 2013). The observed steepening is consistent with the dispersion of Alfvénic to kinetic Alfvén wave (KAW) turbulence alongside some intermittency or dissipation (Boldyrev & Perez, 2012; Chen et al., 2013; Franci et al., 2015, 2016; Howes et al., 2011; Schekochihin et al., 2009).…”