“…However, it has been found that the Maxwellian energy spectrum tends to underestimate the incident soft (0.1–1 keV) electrons and the difference of the 0.1 keV electrons can be up to 2–3 orders of magnitude (e.g., McGranaghan, Knipp, Matsuo, et al., 2015; McGranaghan, Knipp, Solomon, Fang, 2015; McIntosh & Anderson, 2014; Wing et al., 2019). Although modeling efforts have been made to incorporate additional types of energy spectra different from a Maxwellian energy spectrum in recently developed electron precipitation models (e.g., McGranaghan et al., 2016; Newell et al., 2009, 2014), soft electron precipitation may still be inaccurately represented (Khazanov et al., 2021; Wing et al., 2019). Since soft electron precipitation is an important ionization source in the F‐region ionosphere, the conductivity and Joule heating at F‐region altitudes may not be correctly estimated when the Maxwellian energy spectrum is used in GCMs (e.g., McGranaghan et al., 2016; Rees, 1989).…”