Exploring the Magnetotail From Low Altitudes: Evolution of Energetic Electron Flux During the Substorm Growth Phase

Abstract The magnetospheric substorm, which plays a crucial role in flux and energy transport across Earth's magnetosphere, features the formation of a thin, elongated current sheet in the magnetotail during its growth phase. This phase is characterized by a decrease in the equatorial magnetic field and the stretching of magnetic field lines. Observing these large‐scale magnetic field reconfigurations is challenging with single‐point satellite measurements, which provide only spatially localized snapshots of system dynamics. Conversely, low‐altitude spacecraft measurements of energetic electron fluxes, such as those from Electron Losses and Fields Investigation (ELFIN), offer a unique opportunity to remotely sense the equatorial magnetic field in the magnetotail during substorms by measuring the latitudinal variations of energetic electron isotropic fluxes. Because of strong scattering caused by the curvature of magnetic field lines, energetic electrons in the magnetotail are mostly isotropic. Consequently, variations in their fluxes at low altitudes are expected to reflect the reconfiguration of the magnetotail magnetic field. To better understand the connection between electron flux variation at low altitudes and magnetic field reconfiguration during substorms, we compared low‐altitude ELFIN observations with simulations from the Rice Convection Model (RCM). The RCM, which assumes fully isotropic electron distributions, provides a robust framework for describing energetic electron dynamics in the plasma sheet and determining the self‐consistent magnetic field configuration during substorms. The comparison of ELFIN observations and RCM simulations confirms our interpretation of electron flux dynamics at low altitudes during the substorm growth phase and validates the use of such observations to infer magnetotail dynamics during substorms.