SIMBAD references

Over two decades ago, the first detection of electron cyclotron maser instability radio emission from a brown dwarf confirmed the presence of aurorally precipitating electrons on these objects. This detection established that brown dwarfs can exhibit magnetic activity that is planetary and auroral, rather than stellar in nature. This discovery motivated ongoing observational searches for the corresponding optical, ultraviolet, and infrared auroral emission expected based on solar system analogs. The continuing nondetection of such auroral emission indicates that important differences exist between auroral processes on brown dwarfs and solar system planets. In this work, we implement a Monte Carlo simulation of monoenergetic electron beams interacting with brown dwarf atmospheres as a step toward understanding the physics of brown dwarf auroral emission. We detail the algorithm and underlying assumptions and validate against previously published Jovian results. Our results agree well with the literature, with some discrepancies from our updated interaction cross sections. We demonstrate the applicability of our simulation across the range of surface gravities and effective temperatures of radio-emitting brown dwarfs. We present an analytic parameterization of interaction rates based on our finding that atmospheric column density governs the interaction profiles. We apply this parameterization to calculate the total volumetric interaction rates and energy deposition rate for representative electron beam energy spectra enabling future predictions for spectra of aurorally emitting brown dwarfs. Simulations of high-energy electron interactions with substellar hydrogen-dominated atmospheres will guide observational searches for multiwavelength auroral features beyond the solar system.