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Electron density irregularities in the ionosphere can give rise to scintillations, affecting radio wave phase and amplitude. While scintillations in the cusp and polar cap regions are commonly associated with mesoscale density inhomogeneities and/or shearing, the auroral regions exhibit a strong correlation between scintillation and density structures generated by electron precipitation (arcs). We aim to examine the impact of electron precipitation on the formation of scintillation‐producing density structures using a high‐resolution physics‐based plasma model, the "Geospace Environment Model of Ion‐Neutral Interactions," coupled with a radio propagation model, the "Satellite‐beacon Ionospheric‐scintillation Global Model of the upper Atmosphere." Specifically, we explore the effects of varying spatial and temporal characteristics of the precipitation, including electron total energy flux and their characteristic energies, obtained from the all‐sky‐imagers and Poker Flat Incoherent Scatter Radar observations, on auroral scintillation. To capture small‐scale structures, we incorporate a power‐law turbulence spectrum that induces short wavelength features sensitive to scintillation. Finally, we compare our simulated scintillation results with satellite‐observed scintillations, along with spectral comparisons. Key Points: A physics‐based plasma model and a radio propagation model are used to examine the effects of precipitation on auroral scintillationPrecipitation fluxes with higher energy, a turbulent noise spectrum, and a faster‐moving arc intensify scintillationThe presence of small‐scale precipitation amplifies both phase and amplitude scintillations [ABSTRACT FROM AUTHOR]