The near-surface environments of Solar System airless bodies including Mercury, the Moon, asteroids, and Mars' moons are controlled by the lack of an appreciable atmosphere, incident solar irradiation, and the compositional and physical properties of the regolith. Early laboratory studies demonstrated that the near-surface environment, particle size, and porosity affected thermal infrared (TIR) emissivity spectral measurements of terrestrial minerals and lunar soils (e.g.,