A method to distinguish between micro- and macro-granular surfaces of small Solar System bodies
D. Bischoff, B. Gundlach, J. Blum

TL;DR
This paper presents a numerical method to distinguish micro- from macro-porous surfaces of small Solar System bodies by analyzing sunrise temperature measurements, aiding remote sensing of their surface structures.
Contribution
It introduces a strategy using surface temperature measurements, especially at sunrise, to differentiate surface porosity types based on thermal properties.
Findings
Sunrise temperature varies significantly with surface structure.
Daily temperature cycles are insensitive to surface granularity.
Higher solar intensity enhances temperature differences at sunrise.
Abstract
The surface granularity of small Solar System bodies is diverse through the different types of planetary bodies and even for specific objects it is often not known in detail. One of the physical properties that strongly depends on the surface structure is the surface temperature. In highly porous media with large voids, radiation can efficiently transport heat, whereas more compact, micro-porous structures transport the heat primarily by conduction through the solid material. In this work, we investigate under which conditions a macro-porous surface can be distinguished from a micro-porous one by simply measuring the surface temperature. In our numerical simulations, we included circular and elliptical orbits with and without obliquity and varied the rotation period of the considered objects. We found that daily temperature cycles are rather insensitive to the specific surface…
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