# Cometary topography and phase darkening

## TL;DR

This study models how cometary surface roughness influences phase darkening, revealing that topography accounts for a significant portion of observed darkening alongside physical and chemical factors.

## Contribution

The paper introduces a numerical model linking cometary topography to phase darkening, quantifying the geometric effects of macro-roughness on observed brightness.

## Key findings

- Self-shadowing accounts for up to 22% of darkening in primitive comets.
- Topography contributes significantly but is not the sole factor in phase darkening.
- Physical and chemical properties remain the primary causes of phase darkening.

## Abstract

Cometary surfaces can change significantly and rapidly due to the sublimation of their volatile material. Many authors have investigated this evolution; Vincent et al. (2017) have used topographic data from all comets visited by spacecrafts to derive a quantitative model which relates large scale roughness (i.e. topography) with the evolution state of the nucleus for Jupiter Family Comets (JFCs). Meanwhile, ground based observers have published measurements of the phase functions of many JFCs and reported a trend in the phase darkening, with primitive objects showing a stronger darkening than evolved ones). In this paper, we use a numerical implementation of the topographic description by Vincent et al. (2017) to build virtual comets and measure the phase darkening induced by the different levels of macro-roughness. We then compare our model with the values published by Kokotanekova et al. (2018) We find that pure geometric effects like self-shadowing can represent up to 22% of the darkening observed for more primitive objects, and 15% for evolved surfaces. This shows that although physical and chemical properties remain the major contributor to the phase darkening, the additional effect of the topography cannot be neglected.