Comparative photometric analysis of the Reiner Gamma swirl and Chang’e 5 landing site

¹ Image Analysis Group, TU Dortmund University Otto-Hahn-Straße 4, Dortmund, Germany
e-mail: marcel.hess@tu-dortmund.de
² Shandong Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, School of Space Science and Physics, Institute of Space Sciences, Shandong University, Weihai, Shandong, 264209, PR China
³ Physical Research Laboratory, University Area, Ahmedabad, Gujarat 380009, India

Received: 7 February 2023
Accepted: 3 May 2023

Abstract

Context. Lunar swirls are bright albedo features only found on the Moon that are still not entirely understood. It is commonly accepted that reduced space weathering plays a role in explaining the origins of lunar swirls because the local magnetic fields that are typically associated with these albedo anomalies are effective in reducing the solar wind influx. However, additional processes are required to fully explain the spectral, photometric, and polarimetric properties of the swirls.

Aims. In this study, we compare the photometric properties of the Chang’e-5 landing site to those of the Reiner Gamma swirl. Because the physical effects of a landing rocket jet on the lunar regolith are relatively well known, these observations can provide important insights into the physical properties of lunar swirls.

Methods. We determined the single scattering albedo, opposition effect strength, and surface roughness of the Reiner Gamma swirl and the Chang’e-5 landing site with their respective statistical uncertainties based on the Hapke model and Bayesian inference sampling.

Results. The Chang’e-5 landing site and the Reiner Gamma swirl exhibit similar photometric properties, in particular: an increased albedo and a reduced opposition effect strength. Additionally, the landing site is about 20% less rough compared to the surrounding area.

Conclusions. These findings suggest that the swirl surface is less porous compared to the surrounding surface, similarly to a landing site where the top layer of the regolith has been blown away effectively so that the compactness was increased. We conclude that external mechanisms that are able to compress the uppermost regolith layer are involved in lunar swirl formation, such as interactions with the gaseous hull of a passing comet.