Using Laser Altimetry to Finely Map the Permanently Shadowed Regions of the Lunar South Pole Using an Iterative Self-Constrained Adjustment Strategy

• Published in: IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
• Main Authors: Huan Xie, Xiaoshuai Liu, Yusheng Xu, Zhen Ye, Shijie Liu, Xin Li, Binbin Li, Qi Xu, Yalei Guo, Xiaohua Tong
• Format: Article in Journal/Newspaper
• Language: English
• Published: IEEE 2022
• Subjects: Laser altimetry; lunar orbiter laser altimeter (LOLA); permanently shadowed regions (PSRs); topographic mapping; Ocean engineering; TC1501-1800; Geophysics. Cosmic physics; QC801-809; Lola; South Pole; South pole
• Online Access: https://doi.org/10.1109/JSTARS.2022.3204765; https://doaj.org/article/e30b66efbc7f4f738f1990a3340763bc

Laser altimeters are capable of achieving fine mapping of the permanently shadowed regions (PSRs) of the Moon, which can provide fundamental topographic data for planetary missions. However, various factors can cause uncertainty in the geolocation of laser spots, which in turn causes terrain artifacts. In this article, we present an iterative self-constrained adjustment method to reduce the uncertainty of laser spot positioning. First, grid search was conducted for each altimetric profile from the lunar orbiter laser altimeter (LOLA), to minimize the weighted root-mean-square error (RMSE), constrained by the other altimetric profiles. Second, the updated profiles were iteratively adjusted until the adjustment value for the plane position converged. In addition, statistics from the standardized de-trended slope and residual were created to eliminate outliers, which were indeed some pseudo-topographic observations. In order to validate the results, the deviation of the elevation by projecting the adjusted laser profiles onto the improved LOLA digital elevation model (DEM) were calculated. The mean absolute error between the two is 0.25 m and the RMSE is 0.46 m. For the local terrain features with large differences, high resolution optical images were used for visual interpretation. The analysis shows that the obtained results appear to be more reasonable. Finally, using the corrected LOLA altimetric data, we made a new DEM of the PSRs within 89°S of the lunar south pole, which can provide a refined and reliable topographic dataset for follow-up research.