Detection of Surface Rocks and Small Craters in Permanently Shadowed Regions of the Lunar South Pole Based on YOLOv7 and Markov Random Field Algorithms in SAR Images

• Published in: Remote Sensing
• Main Authors: Tong Xia, Xuancheng Ren, Yuntian Liu, Niutao Liu, Feng Xu, Ya-Qiu Jin
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2024
• Subjects: crater detection; rocks; lunar south pole; PSR; SAR; Science; Q; Shackleton; South Pole; South pole
• Online Access: https://doi.org/10.3390/rs16111834; https://doaj.org/article/6839eef0764f41c09b694d370feff5fc

Excluding rough areas with surface rocks and craters is critical for the safety of landing missions, such as China’s Chang’e-7 mission, in the permanently shadowed region (PSR) of the lunar south pole. Binned digital elevation model (DEM) data can describe the undulating surface, but the DEM data can hardly detect surface rocks because of median-averaging. High-resolution images from a synthetic aperture radar (SAR) can be used to map discrete rocks and small craters according to their strong backscattering. This study utilizes the You Only Look Once version 7 (YOLOv7) tool to detect varying-sized craters in SAR images. It also employs the Markov random field (MRF) algorithm to identify surface rocks, which are usually difficult to detect in DEM data. The results are validated by optical images and DEM data in non-PSR. With the assistance of the DEM data, regions with slopes larger than 10° are excluded. YOLOv7 and MRF are applied to detect craters and rocky surfaces and exclude regions with steep slopes in the PSRs of craters Shoemaker, Slater, and Shackleton, respectively. This study proves SAR images are feasible in the selection of landing sites in the PSRs for future missions.