Abstract

Lunar craters are very important for estimating the geological age of the Moon, studying the evolution of the Moon, and for landing site selection. Due to a lack of labeled samples, processing times due to high-resolution imagery, the small number of suitable detection models, and the influence of solar illumination, Crater Detection Algorithms (CDAs) based on Digital Orthophoto Maps (DOMs) have not yet been well-developed. In this paper, a large number of training data are labeled manually in the Highland and Maria regions, using the Chang’E-2 (CE-2) DOM; however, the labeled data cannot cover all kinds of crater types. To solve the problem of small crater detection, a new crater detection model (Crater R-CNN) is proposed, which can effectively extract the spatial and semantic information of craters from DOM data. As incomplete labeled samples are not conducive for model training, the Two-Teachers Self-training with Noise (TTSN) method is used to train the Crater R-CNN model, thus constructing a new model—called Crater R-CNN with TTSN—which can achieve state-of-the-art performance. To evaluate the accuracy of the model, three other detection models (Mask R-CNN, no-Mask R-CNN, and Crater R-CNN) based on semi-supervised deep learning were used to detect craters in the Highland and Maria regions. The results indicate that Crater R-CNN with TTSN achieved the highest precision (of 91.4% and 88.5%, respectively) in the Highland and Maria regions, even obtaining the highest recall and F1 score. Compared with Mask R-CNN, no-Mask R-CNN, and Crater R-CNN, Crater R-CNN with TTSN had strong robustness and better generalization ability for crater detection within 1 km in different terrains, making it possible to detect small craters with high accuracy when using DOM data.

Highlights

  • IntroductionCraters are the main type of lunar topography, which record information about past meteorite impacts and solar activities, such as solar winds and cosmic X-ray radiation [1]

  • Craters are the main type of lunar topography, which record information about past meteorite impacts and solar activities, such as solar winds and cosmic X-ray radiation [1].craters are used to study the geological age [2,3], evolution, dynamic mechanisms, and the meteorite impact history [4,5] of the Moon

  • We describe a robust and highly accurate method based on Crater R-CNN and

Read more

Summary

Introduction

Craters are the main type of lunar topography, which record information about past meteorite impacts and solar activities, such as solar winds and cosmic X-ray radiation [1]. Craters are used to study the geological age [2,3], evolution, dynamic mechanisms, and the meteorite impact history [4,5] of the Moon. Craters are a hindrance to lunar landings and cruising, affecting landing site selection, rover navigation and positioning, and cruising route planning [6]. As craters play an important role in lunar scientific research and engineering, lunar crater detection has become a critical problem. Several crater databases have been built using low-resolution remote sensing data.

Objectives
Methods
Results
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.