Na Sun , Yongjiu Feng , Xiaohua Tong , Pengshuo Li , Rong Wang , Yuhao Wang , Yuze Cao , Zilong Cao , Xiong Xu , Yusheng Xu , Shijie Liu
{"title":"一种考虑图像阴影的滑动窗口方法用于MRO HiRISE数据集的火星岩石探测","authors":"Na Sun , Yongjiu Feng , Xiaohua Tong , Pengshuo Li , Rong Wang , Yuhao Wang , Yuze Cao , Zilong Cao , Xiong Xu , Yusheng Xu , Shijie Liu","doi":"10.1016/j.pss.2025.106155","DOIUrl":null,"url":null,"abstract":"<div><div>Rock distribution is a crucial factor in landing site selection for Mars exploration. Typically, rocks in flat Martian terrains are characterized by clear boundaries and distinct shadows. We developed a new method (named SSW-ROCK) for rock detection from HiRISE images using the shadow (S) and sliding window technique (SW). SSW-ROCK uses shadows to define the minimum bounding rectangle in the direction of illumination, establishing an initial sliding window based on this rectangle. The window is then slid to the termination position according to the predefined conditions. The rock size can be obtained by fitting the ellipse with the positions of the initial and termination windows. The rock height is estimated using the shadow length along the illumination direction. We used five HiRISE images of Mars between 65° N −70° N for rock detection and detected 532,284 rocks with maximum diameters >1.5 m. We selected accuracy assessment areas in each of the five images and extracted the rocks manually. The SSW-ROCK results were assessed for accuracy using the manual results as a benchmark. In the assessment, we proposed two evaluation metrics, PS and PM: PS measures the proportion of SSW-ROCK results with center points within the range of manual results, while PM measures the proportion of manual results with center points within the range of SSW-ROCK results. Accuracy assessments in five selected areas showed that the mean for both PS and PM exceeded 77 %. Additionally, the dimensions detected by the SSW-ROCK method for known Mars landers closely match their actual sizes. These experiments demonstrate that the SSW-ROCK method is effective for rock detection in flat Martian terrains.</div></div>","PeriodicalId":20054,"journal":{"name":"Planetary and Space Science","volume":"265 ","pages":"Article 106155"},"PeriodicalIF":1.8000,"publicationDate":"2025-06-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A sliding window method considering image shadow to detect Mars rock from MRO HiRISE datasets\",\"authors\":\"Na Sun , Yongjiu Feng , Xiaohua Tong , Pengshuo Li , Rong Wang , Yuhao Wang , Yuze Cao , Zilong Cao , Xiong Xu , Yusheng Xu , Shijie Liu\",\"doi\":\"10.1016/j.pss.2025.106155\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Rock distribution is a crucial factor in landing site selection for Mars exploration. Typically, rocks in flat Martian terrains are characterized by clear boundaries and distinct shadows. We developed a new method (named SSW-ROCK) for rock detection from HiRISE images using the shadow (S) and sliding window technique (SW). SSW-ROCK uses shadows to define the minimum bounding rectangle in the direction of illumination, establishing an initial sliding window based on this rectangle. The window is then slid to the termination position according to the predefined conditions. The rock size can be obtained by fitting the ellipse with the positions of the initial and termination windows. The rock height is estimated using the shadow length along the illumination direction. We used five HiRISE images of Mars between 65° N −70° N for rock detection and detected 532,284 rocks with maximum diameters >1.5 m. We selected accuracy assessment areas in each of the five images and extracted the rocks manually. The SSW-ROCK results were assessed for accuracy using the manual results as a benchmark. In the assessment, we proposed two evaluation metrics, PS and PM: PS measures the proportion of SSW-ROCK results with center points within the range of manual results, while PM measures the proportion of manual results with center points within the range of SSW-ROCK results. Accuracy assessments in five selected areas showed that the mean for both PS and PM exceeded 77 %. Additionally, the dimensions detected by the SSW-ROCK method for known Mars landers closely match their actual sizes. These experiments demonstrate that the SSW-ROCK method is effective for rock detection in flat Martian terrains.</div></div>\",\"PeriodicalId\":20054,\"journal\":{\"name\":\"Planetary and Space Science\",\"volume\":\"265 \",\"pages\":\"Article 106155\"},\"PeriodicalIF\":1.8000,\"publicationDate\":\"2025-06-21\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Planetary and Space Science\",\"FirstCategoryId\":\"101\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0032063325001229\",\"RegionNum\":4,\"RegionCategory\":\"物理与天体物理\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ASTRONOMY & ASTROPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Planetary and Space Science","FirstCategoryId":"101","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0032063325001229","RegionNum":4,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
A sliding window method considering image shadow to detect Mars rock from MRO HiRISE datasets
Rock distribution is a crucial factor in landing site selection for Mars exploration. Typically, rocks in flat Martian terrains are characterized by clear boundaries and distinct shadows. We developed a new method (named SSW-ROCK) for rock detection from HiRISE images using the shadow (S) and sliding window technique (SW). SSW-ROCK uses shadows to define the minimum bounding rectangle in the direction of illumination, establishing an initial sliding window based on this rectangle. The window is then slid to the termination position according to the predefined conditions. The rock size can be obtained by fitting the ellipse with the positions of the initial and termination windows. The rock height is estimated using the shadow length along the illumination direction. We used five HiRISE images of Mars between 65° N −70° N for rock detection and detected 532,284 rocks with maximum diameters >1.5 m. We selected accuracy assessment areas in each of the five images and extracted the rocks manually. The SSW-ROCK results were assessed for accuracy using the manual results as a benchmark. In the assessment, we proposed two evaluation metrics, PS and PM: PS measures the proportion of SSW-ROCK results with center points within the range of manual results, while PM measures the proportion of manual results with center points within the range of SSW-ROCK results. Accuracy assessments in five selected areas showed that the mean for both PS and PM exceeded 77 %. Additionally, the dimensions detected by the SSW-ROCK method for known Mars landers closely match their actual sizes. These experiments demonstrate that the SSW-ROCK method is effective for rock detection in flat Martian terrains.
期刊介绍:
Planetary and Space Science publishes original articles as well as short communications (letters). Ground-based and space-borne instrumentation and laboratory simulation of solar system processes are included. The following fields of planetary and solar system research are covered:
• Celestial mechanics, including dynamical evolution of the solar system, gravitational captures and resonances, relativistic effects, tracking and dynamics
• Cosmochemistry and origin, including all aspects of the formation and initial physical and chemical evolution of the solar system
• Terrestrial planets and satellites, including the physics of the interiors, geology and morphology of the surfaces, tectonics, mineralogy and dating
• Outer planets and satellites, including formation and evolution, remote sensing at all wavelengths and in situ measurements
• Planetary atmospheres, including formation and evolution, circulation and meteorology, boundary layers, remote sensing and laboratory simulation
• Planetary magnetospheres and ionospheres, including origin of magnetic fields, magnetospheric plasma and radiation belts, and their interaction with the sun, the solar wind and satellites
• Small bodies, dust and rings, including asteroids, comets and zodiacal light and their interaction with the solar radiation and the solar wind
• Exobiology, including origin of life, detection of planetary ecosystems and pre-biological phenomena in the solar system and laboratory simulations
• Extrasolar systems, including the detection and/or the detectability of exoplanets and planetary systems, their formation and evolution, the physical and chemical properties of the exoplanets
• History of planetary and space research