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Cartography of the Lunokhod-1 landing site and traverse from LRO image and stereo-topographic data

机译:Lunokhod-1着陆点的制图,并从LRO图像和立体地形数据遍历

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We have derived a stereo-topographic model and an orthoimage mosaic based on Lunar Reconnaissance Orbiter (LRO) Narrow Angle Camera (NAC) images to study the Luna-17 landing site. In the images (0.33-0.5 m/pixel), the Lunokhod-1, the Luna-17 landed spacecraft, and the rover tracks can clearly be identified and mapped for 99% of the traverse. The traverse was found to be 9.93 km long, approximately 0.50 km shorter over what had been estimated earlier (10.54 km). The total topographic relief along the traverse was found to be within 26 m. Along its traverse, the rover encountered slopes of up to 5 , estimated over 2.5 m baselength. By comparison with previously published topographic maps and using our orthomosaic as a reference (which had been tied to the well-known Lunokhod-1 Laser reflector coordinates), we report on coordinates of Lunokhod-1's panorama points and overnight stops. Comparisons of currently mapped tracks with previous traverse reconstructions show good matches on small scale, but reveal that previous maps had long-wavelength geometric distortions of up to 100-m level. Agreement in topographic trends was very limited.
机译:我们基于月球侦察轨道器(LRO)窄角相机(NAC)图像得出了立体地形模型和正射影像马赛克,以研究Luna-17着陆点。在图像(0.33-0.5 m /像素)中,可以清楚地识别出Lunokhod-1,Luna-17降落的航天器和漫游者的轨迹,并将其映射为遍历的99%。测得的导线长度为9.93公里,比先前估计的导线长度(10.54公里)短约0.50公里。发现沿导线的总地形起伏在26 m以内。漫游车沿其行驶路线遇到的坡度最大为5,​​估计超过2.5 m的基长。通过与先前发布的地形图进行比较,并以我们的正马赛克为参考(已绑定到著名的Lunokhod-1激光反射器坐标),我们报告Lunokhod-1的全景点和过夜停靠点的坐标。当前映射的轨迹与先前的遍历重建的比较显示了小比例的良好匹配,但是揭示了先前的映射具有高达100-m级别的长波长几何变形。地形趋势的一致性非常有限。

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