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Topographic modeling and analysis of the landing site of Chang'E-3 on the Moon

机译:E娥三号登陆月球的地形建模与分析

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The Chinese lunar probe Chang'E-3, carrying the "Jade Rabbit" lunar rover, successfully landed in the Sinus Iridum area on the Moon on December 14, 2013. This paper presents the characterization activities that were done for the selection of the landing area, including topographic modeling and analysis based on multisource lunar remote sensing data. Seven meter-resolution Chang'E-2 imagery and Lunar Orbiter Laser Altimeter data were integrated to generate a digital elevation model (DEM) with a resolution of 20 m for the entire Sinus Iridum landing area. Long baseline slopes were assessed according to this DEM for all of this area. Lunar Reconnaissance Orbiter narrow-angle camera images and 1.5 m-resolution Chang'E-2 imagery were used to derive DEMs with higher resolution (4 m) at several local regions within the Sinus Iridum landing area. Slope analyses at lander footprint scale (~8 m) were performed in these local regions. Craters were detected from the DEMs and the derived orthophotos, and size-frequency distributions were generated. Crater morphological statistics, including the depth/diameter ratios, rim height/diameter ratios and wall slopes, were analyzed. The results showed that the Sinus Iridum landing area is relatively flat. Most of the area has slopes of less than 15°. The steeper slopes are mainly alongside craters and ridges. The crater size-frequency distribution is close to the equilibrium distribution. The crater ages, as indicated by their morphological statistics, vary from mature to relatively fresh in different regions. These topographic modeling and analysis results were used for strategic planning to identify the landing site for the Chang'E-3 and made a useful contribution to the success of the Chang'E-3 mission.
机译:携带“玉兔”月球车的中国登月探测器Chang娥三号于2013年12月14日成功降落在月球的窦铱地区。本文介绍了为选择降落而进行的表征活动区域,包括基于多源月球遥感数据的地形建模和分析。集成了七米分辨率的Chang'E-2影像和月球轨道激光测高仪数据,以生成整个窦铱星着陆区分辨率为20 m的数字高程模型(DEM)。根据该DEM评估了整个区域的长基线斜率。月球侦察轨道器窄角相机图像和1.5 m分辨率的Chang'E-2图像被用于在仙女座铱星着陆区内的几个局部区域获得更高分辨率(4 m)的DEM。在这些局部地区进行了着陆器足迹规模(〜8 m)的斜坡分析。从DEM和派生的正射照片中发现了火山口,并生成了尺寸-频率分布。分析了火山口的形态统计数据,包括深度/直径比,轮辋高度/直径比和壁坡度。结果表明,窦铱星登陆区相对平坦。大部分地区的坡度小于15°。较陡的斜坡主要与火山口和山脊并排。火山口的大小-频率分布接近于平衡分布。形态统计表明,火山口年龄在不同地区从成熟到相对新鲜。这些地形建模和分析结果用于战略规划,以识别Chang娥三号的着陆点,并为Chang娥三号任务的成功做出了有益的贡献。

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