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Surface Roughness of the Chang’E-6 Lunar Samples and Landing Site from Submicrometer to Kilometer Scales: Implications for Lunar Surface Processes and Remote Sensing Data Modeling

  • Authors: Jun Du, Jianxin Tian, Yang Liu, Chenxiang Li, Yazhou Yang, Minge Liu, Huimin Shao, Mengyuan Zhang, Ding Nan, Dijun Guo, Yuchen Xu, Feng Zhang, Kaichang Di, Rui Wen, Shifeng Dai, Yongliao Zou

Jun Du et al 2026 The Astronomical Journal 171 .

  • Provider: AAS Journals

Caption: Figure 5.

Two-dimensional bidirectional slopes of the AFM (panel (a)), ALSCC (panel (b)), PCAM (panel (c)), LCAM (panel (d)), NAC (panel (e)), and SLDEM (panel (f)) ROIs. In panels (a)–(f), all white arrows point to craters or depressions. In panels (a)–(c), all red arrows point to rocks or particles. In panels (e) and (f), the orange arrows point to the wrinkle ridges. In panels (a)–(f), the solid arrows point to features that are discernible in both elevation and slope data, whereas the dashed ones denote those that are discernible in the elevation data but undetectable in the slope data.

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