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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 A8.

Diagrams illustrating the procedure used to evaluate the fidelity of interpolated surface elevations. In panel (a), the original (blue) elevation data have a uniform resolution. In panel (b), the resolution of the densified (red) elevation data decreases from top to bottom, which mimics the resolution of elevation data in a simple cylindrical projection. In panel (c), the interpolated (green) elevation data were obtained by interpolating the densified elevation data to the resolution of the original elevation data. In panel (d), a flowchart summarizes the procedure, where xori and xdensi denote the x-coordinates of the original and densified elevations, hori, hdensi, and hinterp represent the original, densified, and interpolated elevations, and fori and fdensi indicate the relations (denoted by “func”) between the x-coordinate and elevation for the original and densified datasets.

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