TY - JOUR
T1 - Millimeter- to Decimeter-Scale Surface Roughness of the Moon at the Chang'e-4 Exploration Region
AU - Guo, Dijun
AU - Fa, Wenzhe
AU - Wu, Bo
AU - Li, Yuan
AU - Liu, Yang
N1 - Funding Information:
The authors thank Hannah Susorney and Paul Helfenstein for their constructive and helpful comments. This work was supported partly by the National Natural Science Foundation of China (No. 41941002, 41902317, 41773065, 11941001), B‐type Strategic Priority Program of the Chinese Academy of Sciences (No. XDB41000000), China Postdoctoral Science Foundation (No. 2019M650319), and the Research Grants Council of Hong Kong (RIF Project No: R5043‐19).
Publisher Copyright:
© 2021. American Geophysical Union. All Rights Reserved.
PY - 2021/10/16
Y1 - 2021/10/16
N2 - The surface slope and roughness of the Moon have been investigated extensively over a wide baseline range except millimeter to decimeter scales. In this study, we present for the first time millimeter-to decimeter-scale surface slope and roughness of the Moon at China's Chang'e-4 landing regions (∼20 m across) using the Digital Terrain Model (DTM) with a resolution of 5 mm/pixel. The bidirectional slope at the 7 mm scale can be larger than 40° with a median value of ∼10°. The root-mean-square (RMS) height within a window size of 125 mm varies from ∼1 mm to ∼18 mm with a median value of ∼4 mm. Both the bidirectional slope and RMS height show scale-dependent behaviors and the parameter of scale dependence, the Hurst exponent, is ∼0.6–0.85. We also synthesized the bidirectional slope at baseline from micrometer to kilometer, showing that bidirectional slope decreases from ∼60° at micrometer to ∼1° at a kilometer. At millimeter-scale, surface roughness is mainly controlled by small impact craters, rocks, and regolith properties. Our roughness results not only bridge the gap in understanding surface roughness from traditional topographic data sets to radar and thermal observations, but also provide valuable information about lunar regolith characteristics, and small-scale geological processes.
AB - The surface slope and roughness of the Moon have been investigated extensively over a wide baseline range except millimeter to decimeter scales. In this study, we present for the first time millimeter-to decimeter-scale surface slope and roughness of the Moon at China's Chang'e-4 landing regions (∼20 m across) using the Digital Terrain Model (DTM) with a resolution of 5 mm/pixel. The bidirectional slope at the 7 mm scale can be larger than 40° with a median value of ∼10°. The root-mean-square (RMS) height within a window size of 125 mm varies from ∼1 mm to ∼18 mm with a median value of ∼4 mm. Both the bidirectional slope and RMS height show scale-dependent behaviors and the parameter of scale dependence, the Hurst exponent, is ∼0.6–0.85. We also synthesized the bidirectional slope at baseline from micrometer to kilometer, showing that bidirectional slope decreases from ∼60° at micrometer to ∼1° at a kilometer. At millimeter-scale, surface roughness is mainly controlled by small impact craters, rocks, and regolith properties. Our roughness results not only bridge the gap in understanding surface roughness from traditional topographic data sets to radar and thermal observations, but also provide valuable information about lunar regolith characteristics, and small-scale geological processes.
KW - Chang'e-4
KW - regolith
KW - the Moon
KW - topographic roughness
UR - http://www.scopus.com/inward/record.url?scp=85116818902&partnerID=8YFLogxK
U2 - 10.1029/2021GL094931
DO - 10.1029/2021GL094931
M3 - Journal article
AN - SCOPUS:85116818902
SN - 0094-8276
VL - 48
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 19
M1 - e2021GL094931
ER -