Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar

The Lunar Penetrating Radar (LPR) carried by the Chang’E-3 (CE-3) and Chang’E-4 (CE-4) mission plays a very important role in lunar exploration. The dual-frequency radar on the rover (DFR) provides a meaningful opportunity to detect the underground structure of the CE-3 landing s...

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Main Authors: Chenyang Xu, Gongbo Zhang, Jianmin Zhang, Zhuo Jia
Format: Article
Language:English
Published: MDPI AG 2020-01-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/10/2/535
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spelling doaj-b1bc0668deb148afb332e423ba61371d2020-11-25T03:35:38ZengMDPI AGApplied Sciences2076-34172020-01-0110253510.3390/app10020535app10020535Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating RadarChenyang Xu0Gongbo Zhang1Jianmin Zhang2Zhuo Jia3College of Geo-exploration Science and Technology, Jilin University, Changchun 130026, ChinaCollege of Geo-exploration Science and Technology, Jilin University, Changchun 130026, ChinaCollege of Geo-exploration Science and Technology, Jilin University, Changchun 130026, ChinaCollege of Geo-exploration Science and Technology, Jilin University, Changchun 130026, ChinaThe Lunar Penetrating Radar (LPR) carried by the Chang’E-3 (CE-3) and Chang’E-4 (CE-4) mission plays a very important role in lunar exploration. The dual-frequency radar on the rover (DFR) provides a meaningful opportunity to detect the underground structure of the CE-3 landing site. The low-frequency channel (channel 1) maps the underground structure to a depth of several hundred meters, while the high-frequency channel (channel 2) can observe the stratigraphic structure of gravel near the surface. As the low-frequency radar image is troubled by unknown noise, time−frequency analysis of a single trace is applied. Then, a method named complete ensemble empirical mode decomposition (CEEMD) is conducted to decompose the channel 1 data, and the Hilbert transform gives us the chance for further data analysis. Finally, combined with regional geology, previous studies, and channel 2 data, a usability analysis of LPR channel 1 data provides a reference for the availability of the CE-4 LPR data.https://www.mdpi.com/2076-3417/10/2/535lunar penetrating radardata analysiscomplete ensemble empirical mode decomposition (ceemd)hilbert transform
collection DOAJ
language English
format Article
sources DOAJ
author Chenyang Xu
Gongbo Zhang
Jianmin Zhang
Zhuo Jia
spellingShingle Chenyang Xu
Gongbo Zhang
Jianmin Zhang
Zhuo Jia
Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar
Applied Sciences
lunar penetrating radar
data analysis
complete ensemble empirical mode decomposition (ceemd)
hilbert transform
author_facet Chenyang Xu
Gongbo Zhang
Jianmin Zhang
Zhuo Jia
author_sort Chenyang Xu
title Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar
title_short Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar
title_full Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar
title_fullStr Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar
title_full_unstemmed Time–Frequency Attribute Analysis of Channel 1 Data of Lunar Penetrating Radar
title_sort time–frequency attribute analysis of channel 1 data of lunar penetrating radar
publisher MDPI AG
series Applied Sciences
issn 2076-3417
publishDate 2020-01-01
description The Lunar Penetrating Radar (LPR) carried by the Chang’E-3 (CE-3) and Chang’E-4 (CE-4) mission plays a very important role in lunar exploration. The dual-frequency radar on the rover (DFR) provides a meaningful opportunity to detect the underground structure of the CE-3 landing site. The low-frequency channel (channel 1) maps the underground structure to a depth of several hundred meters, while the high-frequency channel (channel 2) can observe the stratigraphic structure of gravel near the surface. As the low-frequency radar image is troubled by unknown noise, time−frequency analysis of a single trace is applied. Then, a method named complete ensemble empirical mode decomposition (CEEMD) is conducted to decompose the channel 1 data, and the Hilbert transform gives us the chance for further data analysis. Finally, combined with regional geology, previous studies, and channel 2 data, a usability analysis of LPR channel 1 data provides a reference for the availability of the CE-4 LPR data.
topic lunar penetrating radar
data analysis
complete ensemble empirical mode decomposition (ceemd)
hilbert transform
url https://www.mdpi.com/2076-3417/10/2/535
work_keys_str_mv AT chenyangxu timefrequencyattributeanalysisofchannel1dataoflunarpenetratingradar
AT gongbozhang timefrequencyattributeanalysisofchannel1dataoflunarpenetratingradar
AT jianminzhang timefrequencyattributeanalysisofchannel1dataoflunarpenetratingradar
AT zhuojia timefrequencyattributeanalysisofchannel1dataoflunarpenetratingradar
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