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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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 |
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1724553320519958528 |