Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar

Active layer thickness (ALT) is a sensitive indicator of response to climate change. ALT has important influence on various aspects of the regional environment such as hydrological processes and vegetation. In this study, 57 ground-penetrating radar (GPR) sections were surveyed along the Qinghai–Tib...

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Published in:Remote Sensing
Main Authors: Shichao Jia, Tingjun Zhang, Jiansheng Hao, Chaoyue Li, Roger Michaelides, Wanwan Shao, Sihao Wei, Kun Wang, Chengyan Fan
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
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Online Access:https://doi.org/10.3390/rs14215606
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spelling ftmdpi:oai:mdpi.com:/2072-4292/14/21/5606/ 2023-08-20T03:59:06+02:00 Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar Shichao Jia Tingjun Zhang Jiansheng Hao Chaoyue Li Roger Michaelides Wanwan Shao Sihao Wei Kun Wang Chengyan Fan agris 2022-11-07 application/pdf https://doi.org/10.3390/rs14215606 EN eng Multidisciplinary Digital Publishing Institute Engineering Remote Sensing https://dx.doi.org/10.3390/rs14215606 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 21; Pages: 5606 active layer thickness ground-penetrating radar Tibetan Plateau permafrost engineering Text 2022 ftmdpi https://doi.org/10.3390/rs14215606 2023-08-01T07:13:21Z Active layer thickness (ALT) is a sensitive indicator of response to climate change. ALT has important influence on various aspects of the regional environment such as hydrological processes and vegetation. In this study, 57 ground-penetrating radar (GPR) sections were surveyed along the Qinghai–Tibet Engineering Corridor (QTEC) during 2018–2021, covering a total length of 58.5 km. The suitability of GPR-derived ALT was evaluated using in situ measurements and reference datasets, for which the bias and root mean square error were approximately −0.16 and 0.43 m, respectively. The GPR results show that the QTEC ALT was in the range of 1.25–6.70 m (mean: 2.49 ± 0.57 m). Observed ALT demonstrated pronounced spatial variability at both regional and fine scales. We developed a statistical estimation model that explicitly considers the soil thermal regime (i.e., ground thawing index, TIg), soil properties, and vegetation. This model was found suitable for simulating ALT over the QTEC, and it could explain 52% (R2 = 0.52) of ALT variability. The statistical model shows that a difference of 10 °C.d in TIg is equivalent to a change of 0.67 m in ALT, and an increase of 0.1 in the normalized difference vegetation index (NDVI) is equivalent to a decrease of 0.23 m in ALT. The fine-scale (<1 km) variation in ALT could account for 77.6% of the regional-scale (approximately 550 km) variation. These results provide a timely ALT benchmark along the QTEC, which can inform the construction and maintenance of engineering facilities along the QTEC. Text Active layer thickness permafrost MDPI Open Access Publishing Remote Sensing 14 21 5606
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic active layer thickness
ground-penetrating radar
Tibetan Plateau
permafrost
engineering
spellingShingle active layer thickness
ground-penetrating radar
Tibetan Plateau
permafrost
engineering
Shichao Jia
Tingjun Zhang
Jiansheng Hao
Chaoyue Li
Roger Michaelides
Wanwan Shao
Sihao Wei
Kun Wang
Chengyan Fan
Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar
topic_facet active layer thickness
ground-penetrating radar
Tibetan Plateau
permafrost
engineering
description Active layer thickness (ALT) is a sensitive indicator of response to climate change. ALT has important influence on various aspects of the regional environment such as hydrological processes and vegetation. In this study, 57 ground-penetrating radar (GPR) sections were surveyed along the Qinghai–Tibet Engineering Corridor (QTEC) during 2018–2021, covering a total length of 58.5 km. The suitability of GPR-derived ALT was evaluated using in situ measurements and reference datasets, for which the bias and root mean square error were approximately −0.16 and 0.43 m, respectively. The GPR results show that the QTEC ALT was in the range of 1.25–6.70 m (mean: 2.49 ± 0.57 m). Observed ALT demonstrated pronounced spatial variability at both regional and fine scales. We developed a statistical estimation model that explicitly considers the soil thermal regime (i.e., ground thawing index, TIg), soil properties, and vegetation. This model was found suitable for simulating ALT over the QTEC, and it could explain 52% (R2 = 0.52) of ALT variability. The statistical model shows that a difference of 10 °C.d in TIg is equivalent to a change of 0.67 m in ALT, and an increase of 0.1 in the normalized difference vegetation index (NDVI) is equivalent to a decrease of 0.23 m in ALT. The fine-scale (<1 km) variation in ALT could account for 77.6% of the regional-scale (approximately 550 km) variation. These results provide a timely ALT benchmark along the QTEC, which can inform the construction and maintenance of engineering facilities along the QTEC.
format Text
author Shichao Jia
Tingjun Zhang
Jiansheng Hao
Chaoyue Li
Roger Michaelides
Wanwan Shao
Sihao Wei
Kun Wang
Chengyan Fan
author_facet Shichao Jia
Tingjun Zhang
Jiansheng Hao
Chaoyue Li
Roger Michaelides
Wanwan Shao
Sihao Wei
Kun Wang
Chengyan Fan
author_sort Shichao Jia
title Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar
title_short Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar
title_full Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar
title_fullStr Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar
title_full_unstemmed Spatial Variability of Active Layer Thickness along the Qinghai–Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar
title_sort spatial variability of active layer thickness along the qinghai–tibet engineering corridor resolved using ground-penetrating radar
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/rs14215606
op_coverage agris
genre Active layer thickness
permafrost
genre_facet Active layer thickness
permafrost
op_source Remote Sensing; Volume 14; Issue 21; Pages: 5606
op_relation Engineering Remote Sensing
https://dx.doi.org/10.3390/rs14215606
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs14215606
container_title Remote Sensing
container_volume 14
container_issue 21
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