中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatial Variability of Active Layer Thickness along the Qinghai-Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar

文献类型:期刊论文

作者Jia, Shichao2; Zhang, Tingjun2; Hao, Jiansheng1; Li, Chaoyue1; Michaelides, Roger3; Shao, Wanwan2; Wei, Sihao2; Wang, Kun2; Fan, Chengyan2
刊名REMOTE SENSING
出版日期2022-11-01
卷号14期号:21页码:16
关键词active layer thickness ground-penetrating radar Tibetan Plateau permafrost engineering
DOI10.3390/rs14215606
通讯作者Hao, Jiansheng(haojs@igsnrr.ac.cn)
英文摘要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% (R-2 = 0.52) of ALT variability. The statistical model shows that a difference of 10 degrees C.d in root 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.
WOS关键词THERMAL STATE ; WATER-CONTENT ; PERMAFROST ; VEGETATION ; CLIMATE ; BARROW ; DEPTH ; INDEX ; BASIN ; MAP
资助项目Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0903] ; Tibet Science and Technology Program[XZ202201ZY0011G]
WOS研究方向Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology
语种英语
WOS记录号WOS:000885809800001
出版者MDPI
资助机构Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Tibet Science and Technology Program
源URL[http://ir.igsnrr.ac.cn/handle/311030/187448]  
专题中国科学院地理科学与资源研究所
通讯作者Hao, Jiansheng
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China
2.Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
3.Washington Univ, Dept Earth & Planetary Sci, St Louis, MO 63130 USA
推荐引用方式
GB/T 7714
Jia, Shichao,Zhang, Tingjun,Hao, Jiansheng,et al. Spatial Variability of Active Layer Thickness along the Qinghai-Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar[J]. REMOTE SENSING,2022,14(21):16.
APA Jia, Shichao.,Zhang, Tingjun.,Hao, Jiansheng.,Li, Chaoyue.,Michaelides, Roger.,...&Fan, Chengyan.(2022).Spatial Variability of Active Layer Thickness along the Qinghai-Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar.REMOTE SENSING,14(21),16.
MLA Jia, Shichao,et al."Spatial Variability of Active Layer Thickness along the Qinghai-Tibet Engineering Corridor Resolved Using Ground-Penetrating Radar".REMOTE SENSING 14.21(2022):16.

入库方式: OAI收割

来源:地理科学与资源研究所

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