Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique

The land surface temperature obtained from remote sensing was widely used in the simulation of permafrost mapping instead of air temperature with the rapid development of remote sensing technology. The land surface freezing and thawing index (LFI and LTI), which is commonly regarded as the ground su...

Full description

Bibliographic Details
Main Authors: Shen Ma, Jingyi Zhao, Ji Chen, Shouhong Zhang, Tianchun Dong, Qihang Mei, Xin Hou, Guojun Liu
Format: Article
Language:English
Published: MDPI AG 2022-12-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/15/1/208
_version_ 1827617232394387456
author Shen Ma
Jingyi Zhao
Ji Chen
Shouhong Zhang
Tianchun Dong
Qihang Mei
Xin Hou
Guojun Liu
author_facet Shen Ma
Jingyi Zhao
Ji Chen
Shouhong Zhang
Tianchun Dong
Qihang Mei
Xin Hou
Guojun Liu
author_sort Shen Ma
collection DOAJ
description The land surface temperature obtained from remote sensing was widely used in the simulation of permafrost mapping instead of air temperature with the rapid development of remote sensing technology. The land surface freezing and thawing index (LFI and LTI), which is commonly regarded as the ground surface freezing and thawing index (GFI and GTI), can produce certain errors in the simulation of permafrost distribution on the Qinghai–Tibet Plateau. This paper improved the accuracy of the thermal condition of the surface soil in the Qinghai–Tibet Engineering Corridor (QTEC) by calculating the LFI (or LTI) and N-factors. The environmental factors affecting the spatial distribution of the GFI and GTI were detected by the GeoDetector model. Finally, the multiple linear relationships between the GFI (or GTI) and the environmental factors were established. The results from 25 monitoring sites in the QTEC show that the <i>N<sub>f</sub></i> (ratio of GFI to LFI) is 1.088, and the <i>N<sub>t</sub></i> (ratio of GTI to LTI) is 0.554. The explanatory power of the interaction between elevation and latitude for the GFI and GTI is 79.3% and 85.6%, respectively. The multiple linear regression model with six explanatory variables established by GFI (or GTI) has good accuracy. This study can provide relatively accurate upper boundary conditions for the simulation of permafrost distribution in the QTEC region.
first_indexed 2024-03-09T09:41:56Z
format Article
id doaj.art-af3f20ad426b487fb1f355a9417dc553
institution Directory Open Access Journal
issn 2072-4292
language English
last_indexed 2024-03-09T09:41:56Z
publishDate 2022-12-01
publisher MDPI AG
record_format Article
series Remote Sensing
spelling doaj.art-af3f20ad426b487fb1f355a9417dc5532023-12-02T00:51:43ZengMDPI AGRemote Sensing2072-42922022-12-0115120810.3390/rs15010208Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector TechniqueShen Ma0Jingyi Zhao1Ji Chen2Shouhong Zhang3Tianchun Dong4Qihang Mei5Xin Hou6Guojun Liu7Beiluhe Observation and Research Station of Frozen Soil Engineering and Environment, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaBeiluhe Observation and Research Station of Frozen Soil Engineering and Environment, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaBeiluhe Observation and Research Station of Frozen Soil Engineering and Environment, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaChina Railway Qinghai-Tibet Group Co., Ltd., Xining 810007, ChinaChina Railway Qinghai-Tibet Group Co., Ltd., Xining 810007, ChinaBeiluhe Observation and Research Station of Frozen Soil Engineering and Environment, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaBeiluhe Observation and Research Station of Frozen Soil Engineering and Environment, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaBeiluhe Observation and Research Station of Frozen Soil Engineering and Environment, State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, ChinaThe land surface temperature obtained from remote sensing was widely used in the simulation of permafrost mapping instead of air temperature with the rapid development of remote sensing technology. The land surface freezing and thawing index (LFI and LTI), which is commonly regarded as the ground surface freezing and thawing index (GFI and GTI), can produce certain errors in the simulation of permafrost distribution on the Qinghai–Tibet Plateau. This paper improved the accuracy of the thermal condition of the surface soil in the Qinghai–Tibet Engineering Corridor (QTEC) by calculating the LFI (or LTI) and N-factors. The environmental factors affecting the spatial distribution of the GFI and GTI were detected by the GeoDetector model. Finally, the multiple linear relationships between the GFI (or GTI) and the environmental factors were established. The results from 25 monitoring sites in the QTEC show that the <i>N<sub>f</sub></i> (ratio of GFI to LFI) is 1.088, and the <i>N<sub>t</sub></i> (ratio of GTI to LTI) is 0.554. The explanatory power of the interaction between elevation and latitude for the GFI and GTI is 79.3% and 85.6%, respectively. The multiple linear regression model with six explanatory variables established by GFI (or GTI) has good accuracy. This study can provide relatively accurate upper boundary conditions for the simulation of permafrost distribution in the QTEC region.https://www.mdpi.com/2072-4292/15/1/208ground surface freezing indexground surface thawing indexN-factorsGeoDetectorthe multiple linear regression modelQinghai–Tibet Engineering Corridor
spellingShingle Shen Ma
Jingyi Zhao
Ji Chen
Shouhong Zhang
Tianchun Dong
Qihang Mei
Xin Hou
Guojun Liu
Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique
Remote Sensing
ground surface freezing index
ground surface thawing index
N-factors
GeoDetector
the multiple linear regression model
Qinghai–Tibet Engineering Corridor
title Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique
title_full Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique
title_fullStr Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique
title_full_unstemmed Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique
title_short Ground Surface Freezing and Thawing Index Distribution in the Qinghai-Tibet Engineering Corridor and Factors Analysis Based on GeoDetector Technique
title_sort ground surface freezing and thawing index distribution in the qinghai tibet engineering corridor and factors analysis based on geodetector technique
topic ground surface freezing index
ground surface thawing index
N-factors
GeoDetector
the multiple linear regression model
Qinghai–Tibet Engineering Corridor
url https://www.mdpi.com/2072-4292/15/1/208
work_keys_str_mv AT shenma groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT jingyizhao groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT jichen groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT shouhongzhang groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT tianchundong groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT qihangmei groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT xinhou groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique
AT guojunliu groundsurfacefreezingandthawingindexdistributionintheqinghaitibetengineeringcorridorandfactorsanalysisbasedongeodetectortechnique