Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains

Permafrost degradation has been widely reported on the Tibetan Plateau (TP). However, directly observed evidence of permafrost thawing processes and degradation rates are very limited, although it is expected to be prevalent near the periphery of a permafrost area. Here, we report permafrost changes...

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Main Authors: Wen Sun, Tingjun Zhang, Gary D. Clow, Yan-Hua Sun, Wen-Yu Zhao, Ben-Ben Liang, Cheng-Yan Fan, Xiao-Qing Peng, Bin Cao
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2022-10-01
Series:Advances in Climate Change Research
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674927822000867
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author Wen Sun
Tingjun Zhang
Gary D. Clow
Yan-Hua Sun
Wen-Yu Zhao
Ben-Ben Liang
Cheng-Yan Fan
Xiao-Qing Peng
Bin Cao
author_facet Wen Sun
Tingjun Zhang
Gary D. Clow
Yan-Hua Sun
Wen-Yu Zhao
Ben-Ben Liang
Cheng-Yan Fan
Xiao-Qing Peng
Bin Cao
author_sort Wen Sun
collection DOAJ
description Permafrost degradation has been widely reported on the Tibetan Plateau (TP). However, directly observed evidence of permafrost thawing processes and degradation rates are very limited, although it is expected to be prevalent near the periphery of a permafrost area. Here, we report permafrost changes and disappearance in the Qilian Mountains (northeastern TP) based on three boreholes instrumented along a 100 m transect during 2014–2021. Our results show that permafrost has significantly degraded in the study area: the mean downward thawing rate from the permafrost table was about 0.16 m per year while the mean upward thawing rate from the permafrost base was about 0.23 m per year. We estimate the mean lateral degradation rate of permafrost in this area was ∼4.14 m per year. More dramatically, the 1.5 m thick permafrost layer at one of the boreholes thawed completely between April of 2018 and December of 2019. Our results indicate that changes in climatic condition may have played only a limited role in controlling the active layer thickness in the vicinity of the altitudinal limit of permafrost; moisture content and soil conditions play key roles in site-specific permafrost thawing. This study provides new quantitative insights for understanding changes near the altitudinal limit of permafrost, and we suggest that land surface models or Earth system model studies of the lateral heat exchanges should be implemented in order to better represent permafrost thawing processes.
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spelling doaj.art-0ce5ff429b124dbbbd96aa31daefc5072022-12-22T02:23:42ZengKeAi Communications Co., Ltd.Advances in Climate Change Research1674-92782022-10-01135642650Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian MountainsWen Sun0Tingjun Zhang1Gary D. Clow2Yan-Hua Sun3Wen-Yu Zhao4Ben-Ben Liang5Cheng-Yan Fan6Xiao-Qing Peng7Bin Cao8Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, ChinaKey Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Corresponding author.Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder 80303, USAKey Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, ChinaKey Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, ChinaKey Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, ChinaKey Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, ChinaKey Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, ChinaNational Tibetan Plateau Data Center, Key Laboratory of Tibetan Environmental Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Corresponding author.Permafrost degradation has been widely reported on the Tibetan Plateau (TP). However, directly observed evidence of permafrost thawing processes and degradation rates are very limited, although it is expected to be prevalent near the periphery of a permafrost area. Here, we report permafrost changes and disappearance in the Qilian Mountains (northeastern TP) based on three boreholes instrumented along a 100 m transect during 2014–2021. Our results show that permafrost has significantly degraded in the study area: the mean downward thawing rate from the permafrost table was about 0.16 m per year while the mean upward thawing rate from the permafrost base was about 0.23 m per year. We estimate the mean lateral degradation rate of permafrost in this area was ∼4.14 m per year. More dramatically, the 1.5 m thick permafrost layer at one of the boreholes thawed completely between April of 2018 and December of 2019. Our results indicate that changes in climatic condition may have played only a limited role in controlling the active layer thickness in the vicinity of the altitudinal limit of permafrost; moisture content and soil conditions play key roles in site-specific permafrost thawing. This study provides new quantitative insights for understanding changes near the altitudinal limit of permafrost, and we suggest that land surface models or Earth system model studies of the lateral heat exchanges should be implemented in order to better represent permafrost thawing processes.http://www.sciencedirect.com/science/article/pii/S1674927822000867PermafrostPermafrost degradationPermafrost lateral thawingQilian Mountains
spellingShingle Wen Sun
Tingjun Zhang
Gary D. Clow
Yan-Hua Sun
Wen-Yu Zhao
Ben-Ben Liang
Cheng-Yan Fan
Xiao-Qing Peng
Bin Cao
Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains
Advances in Climate Change Research
Permafrost
Permafrost degradation
Permafrost lateral thawing
Qilian Mountains
title Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains
title_full Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains
title_fullStr Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains
title_full_unstemmed Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains
title_short Observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the Qilian Mountains
title_sort observed permafrost thawing and disappearance near the altitudinal limit of permafrost in the qilian mountains
topic Permafrost
Permafrost degradation
Permafrost lateral thawing
Qilian Mountains
url http://www.sciencedirect.com/science/article/pii/S1674927822000867
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