Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019

Since the 20th century, due to global warming, permafrost areas have undergone significant changes. The degradation of permafrost has complicated water cycle processes. Taking the upper Yellow River basin (UYRB) as a demonstration, this study discusses the long-term (1960–2019) changes in frozen gro...

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Main Authors: Lei Song, Lei Wang, Jing Zhou, Dongliang Luo, Xiuping Li
Format: Article
Language:English
Published: IOP Publishing 2022-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aca4eb
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author Lei Song
Lei Wang
Jing Zhou
Dongliang Luo
Xiuping Li
author_facet Lei Song
Lei Wang
Jing Zhou
Dongliang Luo
Xiuping Li
author_sort Lei Song
collection DOAJ
description Since the 20th century, due to global warming, permafrost areas have undergone significant changes. The degradation of permafrost has complicated water cycle processes. Taking the upper Yellow River basin (UYRB) as a demonstration, this study discusses the long-term (1960–2019) changes in frozen ground and their hydrological effects with a cryosphere-hydrology model, in particular a permafrost version of the water and energy budget-based distributed hydrological model. The permafrost at the UYRB, with thickening active layer and lengthening thawing duration, has degraded by 10.8%. The seasonally frozen ground has a more pronounced intra-annual regulation that replenishes surface runoff in the warm season, while the degradation of permafrost leads to a runoff increase. The occurrence of extreme events at the UYRB has gradually decreased with the degradation of frozen ground, but spring droughts and autumn floods become more serious. The results may help better understand the hydrological impacts of permafrost degradation in the Tibetan Plateau.
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spelling doaj.art-c73b470e030c4542a23567a4976f7df22023-08-09T15:20:09ZengIOP PublishingEnvironmental Research Letters1748-93262022-01-01171212403810.1088/1748-9326/aca4ebDivergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019Lei Song0https://orcid.org/0000-0002-7176-5882Lei Wang1Jing Zhou2Dongliang Luo3Xiuping Li4State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences , Beijing 100101, People’s Republic of China; University of Chinese Academy of Sciences , Beijing, People’s Republic of China; PIESAT Information Technology Co., Ltd , Beijing, People’s Republic of ChinaState Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences , Beijing 100101, People’s Republic of China; University of Chinese Academy of Sciences , Beijing, People’s Republic of ChinaState Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences , Beijing 100101, People’s Republic of ChinaState Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences , Lanzhou, People’s Republic of ChinaState Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences , Beijing 100101, People’s Republic of ChinaSince the 20th century, due to global warming, permafrost areas have undergone significant changes. The degradation of permafrost has complicated water cycle processes. Taking the upper Yellow River basin (UYRB) as a demonstration, this study discusses the long-term (1960–2019) changes in frozen ground and their hydrological effects with a cryosphere-hydrology model, in particular a permafrost version of the water and energy budget-based distributed hydrological model. The permafrost at the UYRB, with thickening active layer and lengthening thawing duration, has degraded by 10.8%. The seasonally frozen ground has a more pronounced intra-annual regulation that replenishes surface runoff in the warm season, while the degradation of permafrost leads to a runoff increase. The occurrence of extreme events at the UYRB has gradually decreased with the degradation of frozen ground, but spring droughts and autumn floods become more serious. The results may help better understand the hydrological impacts of permafrost degradation in the Tibetan Plateau.https://doi.org/10.1088/1748-9326/aca4ebcryosphere-hydrology modelfrozen groundrunoffsoil temperature and moistureupper Yellow River basinTibetan Plateau
spellingShingle Lei Song
Lei Wang
Jing Zhou
Dongliang Luo
Xiuping Li
Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019
Environmental Research Letters
cryosphere-hydrology model
frozen ground
runoff
soil temperature and moisture
upper Yellow River basin
Tibetan Plateau
title Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019
title_full Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019
title_fullStr Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019
title_full_unstemmed Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019
title_short Divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of Tibetan Plateau during 1960–2019
title_sort divergent runoff impacts of permafrost and seasonally frozen ground at a large river basin of tibetan plateau during 1960 2019
topic cryosphere-hydrology model
frozen ground
runoff
soil temperature and moisture
upper Yellow River basin
Tibetan Plateau
url https://doi.org/10.1088/1748-9326/aca4eb
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AT jingzhou divergentrunoffimpactsofpermafrostandseasonallyfrozengroundatalargeriverbasinoftibetanplateauduring19602019
AT dongliangluo divergentrunoffimpactsofpermafrostandseasonallyfrozengroundatalargeriverbasinoftibetanplateauduring19602019
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