Articles | Volume 12, issue 2
https://doi.org/10.5194/tc-12-657-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-12-657-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Change in frozen soils and its effect on regional hydrology, upper Heihe basin, northeastern Qinghai–Tibetan Plateau
School of Water Resources and Environment, China University of
Geosciences, Beijing 100083, China
Dawen Yang
CORRESPONDING AUTHOR
State Key Laboratory of Hydroscience and Engineering, Department of
Hydraulic Engineering, Tsinghua University, Beijing 100084, China
Yue Qin
State Key Laboratory of Hydroscience and Engineering, Department of
Hydraulic Engineering, Tsinghua University, Beijing 100084, China
Yuhan Wang
State Key Laboratory of Hydroscience and Engineering, Department of
Hydraulic Engineering, Tsinghua University, Beijing 100084, China
Hongyi Li
Cold and Arid Regions Environmental and Engineering Research
Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Yanlin Zhang
Cold and Arid Regions Environmental and Engineering Research
Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Tingjun Zhang
Key Laboratory of West China's Environmental Systems (MOE), College
of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000,
China
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111 citations as recorded by crossref.
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- Unsustainable water supply from thawing permafrost on the Tibetan Plateau in a changing climate T. Wang et al. 10.1016/j.scib.2023.04.037
- Pervasive Permafrost Thaw Exacerbates Future Risk of Water Shortage Across the Tibetan Plateau T. Wang et al. 10.1029/2022EF003463
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- Hydrothermal variations in soils resulting from the freezing and thawing processes in the active layer of an alpine grassland in the Qilian Mountains, northeastern Tibetan Plateau Q. Wang et al. 10.1007/s00704-018-2529-y
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- Application of an improved distributed hydrological model based on the soil–gravel structure in the Niyang River basin, Qinghai–Tibet Plateau P. Wang et al. 10.5194/hess-27-2681-2023
- Impacts of seasonally frozen soil hydrothermal dynamics on the watershed hydrological processes inferred from a spatially distributed numerical modelling approach H. Gao et al. 10.1016/j.jhydrol.2023.129947
- Integrated hydrometeorological, snow and frozen-ground observations in the alpine region of the Heihe River Basin, China T. Che et al. 10.5194/essd-11-1483-2019
- Three in one: GPS-IR measurements of ground surface elevation changes, soil moisture, and snow depth at a permafrost site in the northeastern Qinghai–Tibet Plateau J. Zhang et al. 10.5194/tc-15-3021-2021
- Using hydrogeochemical data to trace groundwater flow paths in a cold alpine catchment Y. Hu et al. 10.1002/hyp.13440
- Exploring the contribution of precipitation to water within the active layer during the thawing period in the permafrost regions of central Qinghai-Tibet Plateau by stable isotopic tracing X. Zhu et al. 10.1016/j.scitotenv.2019.01.064
- Remote sensing spatiotemporal patterns of frozen soil and the environmental controls over the Tibetan Plateau during 2002–2016 G. Zheng et al. 10.1016/j.rse.2020.111927
- Partitioning the contributions of cryospheric change to the increase of streamflow on the Nu River Y. Yang et al. 10.1016/j.jhydrol.2021.126330
- Prediction of sediment transport capacity using thawed depth deduced from temperature measurement C. Shi et al. 10.1016/j.still.2020.104858
- Improving Permafrost Physics in a Distributed Cryosphere‐Hydrology Model and Its Evaluations at the Upper Yellow River Basin L. Song et al. 10.1029/2020JD032916
- Runoff and sediment effect of the soil-water conservation measures in a typical river basin of the Loess Plateau H. Yang et al. 10.1016/j.catena.2024.108218
- Understanding the Effects of Cold and Warm Season Air Warming on the Permafrost Hydrology Changes in the Source Region of the Lancang River, the Qinghai‐Tibetan Plateau L. Xu & B. Gao 10.1029/2022JD036551
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Latest update: 06 Oct 2024
Short summary
This study developed a distributed hydrological model coupled with cryospherical processes and applied it in order to simulate the long-term change of frozen ground and its effect on hydrology in the upper Heihe basin. Results showed that the permafrost area shrank by 8.8%, and the frozen depth of seasonally frozen ground decreased. Runoff in cold seasons and annual liquid soil moisture increased due to frozen soils change. Groundwater recharge was enhanced due to the degradation of permafrost.
This study developed a distributed hydrological model coupled with cryospherical processes and...