Articles | Volume 24, issue 3
https://doi.org/10.5194/hess-24-1145-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-24-1145-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Understanding the effects of climate warming on streamflow and active groundwater storage in an alpine catchment: the upper Lhasa River
Lu Lin
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, People's Republic of China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, People's Republic of China
Man Gao
Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, People's Republic of China
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, People's Republic of China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, People's Republic of China
Jiarong Wang
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, People's Republic of China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, People's Republic of China
Shuhong Wang
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, People's Republic of China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, People's Republic of China
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, People's Republic of China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, People's Republic of China
Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, People's Republic of China
Linze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou 730000, People's Republic of China
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- Solid Water Melt Dominates the Increase of Total Groundwater Storage in the Tibetan Plateau Y. Zou et al. 10.1029/2022GL100092
- Characteristics of Soil Temperature Change in Lhasa in the Face of Climate Change M. Jia et al. 10.3390/atmos15040450
- Permafrost on the Tibetan Plateau is degrading: Historical and projected trends T. Shen et al. 10.1016/j.jhydrol.2023.130501
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- Climate and landscape controls on spatio-temporal patterns of stream water stable isotopes in a large glacierized mountain basin on the Tibetan Plateau M. Gao et al. 10.1016/j.scitotenv.2020.144799
27 citations as recorded by crossref.
- Can we use precipitation isotope outputs of isotopic general circulation models to improve hydrological modeling in large mountainous catchments on the Tibetan Plateau? Y. Nan et al. 10.5194/hess-25-6151-2021
- Quantifying the impacts of climate change and human activities on runoff and suspended sediment load in the Lhasa River Basin, Tibetan Plateau W. Zhang et al. 10.1002/esp.5917
- Revealing temporal variation of baseflow and its underlying causes in the source region of the Yangtze River (China) G. Wu et al. 10.2166/nh.2024.185
- Characterizing 4 decades of accelerated glacial mass loss in the west Nyainqentanglha Range of the Tibetan Plateau S. Wang et al. 10.5194/hess-27-933-2023
- Reconstructing groundwater storage variations from GRACE observations using a new Gaussian-Han-Fan (GHF) smoothing approach F. Fatolazadeh & K. Goïta 10.1016/j.jhydrol.2021.127234
- An improved method to estimate the rate of change of streamflow recession and basin synthetic recession parameters from hydrographs M. Gao et al. 10.1016/j.jhydrol.2021.127254
- Spatial variability of runoff recharge sources and influence mechanisms in an arid mountain flow‐producing zone L. Sang et al. 10.1002/hyp.14642
- Understanding the hydrological regime based on the runoff events in a mountainous catchment with seasonally frozen soil in the Qinghai‐Tibet plateau P. Lin et al. 10.1002/hyp.14716
- Evaluation of seasonal catchment dynamic storage components using an analytical streamflow duration curve model C. Huang & H. Yeh 10.1186/s42834-022-00161-8
- Terrestrial water storage regime and its change in the endorheic Tibetan Plateau L. Wang et al. 10.1016/j.scitotenv.2021.152729
- Development and evaluation of temperature-induced variable source area runoff generation model L. Guo et al. 10.1016/j.jhydrol.2022.127894
- Groundwater storage trend in headwater basins in different Brazilian regions V. Wojahn et al. 10.1007/s40899-024-01179-z
- Evolution trends and driving factors of groundwater storage, recharge, and discharge in the Qinghai-Tibet Plateau: Study progress and challenges P. Xu et al. 10.1016/j.jhydrol.2024.130815
- Increasing annual streamflow and groundwater storage in response to climate warming in the Yangtze River source region W. Yi et al. 10.1088/1748-9326/ac0f27
- A deep learning-based method for mapping alpine intermittent rivers and ephemeral streams of the Tibetan Plateau from Sentinel-1 time series and DEMs J. Fei et al. 10.1016/j.rse.2022.113271
- Significant regime shifts in historical water yield in the Upper Brahmaputra River basin H. Li et al. 10.5194/hess-26-6399-2022
- A probabilistic framework for robust master recession curve parameterization M. Gao et al. 10.1016/j.jhydrol.2023.129922
- Analysis of the Behavior of Groundwater Storage Systems at Different Time Scales in Basins of South Central Chile: A Study Based on Flow Recession Records V. Parra et al. 10.3390/w15142503
- Changes in nonlinearity and stability of streamflow recession characteristics under climate warming in a large glaciated basin of the Tibetan Plateau J. Wang et al. 10.5194/hess-26-3901-2022
- Solid Water Melt Dominates the Increase of Total Groundwater Storage in the Tibetan Plateau Y. Zou et al. 10.1029/2022GL100092
- Characteristics of Soil Temperature Change in Lhasa in the Face of Climate Change M. Jia et al. 10.3390/atmos15040450
- Permafrost on the Tibetan Plateau is degrading: Historical and projected trends T. Shen et al. 10.1016/j.jhydrol.2023.130501
- Impacts of elevational variability of climate and frozen ground on streamflow in a glacierized catchment in Tibetan Plateau M. Gao et al. 10.1016/j.jhydrol.2023.129312
- Glaciers determine the sensitivity of hydrological processes to perturbed climate in a large mountainous basin on the Tibetan Plateau Y. Nan & F. Tian 10.5194/hess-28-669-2024
- Impact of climate and NDVI changes on catchment storage–discharge dynamics in southern Taiwan C. Huang & H. Yeh 10.1080/02626667.2022.2114835
- Hydrochemistry of the Lhasa River, Tibetan Plateau: Spatiotemporal Variations of Major Ions Compositions and Controlling Factors Using Multivariate Statistical Approaches M. Zhu et al. 10.3390/w13243660
- Climate and landscape controls on spatio-temporal patterns of stream water stable isotopes in a large glacierized mountain basin on the Tibetan Plateau M. Gao et al. 10.1016/j.scitotenv.2020.144799
Latest update: 25 Dec 2024
Short summary
In this paper, recession flow analysis – assuming nonlinearized outflow from aquifers into streams – was used to quantify active groundwater storage in a headwater catchment with high glacierization and large-scale frozen ground on the Tibetan Plateau. Hence, this work provides a perspective to clarify the impact of glacial retreat and frozen ground degradation due to climate change on hydrological processes.
In this paper, recession flow analysis – assuming nonlinearized outflow from aquifers into...