Articles | Volume 26, issue 14
https://doi.org/10.5194/hess-26-3901-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/hess-26-3901-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
28 Jul 2022
Research article |
| 28 Jul 2022
| 28 Jul 2022
Changes in nonlinearity and stability of streamflow recession characteristics under climate warming in a large glaciated basin of the Tibetan Plateau
Jiarong Wang
Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, P. R. China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, P. R. China
Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, P. R. China
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, P. R. China
Man Gao
Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, P. R. China
Qi Hu
School of Natural Resources and Department of Earth and Atmospheric Sciences, University of Nebraska–Lincoln, Lincoln, NE 68583, USA
Jintao Liu
College of Hydrology and Water Resources, Hohai University, Nanjing 210098, P. R. China
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Hydrol. Earth Syst. Sci., 24, 1145–1157, https://doi.org/10.5194/hess-24-1145-2020, https://doi.org/10.5194/hess-24-1145-2020, 2020
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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.
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We assessed and compared the glacier areal retreat rate and surface thinning rate and the effects of topography, debris cover and proglacial lakes in the west Nyainqentanglha Range (WNT) during 1976–2000 and 2000–2020. Our study will help us to better understand the glacier change characteristics in the WNT on a long timescale and will serve as a reference for glacier changes in other regions on the Tibetan Plateau.
Lu Lin, Man Gao, Jintao Liu, Jiarong Wang, Shuhong Wang, Xi Chen, and Hu Liu
Hydrol. Earth Syst. Sci., 24, 1145–1157, https://doi.org/10.5194/hess-24-1145-2020, https://doi.org/10.5194/hess-24-1145-2020, 2020
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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.
Zhongkai Li, Hu Liu, Wenzhi Zhao, Qiyue Yang, Rong Yang, and Jintao Liu
Hydrol. Earth Syst. Sci., 23, 4685–4706, https://doi.org/10.5194/hess-23-4685-2019, https://doi.org/10.5194/hess-23-4685-2019, 2019
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A database of soil moisture measurements from the middle Heihe River basin of China was used to test the potential of a soil moisture database in estimating the soil water balance components (SWBCs). We determined SWBCs using a method that combined the soil water balance method and the inverse Richards equation. This work confirmed that relatively reasonable estimations of the SWBCs in coarse-textured sandy soils can be derived using soil moisture measurements.
Man Gao, Xi Chen, and Jintao Liu
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-453, https://doi.org/10.5194/hess-2019-453, 2019
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We developed a new tracer-aided hydrological model for karst catchments. This model captured the flow and tracer dynamics within each landscape unit quite well, and we could estimate the storage, fluxes and age of water within each. Such tracer-aided models enhance our understanding of the hydrological connectivity between different landscape units and the mixing processes between various flow sources. It is an encouraging step forward in tracer-aided modelling of karst catchments.
Lu Lin, Man Gao, Jintao Liu, Xi Chen, and Hu Liu
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-541, https://doi.org/10.5194/hess-2018-541, 2018
Manuscript not accepted for further review
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In the paper, recession flow analysis assuming nonlinearized outflow from aquifers into streams was used to quantify active groundwater storage in a headwater catchment with larger glacierization and large-scale frozen ground on the Tibetan Plateau, which provides a perspective to clarify the way of glacial retreat and frozen ground degradation on hydrological processes. We are very grateful to all editors and reviewers for their efforts to help us improve the quality of the manuscript.
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Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-518, https://doi.org/10.5194/hess-2018-518, 2018
Manuscript not accepted for further review
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A database of soil moisture measurements was used to test the potential of a soil moisture database in estimating the SWBCs. Although the planting of the past decade have significantly increased the soils' water-holding ability, the magnitude of increase in most of the parameters was independent of the treatments. Significant variances were observed among the plots in both the cumulative irrigation volumes and deep drainages, and the ET demands for all the plots behaved pretty much the same.
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Hydrol. Earth Syst. Sci., 22, 2891–2901, https://doi.org/10.5194/hess-22-2891-2018, https://doi.org/10.5194/hess-22-2891-2018, 2018
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The spatial runoff is decomposed into a deterministic trend and deviations from it caused by stochastic fluctuations which are described by Budyko method and stochastic interpolation. This coupled method is applied to spatially interpolate runoff in the Huaihe River basin of China. Results show that the coupled method reduces the error in overestimating low runoff and underestimating high runoff suffered by the other two methods, so it improves the prediction accuracy of the mean annual runoff.
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Subject: Catchment hydrology | Techniques and Approaches: Mathematical applications
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Hydrol. Earth Syst. Sci., 26, 6339–6359, https://doi.org/10.5194/hess-26-6339-2022, https://doi.org/10.5194/hess-26-6339-2022, 2022
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Paul Royer-Gaspard, Vazken Andréassian, and Guillaume Thirel
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Wencong Yang, Hanbo Yang, Dawen Yang, and Aizhong Hou
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This study quantified the causal effects of land cover changes and dams on the changes in annual maximum discharges (Q) in 757 catchments of China using panel regressions. We found that a 1 % point increase in urban areas causes a 3.9 % increase in Q, and a 1 unit increase in reservoir index causes a 21.4 % decrease in Q for catchments with no dam before. This study takes the first step to explain the human-caused flood changes on a national scale in China.
Weifei Yang, Changlai Xiao, Zhihao Zhang, and Xiujuan Liang
Hydrol. Earth Syst. Sci., 25, 1747–1760, https://doi.org/10.5194/hess-25-1747-2021, https://doi.org/10.5194/hess-25-1747-2021, 2021
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This study analyzed the effectiveness of the conductivity mass balance (CMB) method for correcting the Eckhardt method. The results showed that the approach of calibrating the Eckhardt method against the CMB method provides a
falsecalibration of total baseflow by offsetting the inherent biases in the baseflow sequences generated by the two methods. The reason for this phenomenon is the baseflow series generated by the two methods containing different transient water sources.
Juliane Mai, James R. Craig, and Bryan A. Tolson
Hydrol. Earth Syst. Sci., 24, 5835–5858, https://doi.org/10.5194/hess-24-5835-2020, https://doi.org/10.5194/hess-24-5835-2020, 2020
James W. Kirchner and Julia L. A. Knapp
Hydrol. Earth Syst. Sci., 24, 5539–5558, https://doi.org/10.5194/hess-24-5539-2020, https://doi.org/10.5194/hess-24-5539-2020, 2020
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Ensemble hydrograph separation is a powerful new tool for measuring the age distribution of streamwater. However, the calculations are complex and may be difficult for researchers to implement on their own. Here we present scripts that perform these calculations in either MATLAB or R so that researchers do not need to write their own codes. We explain how these scripts work and how to use them. We demonstrate several potential applications using a synthetic catchment data set.
Antoine Allam, Roger Moussa, Wajdi Najem, and Claude Bocquillon
Hydrol. Earth Syst. Sci., 24, 4503–4521, https://doi.org/10.5194/hess-24-4503-2020, https://doi.org/10.5194/hess-24-4503-2020, 2020
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With serious concerns about global change rising in the Mediterranean, we established a new climatic classification to follow hydrological and ecohydrological activities. The classification coincided with a geographical distribution ranging from the most seasonal and driest class in the south to the least seasonal and most humid in the north. RCM scenarios showed that northern classes evolve to southern ones with shorter humid seasons and earlier snowmelt which might affect hydrologic regimes.
Mingguo Zheng
Hydrol. Earth Syst. Sci., 24, 2365–2378, https://doi.org/10.5194/hess-24-2365-2020, https://doi.org/10.5194/hess-24-2365-2020, 2020
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This paper developed a mathematically precise method to partition climate and catchment effects on streamflow. The method reveals that both the change magnitude and pathway (timing of change), not the magnitude alone, dictate the partition unless for a linear system. The method has wide relevance. For example, it suggests that the global warming effect of carbon emission is path dependent, and an optimal pathway would facilitate a higher global budget of carbon emission.
José Manuel Tunqui Neira, Vazken Andréassian, Gaëlle Tallec, and Jean-Marie Mouchel
Hydrol. Earth Syst. Sci., 24, 1823–1830, https://doi.org/10.5194/hess-24-1823-2020, https://doi.org/10.5194/hess-24-1823-2020, 2020
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This paper deals with the mathematical representation of concentration–discharge relationships. We propose a two-sided affine power scaling relationship (2S-APS) as an alternative to the classic one-sided power scaling relationship (commonly known as
power law). We also discuss the identification of the parameters of the proposed relationship, using an appropriate numerical criterion, based on high-frequency chemical time series of the Orgeval-ORACLE observatory.
Long Yang, Lachun Wang, Xiang Li, and Jie Gao
Hydrol. Earth Syst. Sci., 23, 5133–5149, https://doi.org/10.5194/hess-23-5133-2019, https://doi.org/10.5194/hess-23-5133-2019, 2019
Julia L. A. Knapp, Colin Neal, Alessandro Schlumpf, Margaret Neal, and James W. Kirchner
Hydrol. Earth Syst. Sci., 23, 4367–4388, https://doi.org/10.5194/hess-23-4367-2019, https://doi.org/10.5194/hess-23-4367-2019, 2019
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We describe, present, and make publicly available two extensive data sets of stable water isotopes in streamwater and precipitation at Plynlimon, Wales, consisting of measurements at 7-hourly intervals for 17 months and at weekly intervals for 4.25 years. We use these data to calculate new water fractions and transit time distributions for different discharge rates and seasons, thus quantifying the contribution of recent precipitation to streamflow under different conditions.
Hui-Min Wang, Jie Chen, Chong-Yu Xu, Hua Chen, Shenglian Guo, Ping Xie, and Xiangquan Li
Hydrol. Earth Syst. Sci., 23, 4033–4050, https://doi.org/10.5194/hess-23-4033-2019, https://doi.org/10.5194/hess-23-4033-2019, 2019
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When using large ensembles of global climate models in hydrological impact studies, there are pragmatic questions on whether it is necessary to weight climate models and how to weight them. We use eight methods to weight climate models straightforwardly, based on their performances in hydrological simulations, and investigate the influences of the assigned weights. This study concludes that using bias correction and equal weighting is likely viable and sufficient for hydrological impact studies.
Nathalie Folton, Eric Martin, Patrick Arnaud, Pierre L'Hermite, and Mathieu Tolsa
Hydrol. Earth Syst. Sci., 23, 2699–2714, https://doi.org/10.5194/hess-23-2699-2019, https://doi.org/10.5194/hess-23-2699-2019, 2019
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The long-term study of precipitation, flows, flood or drought mechanisms, in the Réal Collobrier research Watershed, located in South-East France, in the Mediterranean forest, improves knowledge of the water cycle and is unique tool for understanding of how catchments function. This study shows a small decrease in rainfall and a marked tendency towards a decrease in the water resources of the catchment in response to climate trends, with a consistent increase in drought severity and duration.
Vazken Andréassian and Tewfik Sari
Hydrol. Earth Syst. Sci., 23, 2339–2350, https://doi.org/10.5194/hess-23-2339-2019, https://doi.org/10.5194/hess-23-2339-2019, 2019
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In this Technical Note, we present two water balance formulas: the Turc–Mezentsev and Tixeront–Fu formulas. These formulas have a puzzling numerical similarity, which we discuss in detail and try to interpret mathematically and hydrologically.
Jan De Niel and Patrick Willems
Hydrol. Earth Syst. Sci., 23, 871–882, https://doi.org/10.5194/hess-23-871-2019, https://doi.org/10.5194/hess-23-871-2019, 2019
James W. Kirchner
Hydrol. Earth Syst. Sci., 23, 303–349, https://doi.org/10.5194/hess-23-303-2019, https://doi.org/10.5194/hess-23-303-2019, 2019
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How long does it take for raindrops to become streamflow? Here I propose a new approach to this old problem. I show how we can use time series of isotope data to measure the average fraction of same-day rainfall appearing in streamflow, even if this fraction varies greatly from rainstorm to rainstorm. I show that we can quantify how this fraction changes from small rainstorms to big ones, and from high flows to low flows, and how it changes with the lag time between rainfall and streamflow.
Ane Zabaleta, Eneko Garmendia, Petr Mariel, Ibon Tamayo, and Iñaki Antigüedad
Hydrol. Earth Syst. Sci., 22, 5227–5241, https://doi.org/10.5194/hess-22-5227-2018, https://doi.org/10.5194/hess-22-5227-2018, 2018
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This study establishes relationships between land cover and river discharge. Using discharge data from 20 catchments of the Bay of Biscay findings showed the influence of land cover on discharge changes with the amount of precipitation, with lower annual water resources associated with the greater presence of forests. Results obtained illustrate the relevance of land planning to the management of water resources and the opportunity to consider it in future climate-change adaptation strategies.
Dusan Jovanovic, Tijana Jovanovic, Alfonso Mejía, Jon Hathaway, and Edoardo Daly
Hydrol. Earth Syst. Sci., 22, 3551–3559, https://doi.org/10.5194/hess-22-3551-2018, https://doi.org/10.5194/hess-22-3551-2018, 2018
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A relationship between the Hurst (H) exponent (a long-term correlation coefficient) within a flow time series and various catchment characteristics for a number of catchments in the USA and Australia was investigated. A negative relationship with imperviousness was identified, which allowed for an efficient catchment classification, thus making the H exponent a useful metric to quantitatively assess the impact of catchment imperviousness on streamflow regime.
Chuanhao Wu, Bill X. Hu, Guoru Huang, Peng Wang, and Kai Xu
Hydrol. Earth Syst. Sci., 22, 1971–1991, https://doi.org/10.5194/hess-22-1971-2018, https://doi.org/10.5194/hess-22-1971-2018, 2018
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China has suffered some of the effects of global warming, and one of the potential implications of climate warming is the alteration of the temporal–spatial patterns of water resources. In this paper, the Budyko-based elasticity method was used to investigate the responses of runoff to historical and future climate variability over China at both grid and catchment scales. The results help to better understand the hydrological effects of climate change and adapt to a changing environment.
Samuel Saxe, Terri S. Hogue, and Lauren Hay
Hydrol. Earth Syst. Sci., 22, 1221–1237, https://doi.org/10.5194/hess-22-1221-2018, https://doi.org/10.5194/hess-22-1221-2018, 2018
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We investigate the impact of wildfire on watershed flow regimes, examining responses across the western United States. On a national scale, our results confirm the work of prior studies: that low, high, and peak flows typically increase following a wildfire. Regionally, results are more variable and sometimes contradictory. Our results may be significant in justifying the calibration of watershed models and in contributing to the overall observational analysis of post-fire streamflow response.
Annette Witt, Bruce D. Malamud, Clara Mangili, and Achim Brauer
Hydrol. Earth Syst. Sci., 21, 5547–5581, https://doi.org/10.5194/hess-21-5547-2017, https://doi.org/10.5194/hess-21-5547-2017, 2017
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Here we present a unique 9.5 m palaeo-lacustrine record of 771 palaeofloods which occurred over a period of 10 000 years in the Piànico–Sèllere basin (southern Alps) during an interglacial period in the Pleistocene (sometime between 400 000 and 800 000 years ago). We analyse the palaeoflood series correlation, clustering, and cyclicity properties, finding a long-range cyclicity with a period of about 2030 years superimposed onto a fractional noise.
Steve J. Birkinshaw, Selma B. Guerreiro, Alex Nicholson, Qiuhua Liang, Paul Quinn, Lili Zhang, Bin He, Junxian Yin, and Hayley J. Fowler
Hydrol. Earth Syst. Sci., 21, 1911–1927, https://doi.org/10.5194/hess-21-1911-2017, https://doi.org/10.5194/hess-21-1911-2017, 2017
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The Yangtze River basin in China is home to more than 400 million people and susceptible to major floods. We used projections of future precipitation and temperature from 35 of the most recent global climate models and applied this to a hydrological model of the Yangtze. Changes in the annual discharge varied between a 29.8 % decrease and a 16.0 % increase. The main reason for the difference between the models was the predicted expansion of the summer monsoon north and and west into the basin.
Maurizio Mazzoleni, Martin Verlaan, Leonardo Alfonso, Martina Monego, Daniele Norbiato, Miche Ferri, and Dimitri P. Solomatine
Hydrol. Earth Syst. Sci., 21, 839–861, https://doi.org/10.5194/hess-21-839-2017, https://doi.org/10.5194/hess-21-839-2017, 2017
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This study assesses the potential use of crowdsourced data in hydrological modeling, which are characterized by irregular availability and variable accuracy. We show that even data with these characteristics can improve flood prediction if properly integrated into hydrological models. This study provides technological support to citizen observatories of water, in which citizens can play an active role in capturing information, leading to improved model forecasts and better flood management.
Martin Durocher, Fateh Chebana, and Taha B. M. J. Ouarda
Hydrol. Earth Syst. Sci., 20, 4717–4729, https://doi.org/10.5194/hess-20-4717-2016, https://doi.org/10.5194/hess-20-4717-2016, 2016
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For regional flood frequency, it is challenging to identify regions with similar hydrological properties. Therefore, previous works have mainly proposed to use regions with similar physiographical properties. This research proposes instead to nonlinearly predict the desired hydrological properties before using them for delineation. The presented method is applied to a case study in Québec, Canada, and leads to hydrologically relevant regions, while enhancing predictions made inside them.
Donghua Zhang, Henrik Madsen, Marc E. Ridler, Jacob Kidmose, Karsten H. Jensen, and Jens C. Refsgaard
Hydrol. Earth Syst. Sci., 20, 4341–4357, https://doi.org/10.5194/hess-20-4341-2016, https://doi.org/10.5194/hess-20-4341-2016, 2016
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We present a method to assimilate observed groundwater head and soil moisture profiles into an integrated hydrological model. The study uses the ensemble transform Kalman filter method and the MIKE SHE hydrological model code. The proposed method is shown to be more robust and provide better results for two cases in Denmark, and is also validated using real data. The hydrological model with assimilation overall improved performance compared to the model without assimilation.
Morgan Fonley, Ricardo Mantilla, Scott J. Small, and Rodica Curtu
Hydrol. Earth Syst. Sci., 20, 2899–2912, https://doi.org/10.5194/hess-20-2899-2016, https://doi.org/10.5194/hess-20-2899-2016, 2016
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We design and implement a theoretical experiment to show that, under low-flow conditions, observed streamflow discrepancies between early and late summer can be attributed to different flow velocities in the river network. By developing an analytic solution to represent flow along a given river network, we emphasize the dependence of streamflow amplitude and time delay on the geomorphology of the network. We also simulate using a realistic river network to highlight the effects of scale.
Zhongwei Huang, Hanbo Yang, and Dawen Yang
Hydrol. Earth Syst. Sci., 20, 2573–2587, https://doi.org/10.5194/hess-20-2573-2016, https://doi.org/10.5194/hess-20-2573-2016, 2016
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The hydrologic processes have been influenced by different climatic factors. However, the dominant climatic factor driving annual runoff change is still unknown in many catchments in China. By using the climate elasticity method proposed by Yang and Yang (2011), the elasticity of runoff to climatic factors was estimated, and the dominant climatic factors driving annual runoff change were detected at catchment scale over China.
Jørn Rasmussen, Henrik Madsen, Karsten Høgh Jensen, and Jens Christian Refsgaard
Hydrol. Earth Syst. Sci., 20, 2103–2118, https://doi.org/10.5194/hess-20-2103-2016, https://doi.org/10.5194/hess-20-2103-2016, 2016
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In the paper, observations are assimilated into a hydrological model in order to improve the model performance. Two methods for detecting and correcting systematic errors (bias) in groundwater head observations are used leading to improved results compared to standard assimilation methods which ignores any bias. This is demonstrated using both synthetic (user generated) observations and real-world observations.
Mohammed Achite and Sylvain Ouillon
Hydrol. Earth Syst. Sci., 20, 1355–1372, https://doi.org/10.5194/hess-20-1355-2016, https://doi.org/10.5194/hess-20-1355-2016, 2016
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Changes of T, P, Q and sediment fluxes in a semi-arid basin little affected by human activities are analyzed from 40 years of measurements. T increased, P decreased, an earlier onset of first summer rains occurred. The flow regime shifted from perennial to intermittent. Sediment flux almost doubled every decade. The sediment regime shifted from two equivalent seasons of sediment delivery to a single major season regime. The C–Q rating curve ability declined due to enhanced hysteresis effects.
C. E. M. Lloyd, J. E. Freer, P. J. Johnes, and A. L. Collins
Hydrol. Earth Syst. Sci., 20, 625–632, https://doi.org/10.5194/hess-20-625-2016, https://doi.org/10.5194/hess-20-625-2016, 2016
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This paper examines the current methodologies for quantifying storm behaviour through hysteresis analysis, and explores a new method. Each method is systematically tested and the impact on the results is examined. Recommendations are made regarding the most effective method of calculating a hysteresis index. This new method allows storm hysteresis behaviour to be directly compared between storms, parameters, and catchments, meaning it has wide application potential in water quality research.
W. Hu and B. C. Si
Hydrol. Earth Syst. Sci., 20, 571–587, https://doi.org/10.5194/hess-20-571-2016, https://doi.org/10.5194/hess-20-571-2016, 2016
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Spatiotemporal SWC was decomposed into into three terms (spatial forcing, temporal forcing, and interactions between spatial and temporal forcing) for near surface and root zone; Empirical orthogonal function indicated that underlying patterns exist in the interaction term at small watershed scales; Estimation of spatially distributed SWC benefits from decomposition of the interaction term; The suggested decomposition of SWC with time stability analysis has potential in SWC downscaling.
Y. Chen, J. Li, and H. Xu
Hydrol. Earth Syst. Sci., 20, 375–392, https://doi.org/10.5194/hess-20-375-2016, https://doi.org/10.5194/hess-20-375-2016, 2016
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Parameter optimization is necessary to improve the flood forecasting capability of physically based distributed hydrological model. A method for parameter optimization with particle swam optimization (PSO) algorithm has been proposed for physically based distributed hydrological model in catchment flood forecasting and validated in southern China. It has found that the appropriate particle number and maximum evolution number of PSO algorithm are 20 and 30 respectively.
D. Hawtree, J. P. Nunes, J. J. Keizer, R. Jacinto, J. Santos, M. E. Rial-Rivas, A.-K. Boulet, F. Tavares-Wahren, and K.-H. Feger
Hydrol. Earth Syst. Sci., 19, 3033–3045, https://doi.org/10.5194/hess-19-3033-2015, https://doi.org/10.5194/hess-19-3033-2015, 2015
J. Rasmussen, H. Madsen, K. H. Jensen, and J. C. Refsgaard
Hydrol. Earth Syst. Sci., 19, 2999–3013, https://doi.org/10.5194/hess-19-2999-2015, https://doi.org/10.5194/hess-19-2999-2015, 2015
C. Kormann, T. Francke, M. Renner, and A. Bronstert
Hydrol. Earth Syst. Sci., 19, 1225–1245, https://doi.org/10.5194/hess-19-1225-2015, https://doi.org/10.5194/hess-19-1225-2015, 2015
S. Gharari, M. Shafiei, M. Hrachowitz, R. Kumar, F. Fenicia, H. V. Gupta, and H. H. G. Savenije
Hydrol. Earth Syst. Sci., 18, 4861–4870, https://doi.org/10.5194/hess-18-4861-2014, https://doi.org/10.5194/hess-18-4861-2014, 2014
S. G. Leibowitz, R. L. Comeleo, P. J. Wigington Jr., C. P. Weaver, P. E. Morefield, E. A. Sproles, and J. L. Ebersole
Hydrol. Earth Syst. Sci., 18, 3367–3392, https://doi.org/10.5194/hess-18-3367-2014, https://doi.org/10.5194/hess-18-3367-2014, 2014
J. Niu, J. Chen, and B. Sivakumar
Hydrol. Earth Syst. Sci., 18, 1475–1492, https://doi.org/10.5194/hess-18-1475-2014, https://doi.org/10.5194/hess-18-1475-2014, 2014
S. Galelli and A. Castelletti
Hydrol. Earth Syst. Sci., 17, 2669–2684, https://doi.org/10.5194/hess-17-2669-2013, https://doi.org/10.5194/hess-17-2669-2013, 2013
K. Rasouli, M. A. Hernández-Henríquez, and S. J. Déry
Hydrol. Earth Syst. Sci., 17, 1681–1691, https://doi.org/10.5194/hess-17-1681-2013, https://doi.org/10.5194/hess-17-1681-2013, 2013
M. Nied, Y. Hundecha, and B. Merz
Hydrol. Earth Syst. Sci., 17, 1401–1414, https://doi.org/10.5194/hess-17-1401-2013, https://doi.org/10.5194/hess-17-1401-2013, 2013
B. Gräler, M. J. van den Berg, S. Vandenberghe, A. Petroselli, S. Grimaldi, B. De Baets, and N. E. C. Verhoest
Hydrol. Earth Syst. Sci., 17, 1281–1296, https://doi.org/10.5194/hess-17-1281-2013, https://doi.org/10.5194/hess-17-1281-2013, 2013
Cited articles
Bekele, E. G. and Nicklow, J. W.: Multi-objective automatic calibration of SWAT using NSGA-II, J. Hydrol., 341, 165–176, https://doi.org/10.1016/j.jhydrol.2007.05.014, 2007.
Bense, V. F., Kooi, H., Ferguson, G., and Read, T.: Permafrost degradation as a control on hydrogeological regime shifts in a warming climate, J. Geophys. Res.-Earth, 117, F03036, https://doi.org/10.1029/2011JF002143, 2012.
Berghuijs, W. R., Hartmann, A., and Woods, R. A.:
Streamflow sensitivity to water storage changes across Europe, Geophys. Res. Lett., 43, 1980–1987, https://doi.org/10.1002/2016GL067927, 2016.
Bergner, F. and Zouhar, G.:
A new approach to the correlation between the coefficient and the exponent in the power law equation of fatigue crack growth, Int. J. Fatigue, 22, 229–230, https://doi.org/10.1016/S0142-1123(99)00123-1, 2000.
Biswal, B.:
Decorrelation is not dissociation: there is no means to entirely decouple the Brutsaert–Nieber parameters in streamflow recession analysis, Adv. Water Resour., 147, 103822, https://doi.org/10.1016/j.advwatres.2020.103822, 2021.
Bring, A., Fedorova, I., Dibike, Y. B., Hinzman, L. D., Mard, J., Mernild, S. H., and Woo, M.:
Arctic terrestrial hydrology: A synthesis of processes, regional effects, and research challenges, J. Geophysi. Res.-Biogeo., 121, 621–649, https://doi.org/10.1002/2015JG003131, 2016.
Brooks, P., Chorover, J., Fan, Y., Godsey, S. E., Maxwell, R. M., McNamara, J., and Tague, C.:
Hydrological partitioning in the critical zone: Recent advances and opportunities for developing transferable understanding of water cycle dynamics, Water Resour. Res., 51, 6973–6987, https://doi.org/10.1002/2015WR017039, 2015.
Brutsaert, W. and Hiyama, T.: The determination of permafrost thawing trends from long-term streamflow measurements with an application in eastern Siberia, J. Geophys. Res.-Atmos., 117, D22110, https://doi.org/10.1029/2012JD018344, 2012.
Brutsaert, W. and Nieber, J. L.:
Regionalized drought flow hydrographs from a mature glaciated plateau, Water Resour. Res., 13, 637–643, https://doi.org/10.1029/WR013i003p00637, 1977.
Burt, T. P. and Williams, P. J.:
Hydraulic conductivity in frozen soils, Earth Surface Processes, 9, 411–416, https://doi.org/10.1002/esp.3290010404, 1976.
Buttle, J. M.:
Mediating stream baseflow response to climate change: The role of basin storage, Hydrol. Process., 32, 363–378, https://doi.org/10.1002/hyp.11418, 2018.
Cai, L. C., Li, Z. W., You, Y. C., and Huang, C.: Analysis of runoff changes in Lhasa River from 1956 to 2016 and the influencing factors, J. Water Resour. Water Eng., 32, 90–96, 2021.
Carey, S. K. and Woo, M. K.:
Freezing of subarctic hillslopes, Wolf Creek Basin, Yukon, Canada, Arct. Antarct. Alp. Res., 37, 1–10, https://doi.org/10.1657/1523-0430(2005)037[0001:FOSHWC]2.0.CO;2, 2005.
Chang, X., Jin, H., He, R., Yang, S., Yu, S., Lv, L., Guo, D., Wang, S., and Kang, X.: Advances in permafrost and cold regions environments studies in the Da Xing'anling (Da Hinggan) mountains, northeastern China, J. Glaciol. Geocryol., 30, 176–82, https://doi.org/10.1007/s11442-008-0201-7, 2008.
Cuo, L., Zhang, Y. X., Zhu, F. X., and Liang, L. Q.:
Characteristics and changes of streamflow on the Tibetan Plateau: A review, J. Hydrol., 2, 49–68, https://doi.org/10.1016/j.ejrh.2014.08.004, 2014.
Dralle, D., Karst, N., and Thompson, S. E.:
a, b careful: The challenge of scale invariance for comparative analyses in power law models of the streamflow recession, Geophys. Res. Lett., 42, 9285–9293, https://doi.org/10.1002/2015GL066007, 2015.
Dralle, D. N., Karst, N. J., Charalampous, K., Veenstra, A., and Thompson, S. E.:
Event-scale power law recession analysis: quantifying methodological uncertainty, Hydrol. Earth Syst. Sci., 21, 65–81, https://doi.org/10.5194/hess-21-65-2017, 2017.
Forster, R. R., Box, J. E., van den Broeke, M. R., Miège, C., Burgess, E. W., van Angelen, J. H., Lenaerts, J. T. M., Koenig, L. S., Paden, J., Lewis, C., Gogineni, S. P., Leuschen, C., and McConnell, J. R.: Extensive liquid meltwater storage in firn within the Greenland ice sheet, Nat. Geosci., 7, 95–98, https://doi.org/10.1038/ngeo2043, 2014.
Harman, C. J., Sivapalan, M., and Kumar, P.:
Power law catchment-scale recessions arising from heterogeneous linear small-scale dynamics, Water Resour. Res., 45, W12601, https://doi.org/10.1029/2008WR007392, 2009.
Hayashi, M.:
Alpine Hydrogeology: The Critical Role of Groundwater in Sourcing the Headwaters of the World, Groundwater, 58, 498–510, https://doi.org/10.1111/gwat.12965, 2020.
He, J., Yang, K., Tang, W., Lu, H., Qin, J., Chen, Y., and Li, X.:
The first high-resolution meteorological forcing dataset for land process studies over China, Scientific Data, 7, 25, https://doi.org/10.1038/s41597-020-0369-y, 2020.
Hinzman, A. M., Lyon, S. W., Ploum, S. W., Sjoberg, Y., van der Velde, Y.:
Increasing non-linearity of the storage-discharge relationship in sub-Arctic catchments, Hydrol. Process., 34, 3894–3909, https://doi.org/10.1002/hyp.13860, 2020.
Ji, F., Fan, L., Andrews, C. B., Yao, Y., and Zheng, C.:
Dynamics of seasonally frozen ground in the Yarlung Zangbo River Basin on the Qinghai-Tibet Plateau: historical trend and future projection, Environ. Res. Lett., 15, 104081, https://doi.org/10.1088/1748-9326/abb731, 2020.
Juen, I., Kaser, G., and Georges, C.:
Modelling observed and future runoff from a glacierized tropical catchment (Cordillera Blanca, Peru), Global Planet. Change, 59, 37–48, https://doi.org/10.1016/j.gloplacha.2006.11.038, 2007.
Kendall, M. G.:
Rank Correlation Methods, 4th edn., Charles Griffin, London, 1975.
Kirchner, J. W.:
Catchments as simple dynamical systems: catchment characterization, rainfall-runoff modeling, and doing hydrology backward, Water Resour. Res., 45, W02429, https://doi.org/10.1029/2008WR006912, 2009.
Koch, J. C., Kikuchi, C. P., Wickland, K. P., and Schuster, P.:
Runoff sources and flow paths in a partially burned, upland boreal catchment underlain by permafrost, Water Resour. Res., 50, 8141–8158. https://doi.org/10.1002/2014WR015586, 2014.
Lamontagne-Hallé, P., McKenzie, J. M., Kurylyk, B. L., and Zipper, S. C.:
Changing groundwater discharge dynamics in permafrost regions, Environ. Res. Lett., 13, 084017, https://doi.org/10.1088/1748-9326/aad404, 2018.
Li, Z. J., Li, Z. X., Song, L. L., Ma, J. Z., and Song Y.:
Environment significance and hydrochemical characteristics of suprapermafrost water in the source region of the Yangtze River, Sci. Total Environ., 644, 1141–1151, https://doi.org/10.1016/j.scitotenv.2018.07.029, 2018.
Lin, L., Gao, M., Liu, J., Wang, J., Wang, S., Chen, X., and Liu, H.:
Understanding the effects of climate warming on streamflow and active groundwater storage in an alpine catchment: the upper Lhasa River, Hydrol. Earth Syst. Sci., 24, 1145–1157, https://doi.org/10.5194/hess-24-1145-2020, 2020.
Liu, J. P. and Zhang, W. C.:
Spatial variability in degree-day f actors in Yarlung Zangpo River Basin, China, Journal of University of Chinese Academy of Sciences, 35, 704–711. 2018.
Liu, Z., Yao, Z., Huang, H., Wu, S., and Liu, G.:
Land use and climate changes and their impacts on Runoff in the Yarlung Zangpo River Basin, China, Land Degrad. Dev., 25, 203–215, https://doi.org/10.1002/ldr.1159, 2014.
Lyon, S. W. and Destouni, G.:
Changes in catchment-scale recession flow properties in response to permafrost thawing in the Yukon River basin, Int. J. Climatol., 30, 2138–2145, https://doi.org/10.1002/joc.1993, 2010.
Lyon, S. W., Destouni, G., Giesler, R., Humborg, C., Mörth, M., Seibert, J., Karlsson, J., and Troch, P. A.:
Estimation of permafrost thawing rates in a sub-arctic catchment using recession flow analysis, Hydrol. Earth Syst. Sci., 13, 595–604, https://doi.org/10.5194/hess-13-595-2009, 2009.
Mallakpour, I. and Villarini, G.: A simulation study to examine the sensitivity of the Pettitt test to detect abrupt changes in mean, International Association of Scientific Hydrology Bulletin, 61, 245–254, https://doi.org/10.1080/02626667.2015.1008482, 2016.
Mann, H.:
Non-parametric test against trend, Econometrical, 13, 245–259, https://doi.org/10.2307/1907187, 1945.
Mao, T. and Wang, G.: Analysis on characteristics of low-flow based on the monthly runoff recession coefficient in the Three-river headwaters region, Resources and environment in the Yangtze basin, Resour. Environ. Yangtze Basin, 25, 1150–1157, 2016.
Niu, F. J., Gao, Z. Y., Lin, Z. J., Luo, J., and Fan, X. W.: Vegetation influence on the soil hydrological regime in permafrost regions of the Qinghai–Tibet Plateau, China, Geoderma, 354, 113892, https://doi.org/10.1016/j.geoderma.2019.113892, 2019.
Payn, R. A., Gooseff, M. N., McGlynn, B. L., Bencala, K. E., and Wondzell, S. M.:
Exploring changes in the spatial distribution of stream baseflow generation during a seasonal recession, Water Resour. Res., 48, 519, https://doi.org/10.1029/2011WR011552, 2012.
Pepin, N., Bradley, R. S., Diaz, H. F., Baraer, M., Caceres, E. B., Forsythe, N., Fowler, H., Greenwood, G., Hashmi, M., Liu, X. D., Miller, J. R., Ning, L., Ohmura, A., Palazzi, E., Rangwala, I., Schöner, W., Severskiy, I., Shahgedanova, M., Wang, M. B., Williamson, S. N., and Yang, D. Q.: Elevation dependent warming in mountain regions of the world, Nat. Clim. Change, 5, 424–430, https://doi.org/10.1038/nclimate2563, 2015.
Pettitt, A. N.:
A non-parametric approach to the change-point problem, J. R. Stat. Soc., 28, 126–135, https://doi.org/10.2307/2346729, 1979.
Ren, W., Yao, T., and Xie, S.:
Stable isotopic composition reveals the spatial and temporal dynamics of discharge in the large river of Yarlungzangbo in the Tibetan Plateau, Sci. Total Environ., 625, 373–381, https://doi.org/10.1016/j.scitotenv.2017.12.310, 2018.
Sen, P. K.:
Estimates of the regression coefficient based on Kendall's tau, J. Am. Stat. Assoc., 63, 1379–1389, https://doi.org/10.1080/01621459.1968.10480934, 1968.
Shi, D., Tan, H., Chen, X., Rao, W., and Renci, B.: Uncovering the mechanisms of seasonal river–groundwater circulation using isotopes and water chemistry in the middle reaches of the Yarlungzangbo River, Tibet, J. Hydrol., 603, 127010, https://doi.org/10.1016/j.jhydrol.2021.127010, 2021.
Su, F., Zhang, L., Ou, T., Chen, D., Yao, T., Tong, K., and Qi, Y.:
Hydrological response to future climate changes for the major upstream river basins in the Tibetan Plateau, Global Planet. Change, 136, 82–95, https://doi.org/10.1016/j.gloplacha.2015.10.012, 2015.
Tallaksen, L. M.:
A review of baseflow recession analysis, J. Hydrol., 165, 349–370, https://doi.org/10.1016/0022-1694(94)02540-R, 1995.
Tan, H., Chen, X., Shi, D., Rao, W., Liu, J., Liu, J., Eastoe, C. J., and Wang, J.: Base flow in the Yarlungzangbo River, Tibet, maintained by the isotopically-depleted precipitation and groundwater discharge, Sci. Total Environ., 759, 143510, https://doi.org/10.1016/j.scitotenv.2020.143510, 2021.
Tashie, A., Pavelsky, T., and Emanuel, R. E.: Spatial and temporal patterns in baseflow recession in the continental United States, Water Resour. Res., 56, e2019WR026425, https://doi.org/10.1029/2019WR026425, 2020.
Tashie, A. M., Scaife, C. I., and Band, L. E.:
Transpiration and subsurface controls on streamflow recession characteristics, Hydrol. Process., 33, 2561–2575, https://doi.org/10.1002/hyp.13530, 2019.
Tian, F., Xu, R., Nan, Y., Li, K., and He, Z.:
Quantification of runoff components in the Yarlung Tsangpo River using a distributed hydrological model, Advances in Water Science, 31, 324–336, https://doi.org/10.14042/j.cnki.32.1309.2020.03.002, 2020 (in Chinese).
Vuille, M., Kaser, G., and Juen, I.:
Glacier mass balance variability in the Cordillera Blanca, Peru and its relationship with climate and the large-scale circulation, Global Planet. Change, 62, 14–28, https://doi.org/10.1016/j.gloplacha.2007.11.003, 2008.
Walvoord, M. A. and Kurylyk, B. L.:
Hydrologic impacts of thawing permafrost – A review, Vadose Zone J., 15, 1–20, https://doi.org/10.2136/vzj2016.01.0010, 2016.
Walvoord, M. A. and Striegl, R. G.:
Increased groundwater to stream discharge from permafrost thawing in the Yukon River basin: Potential impacts on lateral export of carbon and nitrogen, Geophys. Res. Lett., 34, 123–134, https://doi.org/10.1029/2007GL030216, 2007.
Walvoord, M. A., Voss, C. I., and Wellman, T. P.:
Influence of permafrost distribution on groundwater flow in the context of climate-driven permafrost thaw: Example from Yukon Flats Basin, Alaska, USA, Water Resour. Res., 48, 524, https://doi.org/10.1029/2011WR011595, 2012.
Wang, J., Chen, X., Hu, Q., and Liu, J.: Responses of terrestrial water storage to climate variation in the Tibetan Plateau, J. Hydrol., 584, 124652, https://doi.org/10.1016/j.jhydrol.2020.124652, 2020.
Wang, J., Chen, X., Liu, J., and Hu, Q.: Changes of precipitation-runoff relationship induced by climate variation in a large glaciated basin of the Tibetan Plateau, J. Geophys. Res.-Atmos., 126, e2020JD034367, https://doi.org/10.1029/2020JD034367, 2021.
Wang, Y. H., Yang, H. B., Gao, B., Wang, T. H., Qin, Y., and Yang, D. W.:
Frozen ground degradation may reduce future runoff in the headwaters of an inland river on the northeastern Tibetan Plateau, J. Hydrol., 564, 1153–1164, https://doi.org/10.1016/j.jhydrol.2018.07.078, 2018.
Wright, N., Hayashi, M., and Quinton, W. L.: Spatial and temporal variations in active layer thawing and their implication on run-off generation in peat-covered permafrost terrain, Water Resour. Res., 45, W05414, https://doi.org/10.1029/2008WR006880, 2009.
Xu, X., Wu, Q., and Zhang, Z.: Responses of active layer thickness on the Qinghai Tibet Plateau to climate change, Journal of Glaciology and Geocryology, 39, 1–8, 2017.
Yamazaki, Y., Kubota, J., Ohata, T., Vuglinsky, V., and Mizuyama, T.:
Seasonal changes in runoff characteristics on a permafrost watershed in the southern mountainous regions of eastern Siberia, Hydrol. Process., 20, 453–467, https://doi.org/10.1002/hyp.5914, 2006.
Yang, K., and He, J.:
China meteorological forcing dataset (1979–2018), National Tibetan Plateau Data Center [data set], https://doi.org/10.11888/AtmosphericPhysics.tpe.249369.file, 2019.
Yao, T. D., Wang, Y. Q., Liu, S. Y., Pu, J. C., Shen, Y. P., and Lu, A. X.:
Recent glacial retreat in high Asia in China and its impact on water resource in northwest China, Sci. China Ser. D, 47, 1065–1075, https://doi.org/10.1360/03yd0256, 2004.
Yao, T., Pu, J., Lu, A., Wang, Y., and Yu, W.: Recent glacial retreat and its impact on hydrological processes on the Tibetan Plateau, China, and surrounding regions, Arct. Antarct. Alp. Res., 39, 642–650,
https://doi.org/10.1657/1523-0430(07-510)[YAO]2.0.CO;2, 2007.
Yao, Y., Zheng, C., Andrews, C. B., Scanlon, B. R., Kuang, X., Zeng, Z., Jeong, S.-J., Lancia, M., Wu, Y., Li, G.:
Role of groundwater in sustaining northern Himalayan rivers, Geophys. Res. Lett., 48, e2020GL092354, https://doi.org/10.1029/2020GL092354, 2021.
Yi, W., Feng, Y., Liang, S., Kuang, X., Yan, D., and Wan, L.: Increasing annual streamflow and groundwater storage in response to climate warming in the Yangtze river source region, Environ. Res. Lett., 16, 084011, https://doi.org/10.1088/1748-9326/ac0f27, 2021.
Yue, S. and Wang, C. Y.: Applicability of pre-whitening to eliminate the influence of serial correlation on the Mann–Kendall test, Water Resour. Res., 38, 41–47, https://doi.org/10.1029/2001WR000861, 2002.
Zhang, D., Huang, J., Guan, X., Chen, B., and Zhang, L.:
Long-term trends of perceptible water and precipitation over the Tibetan Plateau derived from satellite and surface measurements, J. Quant. Spectrosc. Ra., 122, 64–71, https://doi.org/10.1016/j.jqsrt.2012.11.028, 2013.
Short summary
The accelerated climate warming in the Tibetan Plateau after 1997 has strong consequences for hydrology, geography, and social wellbeing. In hydrology, the change in streamflow as a result of changes in dynamic water storage originating from glacier melt and permafrost thawing in a warming climate directly affects the available water resources for societies of some of the most populated nations in the world.
The accelerated climate warming in the Tibetan Plateau after 1997 has strong consequences for...
