Articles | Volume 28, issue 3
https://doi.org/10.5194/hess-28-719-2024
© Author(s) 2024. 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-28-719-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
16 Feb 2024
Research article |
| 16 Feb 2024
| 16 Feb 2024
Soil water sources and their implications for vegetation restoration in the Three-Rivers Headwater Region during different ablation periods
Zongxing Li
CORRESPONDING AUTHOR
Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Qilian Mountains/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China
Juan Gui
Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Qilian Mountains/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
Qiao Cui
Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Qilian Mountains/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
Jian Xue
Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Qilian Mountains/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
Fa Du
Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Qilian Mountains/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
Lanping Si
Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Qilian Mountains/ Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
Related authors
Juan Gui, Zongxing Li, Qi Feng, Qiao Cui, and Jian Xue
Hydrol. Earth Syst. Sci., 27, 97–122, https://doi.org/10.5194/hess-27-97-2023, https://doi.org/10.5194/hess-27-97-2023, 2023
Short summary
Short summary
As the transition zone between the Tibetan Plateau and the arid region, the Qilian Mountains are important ecological barriers and source regions of inland rivers in northwest China. In recent decades, drastic changes in the cryosphere have had a significant impact on the quantity and formation process of water resources in the Qilian Mountains. The mountain runoff of the Qilian Mountains mainly comes from the cryosphere belt, which contributes to approximately 80 % runoff.
Li Zongxing, Gui Juan, Zhang Baijuan, and Feng Qi
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-558, https://doi.org/10.5194/hess-2021-558, 2021
Manuscript not accepted for further review
Short summary
Short summary
Building spatial patterns of stable isotope of soil water; Finding influencing factors of stable isotope in soil water; Precipitation contributes to about 88 % of soil water; Ground ice accounts for about 12 % of soil water; Ecological conservation would be urgent under permafrost degradation.
Tingting Ning, Zhi Li, Qi Feng, Zongxing Li, and Yanyan Qin
Hydrol. Earth Syst. Sci., 25, 3455–3469, https://doi.org/10.5194/hess-25-3455-2021, https://doi.org/10.5194/hess-25-3455-2021, 2021
Short summary
Short summary
Previous studies decomposed ET variance in precipitation, potential ET, and total water storage changes based on Budyko equations. However, the effects of snowmelt and vegetation changes have not been incorporated in snow-dependent basins. We thus extended this method in arid alpine basins of northwest China and found that ET variance is primarily controlled by rainfall, followed by coupled rainfall and vegetation. The out-of-phase seasonality between rainfall and snowmelt weaken ET variance.
Zong-Jie Li, Zong-Xing Li, Ling-Ling Song, Juan Gui, Jian Xue, Bai Juan Zhang, and Wen De Gao
Hydrol. Earth Syst. Sci., 24, 4169–4187, https://doi.org/10.5194/hess-24-4169-2020, https://doi.org/10.5194/hess-24-4169-2020, 2020
Short summary
Short summary
This study mainly explores the hydraulic relations, recharge–drainage relations and their transformation paths, and the processes of each water body. It determines the composition of runoff, quantifies the contribution of each runoff component to different types of tributaries, and analyzes the hydrological effects of the temporal and spatial variation in runoff components. More importantly, we discuss the hydrological significance of permafrost and hydrological processes.
Juan Gui, Zongxing Li, Qi Feng, Qiao Cui, and Jian Xue
Hydrol. Earth Syst. Sci., 27, 97–122, https://doi.org/10.5194/hess-27-97-2023, https://doi.org/10.5194/hess-27-97-2023, 2023
Short summary
Short summary
As the transition zone between the Tibetan Plateau and the arid region, the Qilian Mountains are important ecological barriers and source regions of inland rivers in northwest China. In recent decades, drastic changes in the cryosphere have had a significant impact on the quantity and formation process of water resources in the Qilian Mountains. The mountain runoff of the Qilian Mountains mainly comes from the cryosphere belt, which contributes to approximately 80 % runoff.
Li Zongxing, Gui Juan, Zhang Baijuan, and Feng Qi
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-558, https://doi.org/10.5194/hess-2021-558, 2021
Manuscript not accepted for further review
Short summary
Short summary
Building spatial patterns of stable isotope of soil water; Finding influencing factors of stable isotope in soil water; Precipitation contributes to about 88 % of soil water; Ground ice accounts for about 12 % of soil water; Ecological conservation would be urgent under permafrost degradation.
Tingting Ning, Zhi Li, Qi Feng, Zongxing Li, and Yanyan Qin
Hydrol. Earth Syst. Sci., 25, 3455–3469, https://doi.org/10.5194/hess-25-3455-2021, https://doi.org/10.5194/hess-25-3455-2021, 2021
Short summary
Short summary
Previous studies decomposed ET variance in precipitation, potential ET, and total water storage changes based on Budyko equations. However, the effects of snowmelt and vegetation changes have not been incorporated in snow-dependent basins. We thus extended this method in arid alpine basins of northwest China and found that ET variance is primarily controlled by rainfall, followed by coupled rainfall and vegetation. The out-of-phase seasonality between rainfall and snowmelt weaken ET variance.
Zong-Jie Li, Zong-Xing Li, Ling-Ling Song, Juan Gui, Jian Xue, Bai Juan Zhang, and Wen De Gao
Hydrol. Earth Syst. Sci., 24, 4169–4187, https://doi.org/10.5194/hess-24-4169-2020, https://doi.org/10.5194/hess-24-4169-2020, 2020
Short summary
Short summary
This study mainly explores the hydraulic relations, recharge–drainage relations and their transformation paths, and the processes of each water body. It determines the composition of runoff, quantifies the contribution of each runoff component to different types of tributaries, and analyzes the hydrological effects of the temporal and spatial variation in runoff components. More importantly, we discuss the hydrological significance of permafrost and hydrological processes.
Related subject area
Subject: Ecohydrology | Techniques and Approaches: Theory development
Root zone in the Earth system
Biocrust-reduced soil water retention and soil infiltration in an alpine Kobresia meadow
The natural abundance of stable water isotopes method may overestimate deep-layer soil water use by trees
Contribution of cryosphere to runoff in the transition zone between the Tibetan Plateau and arid region based on environmental isotopes
Vegetation optimality explains the convergence of catchments on the Budyko curve
Differential response of plant transpiration to uptake of rainwater-recharged soil water for dominant tree species in the semiarid Loess Plateau
Isotopic offsets between bulk plant water and its sources are larger in cool and wet environments
Hydrology without dimensions
Long-term climate-influenced land cover change in discontinuous permafrost peatland complexes
Groundwater fauna in an urban area – natural or affected?
Age and origin of leaf wax n-alkanes in fluvial sediment–paleosol sequences and implications for paleoenvironmental reconstructions
Seasonal partitioning of precipitation between streamflow and evapotranspiration, inferred from end-member splitting analysis
The influence of litter crusts on soil properties and hydrological processes in a sandy ecosystem
Unexplained hydrogen isotope offsets complicate the identification and quantification of tree water sources in a riparian forest
A synthesis of three decades of hydrological research at Scotty Creek, NWT, Canada
Potential evaporation at eddy-covariance sites across the globe
Scaling properties reveal regulation of river flows in the Amazon through a “forest reservoir”
Water movement through plant roots – exact solutions of the water flow equation in roots with linear or exponential piecewise hydraulic properties
Large-scale vegetation responses to terrestrial moisture storage changes
Vegetation dynamics and climate seasonality jointly control the interannual catchment water balance in the Loess Plateau under the Budyko framework
Leaf-scale experiments reveal an important omission in the Penman–Monteith equation
The Budyko functions under non-steady-state conditions
Matching the Budyko functions with the complementary evaporation relationship: consequences for the drying power of the air and the Priestley–Taylor coefficient
Hydrological recovery in two large forested watersheds of southeastern China: the importance of watershed properties in determining hydrological responses to reforestation
The socioecohydrology of rainwater harvesting in India: understanding water storage and release dynamics across spatial scales
Nitrate sinks and sources as controls of spatio-temporal water quality dynamics in an agricultural headwater catchment
Impacts of beaver dams on hydrologic and temperature regimes in a mountain stream
Estimation of crop water requirements: extending the one-step approach to dual crop coefficients
Technical Note: On the Matt–Shuttleworth approach to estimate crop water requirements
Horizontal soil water potential heterogeneity: simplifying approaches for crop water dynamics models
Hurricane impacts on a pair of coastal forested watersheds: implications of selective hurricane damage to forest structure and streamflow dynamics
Regional and local patterns in depth to water table, hydrochemistry and peat properties of bogs and their laggs in coastal British Columbia
Impacts of forest changes on hydrology: a case study of large watersheds in the upper reaches of Minjiang River watershed in China
A simple three-dimensional macroscopic root water uptake model based on the hydraulic architecture approach
Training hydrologists to be ecohydrologists and play a leading role in environmental problem solving
Thermodynamic constraints on effective energy and mass transfer and catchment function
Can we predict groundwater discharge from terrestrial ecosystems using existing eco-hydrological concepts?
Macroinvertebrate community responses to a dewatering disturbance gradient in a restored stream
Mechanisms of vegetation uprooting by flow in alluvial non-cohesive sediment
Forest decline caused by high soil water conditions in a permafrost region
Hongkai Gao, Markus Hrachowitz, Lan Wang-Erlandsson, Fabrizio Fenicia, Qiaojuan Xi, Jianyang Xia, Wei Shao, Ge Sun, and Hubert Savenije
EGUsphere, https://doi.org/10.5194/egusphere-2024-332, https://doi.org/10.5194/egusphere-2024-332, 2024
Short summary
Short summary
The concept of root zone is widely used, but still lacks a precise definition. Moreover, its importance in Earth system science is not well elaborated. Here, we clarified its definition with several similar terms, to bridge the multi-disciplinary gap. We underscore the key role of root zone in Earth system, which links biosphere, hydrosphere, lithosphere, atmosphere, and anthroposphere. To better represent root zone, we advocate a paradigm shift towards ecosystem-centered modelling.
Licong Dai, Ruiyu Fu, Xiaowei Guo, Yangong Du, Guangmin Cao, Huakun Zhou, and Zhongmin Hu
Hydrol. Earth Syst. Sci., 27, 4247–4256, https://doi.org/10.5194/hess-27-4247-2023, https://doi.org/10.5194/hess-27-4247-2023, 2023
Short summary
Short summary
We found that, in the 0–30 cm soil layer, soil water retention and soil water content in normal Kobresia meadow (NM) were higher than those in biocrust meadow (BM), whereas the 30–40 cm layer's soil water retention and soil water content in NM were lower than those in BM. The topsoil infiltration rate in BM was lower than that in NM. Our findings revealed that the establishment of biocrust did not improve soil water retention and infiltration.
Shaofei Wang, Xiaodong Gao, Min Yang, Gaopeng Huo, Xiaolin Song, Kadambot H. M. Siddique, Pute Wu, and Xining Zhao
Hydrol. Earth Syst. Sci., 27, 123–137, https://doi.org/10.5194/hess-27-123-2023, https://doi.org/10.5194/hess-27-123-2023, 2023
Short summary
Short summary
Water uptake depth of 11-year-old apple trees reached 300 cm in the blossom and young fruit stage and only 100 cm in the fruit swelling stage, while 17-year-old trees always consumed water from 0–320 cm soil layers. Overall, the natural abundance of stable water isotopes method overestimated the contribution of deep soil water, especially in the 320–500 cm soils. Our findings highlight that determining the occurrence of root water uptake in deep soils helps to quantify trees' water use strategy.
Juan Gui, Zongxing Li, Qi Feng, Qiao Cui, and Jian Xue
Hydrol. Earth Syst. Sci., 27, 97–122, https://doi.org/10.5194/hess-27-97-2023, https://doi.org/10.5194/hess-27-97-2023, 2023
Short summary
Short summary
As the transition zone between the Tibetan Plateau and the arid region, the Qilian Mountains are important ecological barriers and source regions of inland rivers in northwest China. In recent decades, drastic changes in the cryosphere have had a significant impact on the quantity and formation process of water resources in the Qilian Mountains. The mountain runoff of the Qilian Mountains mainly comes from the cryosphere belt, which contributes to approximately 80 % runoff.
Remko C. Nijzink and Stanislaus J. Schymanski
Hydrol. Earth Syst. Sci., 26, 6289–6309, https://doi.org/10.5194/hess-26-6289-2022, https://doi.org/10.5194/hess-26-6289-2022, 2022
Short summary
Short summary
Most catchments plot close to the empirical Budyko curve, which allows for estimating the long-term mean annual evaporation and runoff. We found that a model that optimizes vegetation properties in response to changes in precipitation leads it to converge to a single curve. In contrast, models that assume no changes in vegetation start to deviate from a single curve. This implies that vegetation has a stabilizing role, bringing catchments back to equilibrium after changes in climate.
Yakun Tang, Lina Wang, Yongqiang Yu, and Dongxu Lu
Hydrol. Earth Syst. Sci., 26, 4995–5013, https://doi.org/10.5194/hess-26-4995-2022, https://doi.org/10.5194/hess-26-4995-2022, 2022
Short summary
Short summary
Whether rainwater-recharged soil water (RRS) uptake can increase plant transpiration after rainfall pulses requires investigation. Our results indicate a differential response of plant transpiration to RRS uptake. Mixed afforestation enhances these water relationships and decreases soil water source competition in deep soil. Our results suggest that plant species or plantation types that can enhance RRS uptake and reduce water competition should be considered for use in water-limited regions.
Javier de la Casa, Adrià Barbeta, Asun Rodríguez-Uña, Lisa Wingate, Jérôme Ogée, and Teresa E. Gimeno
Hydrol. Earth Syst. Sci., 26, 4125–4146, https://doi.org/10.5194/hess-26-4125-2022, https://doi.org/10.5194/hess-26-4125-2022, 2022
Short summary
Short summary
Recently, studies have been reporting mismatches in the water isotopic composition of plants and soils. In this work, we reviewed worldwide isotopic composition data of field and laboratory studies to see if the mismatch is generalised, and we found it to be true. This contradicts theoretical expectations and may underlie an non-described phenomenon that should be forward investigated and implemented in ecohydrological models to avoid erroneous estimations of water sources used by vegetation.
Amilcare Porporato
Hydrol. Earth Syst. Sci., 26, 355–374, https://doi.org/10.5194/hess-26-355-2022, https://doi.org/10.5194/hess-26-355-2022, 2022
Short summary
Short summary
Applying dimensional analysis to the partitioning of water and soil on terrestrial landscapes reveals their dominant environmental controls. We discuss how the dryness index and the storage index affect the long-term rainfall partitioning, the key nonlinear control of the dryness index in global datasets of weathering rates, and the existence of new macroscopic relations among average variables in landscape evolution statistics with tantalizing analogies with turbulent fluctuations.
Olivia Carpino, Kristine Haynes, Ryan Connon, James Craig, Élise Devoie, and William Quinton
Hydrol. Earth Syst. Sci., 25, 3301–3317, https://doi.org/10.5194/hess-25-3301-2021, https://doi.org/10.5194/hess-25-3301-2021, 2021
Short summary
Short summary
This study demonstrates how climate warming in peatland-dominated regions of discontinuous permafrost is changing the form and function of the landscape. Key insights into the rates and patterns of such changes in the coming decades are provided through careful identification of land cover transitional stages and characterization of the hydrological and energy balance regimes for each stage.
Fabien Koch, Kathrin Menberg, Svenja Schweikert, Cornelia Spengler, Hans Jürgen Hahn, and Philipp Blum
Hydrol. Earth Syst. Sci., 25, 3053–3070, https://doi.org/10.5194/hess-25-3053-2021, https://doi.org/10.5194/hess-25-3053-2021, 2021
Short summary
Short summary
In this study, we address the question of whether groundwater fauna in an urban area is natural or affected in comparison to forested land. We find noticeable differences in the spatial distribution of groundwater species and abiotic parameters. An ecological assessment reveals that conditions in the urban area are mainly not good. Yet, there is no clear spatial pattern in terms of land use and anthropogenic impacts. These are significant findings for conservation and usage of urban groundwater.
Marcel Bliedtner, Hans von Suchodoletz, Imke Schäfer, Caroline Welte, Gary Salazar, Sönke Szidat, Mischa Haas, Nathalie Dubois, and Roland Zech
Hydrol. Earth Syst. Sci., 24, 2105–2120, https://doi.org/10.5194/hess-24-2105-2020, https://doi.org/10.5194/hess-24-2105-2020, 2020
Short summary
Short summary
This study investigates the age and origin of leaf wax n-alkanes from a fluvial sediment–paleosol sequence (FSPS) by compound-class 14C dating. Our results show varying age offsets between the formation and sedimentation of leaf wax n-alkanes from well-developed (paleo)soils and fluvial sediments that are mostly due to their complex origin in such sequences. Thus, dating the leaf wax n-alkanes is an important step for more robust leaf-wax-based paleoenvironmental reconstructions in FSPSs.
James W. Kirchner and Scott T. Allen
Hydrol. Earth Syst. Sci., 24, 17–39, https://doi.org/10.5194/hess-24-17-2020, https://doi.org/10.5194/hess-24-17-2020, 2020
Short summary
Short summary
Perhaps the oldest question in hydrology is
Where does water go when it rains?. Here we present a new way to measure how the terrestrial water cycle partitions precipitation into its two ultimate fates:
green waterthat is evaporated or transpired back to the atmosphere and
blue waterthat is discharged to stream channels. Our analysis may help in gauging the vulnerability of both water resources and terrestrial ecosystems to changes in rainfall patterns.
Yu Liu, Zeng Cui, Ze Huang, Hai-Tao Miao, and Gao-Lin Wu
Hydrol. Earth Syst. Sci., 23, 2481–2490, https://doi.org/10.5194/hess-23-2481-2019, https://doi.org/10.5194/hess-23-2481-2019, 2019
Short summary
Short summary
We focus on the positive effects of litter crusts on soil water holding capacity and water interception capacity compared with biocrusts. Litter crusts can significantly improve sandy water content and organic matter. Water-holding capacity increased with development of litter crusts in the sandy interface. Water infiltration rate is increased by sandy and litter crusts' interface properties. Litter crusts provided a better microhabitat conducive to plant growth in sandy lands.
Adrià Barbeta, Sam P. Jones, Laura Clavé, Lisa Wingate, Teresa E. Gimeno, Bastien Fréjaville, Steve Wohl, and Jérôme Ogée
Hydrol. Earth Syst. Sci., 23, 2129–2146, https://doi.org/10.5194/hess-23-2129-2019, https://doi.org/10.5194/hess-23-2129-2019, 2019
Short summary
Short summary
Plant water sources of a beech riparian forest were monitored using stable isotopes. Isotopic fractionation during root water uptake is usually neglected but may be more common than previously accepted. Xylem water was always more depleted in δ2H than all sources considered, suggesting isotopic discrimination during water uptake or within plant tissues. Thus, the identification and quantification of tree water sources was affected. Still, oxygen isotopes were a good tracer of plant source water.
William Quinton, Aaron Berg, Michael Braverman, Olivia Carpino, Laura Chasmer, Ryan Connon, James Craig, Élise Devoie, Masaki Hayashi, Kristine Haynes, David Olefeldt, Alain Pietroniro, Fereidoun Rezanezhad, Robert Schincariol, and Oliver Sonnentag
Hydrol. Earth Syst. Sci., 23, 2015–2039, https://doi.org/10.5194/hess-23-2015-2019, https://doi.org/10.5194/hess-23-2015-2019, 2019
Short summary
Short summary
This paper synthesizes nearly three decades of eco-hydrological field and modelling studies at Scotty Creek, Northwest Territories, Canada, highlighting the key insights into the major water flux and storage processes operating within and between the major land cover types of this wetland-dominated region of discontinuous permafrost. It also examines the rate and pattern of permafrost-thaw-induced land cover change and how such changes will affect the hydrology and water resources of the region.
Wouter H. Maes, Pierre Gentine, Niko E. C. Verhoest, and Diego G. Miralles
Hydrol. Earth Syst. Sci., 23, 925–948, https://doi.org/10.5194/hess-23-925-2019, https://doi.org/10.5194/hess-23-925-2019, 2019
Short summary
Short summary
Potential evaporation (Ep) is the amount of water an ecosystem would consume if it were not limited by water availability or other stress factors. In this study, we compared several methods to estimate Ep using a global dataset of 107 FLUXNET sites. A simple radiation-driven method calibrated per biome consistently outperformed more complex approaches and makes a suitable tool to investigate the impact of water use and demand, drought severity and biome productivity.
Juan Fernando Salazar, Juan Camilo Villegas, Angela María Rendón, Estiven Rodríguez, Isabel Hoyos, Daniel Mercado-Bettín, and Germán Poveda
Hydrol. Earth Syst. Sci., 22, 1735–1748, https://doi.org/10.5194/hess-22-1735-2018, https://doi.org/10.5194/hess-22-1735-2018, 2018
Short summary
Short summary
River flow regimes are being altered by global change. Understanding the mechanisms behind such alterations is crucial for hydrological prediction. We introduce a novel interpretation of river flow metrics (scaling) that allows any river basin to be classified as regulated or unregulated, and to identify transitions between these states. We propose the
forest reservoirhypothesis to explain how forest loss can force the Amazonian river basins from regulated to unregulated states.
Félicien Meunier, Valentin Couvreur, Xavier Draye, Mohsen Zarebanadkouki, Jan Vanderborght, and Mathieu Javaux
Hydrol. Earth Syst. Sci., 21, 6519–6540, https://doi.org/10.5194/hess-21-6519-2017, https://doi.org/10.5194/hess-21-6519-2017, 2017
Short summary
Short summary
To maintain its yield, a plant needs to transpire water that it acquires from the soil. A deep understanding of the mechanisms that lead to water uptake location and intensity is required to correctly simulate the water transfer in the soil to the atmosphere. This work presents novel and general solutions of the water flow equation in roots with varying hydraulic properties that deeply affect the uptake pattern and the transpiration rate and can be used in ecohydrological models.
Robert L. Andrew, Huade Guan, and Okke Batelaan
Hydrol. Earth Syst. Sci., 21, 4469–4478, https://doi.org/10.5194/hess-21-4469-2017, https://doi.org/10.5194/hess-21-4469-2017, 2017
Short summary
Short summary
In this study we statistically analyse the relationship between vegetation cover and components of total water storage. Splitting water storage into different components allows for a more comprehensive understanding of the temporal response of vegetation to changes in water storage. Generally, vegetation appears to be more sensitive to interannual changes in water storage than to shorter changes, though this varies in different land use types.
Tingting Ning, Zhi Li, and Wenzhao Liu
Hydrol. Earth Syst. Sci., 21, 1515–1526, https://doi.org/10.5194/hess-21-1515-2017, https://doi.org/10.5194/hess-21-1515-2017, 2017
Short summary
Short summary
The relationship between controlling parameters of annual catchment water balance and climate seasonality (S) and vegetation coverage (M) was discussed under the Budyko framework and an empirical equation was further developed so that the contributions from M to actual evapotranspiration (ET) could be determined more accurately. The results showed that the effects of landscape condition changes to ET variation will be estimated with a large error if the impacts of S are ignored.
Stanislaus J. Schymanski and Dani Or
Hydrol. Earth Syst. Sci., 21, 685–706, https://doi.org/10.5194/hess-21-685-2017, https://doi.org/10.5194/hess-21-685-2017, 2017
Short summary
Short summary
Most of the rain falling on land is returned to the atmosphere by plant leaves, which release water vapour (transpire) through tiny pores. To better understand this process, we used artificial leaves in a special wind tunnel and discovered major problems with an established approach (PM equation) widely used to quantify transpiration and its sensitivity to climate change. We present an improved set of equations, consistent with experiments and displaying more realistic climate sensitivity.
Roger Moussa and Jean-Paul Lhomme
Hydrol. Earth Syst. Sci., 20, 4867–4879, https://doi.org/10.5194/hess-20-4867-2016, https://doi.org/10.5194/hess-20-4867-2016, 2016
Short summary
Short summary
A new physically based formulation is proposed to extend the Budyko framework under non-steady-state conditions, taking into account the change in water storage. The new formulation, which introduces an additional parameter, represents a generic framework applicable to any Budyko function at various time steps. It is compared to other formulations from the literature and the analytical solution of Greve et al. (2016) appears to be a particular case.
Jean-Paul Lhomme and Roger Moussa
Hydrol. Earth Syst. Sci., 20, 4857–4865, https://doi.org/10.5194/hess-20-4857-2016, https://doi.org/10.5194/hess-20-4857-2016, 2016
Short summary
Short summary
The Budyko functions are matched with the complementary evaporation relationship. We show that there is a functional dependence between the Budyko functions and the drying power of the air. Examining the case where potential evaporation is calculated by means of a Priestley–Taylor type equation with a varying coefficient, we show that this coefficient should have a specified value as a function of the Budyko shape parameter and the aridity index.
Wenfei Liu, Xiaohua Wei, Qiang Li, Houbao Fan, Honglang Duan, Jianping Wu, Krysta Giles-Hansen, and Hao Zhang
Hydrol. Earth Syst. Sci., 20, 4747–4756, https://doi.org/10.5194/hess-20-4747-2016, https://doi.org/10.5194/hess-20-4747-2016, 2016
Short summary
Short summary
In recent decades, limited research has been conducted to examine the role of watershed properties in hydrological responses in large watersheds. Based on pair-wise comparisons, we conclude that reforestation decreased high flows but increased low flows in the watersheds studied. Hydrological recovery through reforestation is largely dependent on watershed properties when forest change and climate are similar and comparable. This finding has important implications for designing reforestation.
Kimberly J. Van Meter, Michael Steiff, Daniel L. McLaughlin, and Nandita B. Basu
Hydrol. Earth Syst. Sci., 20, 2629–2647, https://doi.org/10.5194/hess-20-2629-2016, https://doi.org/10.5194/hess-20-2629-2016, 2016
Short summary
Short summary
Although village-scale rainwater harvesting (RWH) structures have been used for millennia in India, many of these structures have fallen into disrepair due to increased dependence on groundwater. This dependence has contributed to declines in groundwater resources, and in turn to efforts to revive older RWH systems. In the present study, we use field data to quantify water fluxes in a cascade of irrigation tanks to better our understanding of the impact of RWH systems on the water balance in con
Tobias Schuetz, Chantal Gascuel-Odoux, Patrick Durand, and Markus Weiler
Hydrol. Earth Syst. Sci., 20, 843–857, https://doi.org/10.5194/hess-20-843-2016, https://doi.org/10.5194/hess-20-843-2016, 2016
Short summary
Short summary
We quantify the spatio-temporal impact of distinct nitrate sinks and sources on stream network nitrate dynamics in an agricultural headwater. By applying a data-driven modelling approach, we are able to fully distinguish between mixing and dilution processes, and biogeochemical in-stream removal processes along the stream network. In-stream nitrate removal is estimated by applying a novel transfer coefficient based on energy availability.
M. Majerova, B. T. Neilson, N. M. Schmadel, J. M. Wheaton, and C. J. Snow
Hydrol. Earth Syst. Sci., 19, 3541–3556, https://doi.org/10.5194/hess-19-3541-2015, https://doi.org/10.5194/hess-19-3541-2015, 2015
Short summary
Short summary
This study quantifies the impacts of beaver on hydrologic and temperature regimes, as well as highlights the importance of understanding the spatial and temporal scales of those impacts.
Reach-scale discharge showed shift from losing to gaining. Temperature increased by 0.38°C (3.8%) and mean residence time by 230%. At the sub-reach scale, discharge gains and losses increased in variability. At the beaver dam scale, we observed increase in thermal heterogeneity with warmer and cooler niches.
J. P. Lhomme, N. Boudhina, M. M. Masmoudi, and A. Chehbouni
Hydrol. Earth Syst. Sci., 19, 3287–3299, https://doi.org/10.5194/hess-19-3287-2015, https://doi.org/10.5194/hess-19-3287-2015, 2015
J. P. Lhomme, N. Boudhina, and M. M. Masmoudi
Hydrol. Earth Syst. Sci., 18, 4341–4348, https://doi.org/10.5194/hess-18-4341-2014, https://doi.org/10.5194/hess-18-4341-2014, 2014
V. Couvreur, J. Vanderborght, L. Beff, and M. Javaux
Hydrol. Earth Syst. Sci., 18, 1723–1743, https://doi.org/10.5194/hess-18-1723-2014, https://doi.org/10.5194/hess-18-1723-2014, 2014
A. D. Jayakaran, T. M. Williams, H. Ssegane, D. M. Amatya, B. Song, and C. C. Trettin
Hydrol. Earth Syst. Sci., 18, 1151–1164, https://doi.org/10.5194/hess-18-1151-2014, https://doi.org/10.5194/hess-18-1151-2014, 2014
S. A. Howie and H. J. van Meerveld
Hydrol. Earth Syst. Sci., 17, 3421–3435, https://doi.org/10.5194/hess-17-3421-2013, https://doi.org/10.5194/hess-17-3421-2013, 2013
X. Cui, S. Liu, and X. Wei
Hydrol. Earth Syst. Sci., 16, 4279–4290, https://doi.org/10.5194/hess-16-4279-2012, https://doi.org/10.5194/hess-16-4279-2012, 2012
V. Couvreur, J. Vanderborght, and M. Javaux
Hydrol. Earth Syst. Sci., 16, 2957–2971, https://doi.org/10.5194/hess-16-2957-2012, https://doi.org/10.5194/hess-16-2957-2012, 2012
M. E. McClain, L. Chícharo, N. Fohrer, M. Gaviño Novillo, W. Windhorst, and M. Zalewski
Hydrol. Earth Syst. Sci., 16, 1685–1696, https://doi.org/10.5194/hess-16-1685-2012, https://doi.org/10.5194/hess-16-1685-2012, 2012
C. Rasmussen
Hydrol. Earth Syst. Sci., 16, 725–739, https://doi.org/10.5194/hess-16-725-2012, https://doi.org/10.5194/hess-16-725-2012, 2012
A. P. O'Grady, J. L. Carter, and J. Bruce
Hydrol. Earth Syst. Sci., 15, 3731–3739, https://doi.org/10.5194/hess-15-3731-2011, https://doi.org/10.5194/hess-15-3731-2011, 2011
J. D. Muehlbauer, M. W. Doyle, and E. S. Bernhardt
Hydrol. Earth Syst. Sci., 15, 1771–1783, https://doi.org/10.5194/hess-15-1771-2011, https://doi.org/10.5194/hess-15-1771-2011, 2011
K. Edmaier, P. Burlando, and P. Perona
Hydrol. Earth Syst. Sci., 15, 1615–1627, https://doi.org/10.5194/hess-15-1615-2011, https://doi.org/10.5194/hess-15-1615-2011, 2011
H. Iwasaki, H. Saito, K. Kuwao, T. C. Maximov, and S. Hasegawa
Hydrol. Earth Syst. Sci., 14, 301–307, https://doi.org/10.5194/hess-14-301-2010, https://doi.org/10.5194/hess-14-301-2010, 2010
Cited articles
Beyer, M., Hamutoko, J. T., Wanke, H., Gaj, M., and Koeniger, P.: Examination of deep root water uptake using anomalies of soil water stable isotopes, depth-controlled isotopic labeling and mixing models, J. Hydrol., 566, 122–136, https://doi.org/10.1016/j.jhydrol.2018.08.060, 2018.
Cao, R. F. and Jin, X. M.: Distribution Characteristics of Soil Moisture in the Three Rivers Headwaters Region, China, J. Environ. Inform. Lett., 6, 55–65, https://doi.org/10.3808/jeil.202100067, 2021.
Cao, W., Sheng, Y., Wu, J., Wang, S., and Ma, S.: Seasonal variation of soil hydrological processes of active layer in source region of the Yellow River, Adv. Water Sci., 29, 1–10, https://doi.org/10.14042/j.cnki.32.1309.2018.01.001, 2018.
Chang, J., Wang, G. X., Gao, Y. Y., and Wang, Y. B.: Impacts of snow cover change on soil water-heat processes of swamp and meadow in Permafrost Region, Qinghai-Tibetan Plateau, Acta Ecolog. Sin., 32, 7289–7301, https://doi.org/10.11733/j.issn.1007-0435.2021.Z1.023, 2012.
Chen, G. Q., Zhu, C. X., Li, S. Y., Zhou, B. R., Li F., Cao X. Y., and Zhou, H. K.: Remote Sensing Model Constructions and Spatial-temporal Changes of Soil Moisture in the Three-River Headwaters Region, Acta Agrest. Sin., 29, 199–207, https://doi.org/10.11733/j.issn.1007-0435.2021.Z1.023, 2021.
Cheng, H.: Future Earth and Sustainable Developments, Innovation, 1, 100055, https://doi.org/10.1016/j.xinn.2020.100055, 2020.
Deng, M., Meng, X., Li, Z., Lyv, Y., Lei, H., Zhao, L., Zhao, S., Ge, J., and Jing, H.: Responses of soil moisture to regional climate change over the Three Rivers Source Region on the Tibetan Plateau, Int. J. Climatol., 40, 2403–2417, https://doi.org/10.1002/joc.6341, 2019.
Fan, J., Shao, Q., Liu, J., Wang, J., Chen, Z., Zhong, H., Xu, X., and Liu, R.: Dynamic Changes of Grassland Yield in Three River Headwater Region from 1988 to 2005, Acta Agrest. Sin., 18, 5–10, https://doi.org/10.11733/j.issn.1007-0435.2010.01.002, 2010.
Gaj, M., Beyer, M., Koeniger, P., Wanke, H., Hamutoko, J. T., and Himmelsbach, T.: In situ unsaturated zone water stable isotope (2H and 18O) measurements in semi-arid environments: a soil water balance, Hydrol. Earth Syst. Sci., 20, 715–731, https://doi.org/10.5194/hess-20-715-2016, 2016.
Geris, J., Tetzlaff, D., McDonnell, J. J., and Soulsby, C.: Spatial and temporal patterns of soil water storage and vegetation water use in humid northern catchments, Sci. Total Environ., 595, 486–493, https://doi.org/10.1016/j.scitotenv.2017.03.275, 2017.
Guan, X. J., Westbrook, C. J., and Spence, C.: Shallow soil moisture–ground thaw interactions and controls – Part 1: Spatiotemporal patterns and correlations over a subarctic landscape, Hydrol. Earth Syst. Sci., 14, 1375–1386, https://doi.org/10.5194/hess-14-1375-2010, 2010.
Guo, L., Zhu, B., Jin, H., Zhang, Y., Min, Y., He, Y., and Shi, H.: Spatial-Temporal Variation Characteristics and Influencing Factors of Soil Moisture in the Yellow River Basin Using ESA CCI SM Products, Atmosphere, 13, 962, https://doi.org/10.3390/atmos13060962, 2022.
Jeppesen, E., Beklioğlu, M., Özkan, K., and Akyürek, Z.: Salinization Increase due to Climate Change Will Have Substantial Negative Effects on Inland Waters: A Call for Multifaceted Research at the Local and Global Scale, Innovation, 1, 100030, https://doi.org/10.1016/j.xinn.2020.100030, 2020.
Jiao, L., An, W., Li, Z., Gao, G., and Wang, C.: Regional variation in soil water and vegetation characteristics in the Chinese Loess Plateau, Ecol. Indic., 115, 106399, https://doi.org/10.1016/j.ecolind.2020.106399, 2020.
Jiao, Y. L., Li R., Zhao L., Wu T. H., Xiao Y., Hu G. J., and Qiao Y. P.: Processes of soil thawing-freezing and features of soil moisture migration in the permafrost active layer, J. Glaciol. Geocryol., 36, 237–247, https://doi.org/10.7522/j.issn.1000-0240.2014.0030, 2014.
Jin, X., Jin, H.-J., Wu, X., Luo, D.-L., Yu, S., Li, X., He, R.-X., Wang, Q., and Knops, J. M. H.: Permafrost Degradation Leads to Biomass and Species Richness Decreases on the Northeastern Qinghai-Tibet Plateau, Plants, 9, 1453, https://doi.org/10.3390/plants9111453, 2020.
Li, J., Zhou, Z., Wang, H., Liu, J., Jia, Y., Hu, P., and Xu, C.-Y.: Development of WEP-COR model to simulate land surface water and energy budgets in a cold region, Hydrol. Res., 50, 99–116, https://doi.org/10.2166/nh.2017.032, 2017.
Li, T., Chen, Y. Z., Han, L. J., Cheng, L. H., Lv, Y. H., Fu, B. J., Feng, X. M., and Wu, X.: Shortened duration and reduced area of frozen soil in the Northern Hemisphere, Innovation, 2, 100146, https://doi.org/10.1016/j.xinn.2021.100146, 2021.
Li, Z., Feng, Q., Wang, Q. J., Song, Y., Cheng, A., and Li, J.: Contribution from frozen soil meltwater to runoff in an in-land river basin under water scarcity by isotopic tracing in northwestern China, Global Planet. Change, 136, 41–51, https://doi.org/10.1016/j.gloplacha.2015.12.002, 2016.
Li, Z., Ma, J., Song, L., Gui, J., Xue, J., Zhang, B., Gao, W., and Li, Z.: Investigation of soil water hydrological process in the permafrost active layer using stable isotopes, Hydrol. Process., 34, 2810–2822, https://doi.org/10.1002/hyp.13765, 2020.
Lin, J., Ma, R., Sun, Z., and Tang, L.: Assessing the Connectivity of a Regional Fractured Aquifer Based on a Hydraulic Conductivity Field Reversed by Multi-Well Pumping Tests and Numerical Groundwater Flow Modeling, J. Earth Sci., 34, 1926–1939, https://doi.org/10.1007/s12583-022-1674-5, 2023.
Liu, G., Wu, X., Zhao, L., Wu, T., Hu, G., Li, R., Qiao, Y., and Wu, X.: Soil water content in permafrost regions exhibited smaller interannual changes than non-permafrost regions during 1986–2016 on the Qinghai-Tibetan Plateau, Catena, 207, 105668, https://doi.org/10.1016/j.catena.2021.105668, 2021.
Liu, Q., Liu, Y., Jin, M., Zhou, J., and Ferré, P. A.: Improving the Estimation of Salt Distribution during Evaporation in Saline Soil by HP1 Model, J. Earth Sci., 34, 1567–1576, https://doi.org/10.1007/s12583-021-1447-6, 2023.
Liu, Z., Wang, S., and Chen, B.: Spatial and temporal variations of frozen ground and its vegetation response in the eastern segment of China-Mongolia-Russia economic corridor from 2000 to 2015, Acta Geogr. Sin., 76, 1231–1244, https://doi.org/10.11821/dlxb202105014, 2021.
Lu, F.-S., Ade, L.-J., Cheng, Y.-X., and Hou, F.-J.: Relationship between soil moisture and vegetation cover in Qilian Mountain alpine steppe, Acta Pratacult. Sin., 29, 23–32, https://doi.org/10.11686/cyxb2020015, 2020.
Lv, M., Wang, Y., and Gao, Z.: The change process of soil hydrological properties in the permafrost active layer of the Qinghai–Tibet Plateau, Catena, 210, 105938, https://doi.org/10.1016/j.catena.2021.105938, 2022.
Ma, D., Luo, S. Q., Guo, D. L., Lyu, S. H., Meng, X. H., Chen, B. L., and Luo, L. H.: Simulated effect of soil freeze-thaw process on surface hydrologic and thermal fluxes in frozen ground region of the Northern Hemisphere, Sci. Cold Arid Reg., 13, 18–29, 2021.
Marchionni, V., Fatichi, S., Tapper, N., Walker, J. P., Manoli, G., and Daly, E.: Assessing vegetation response to irrigation strategies and soil properties in an urban reserve in southeast Australia, Landsc. Urban Plan., 215, 104198, https://doi.org/10.1016/j.landurbplan.2021.104198, 2021.
Martínez García, G., Pachepsky, Y. A., and Vereecken, H.: Effect of soil hydraulic properties on the relationship between the spatial mean and variability of soil moisture, J. Hydrol., 516, 154–160, https://doi.org/10.1016/j.jhydrol.2014.01.069, 2014.
Shiting, Y., Guangxin, L. U., Xin, L. I., Ning, D., Yingcheng, W., Dongzhu, Z., Gang, F. U., Junbang, W., and Huakun, Z.: Effects of Simulated Warming on Soil Moisture of Alpine Meadow at Chengduo of Yushu Prefecture, Qinghai Province, Ecol. Environ. Sci., 28, 2176–2184, https://doi.org/10.16258/j.cnki.1674-5906.2019.11.005, 2019.
Song, L. L., Li, Z. J., Tian, Q., Wang, L. F., He, J., Yuan, R. F., Gui, J., Zhang, B. J., and Lv, Y. M.: Variation and relationship between soil moisture and environmental factors in the source region of the Yangtze River from 2005 to 2016, Sci. Cold Arid Reg., 11, 184–193, 2019.
Spennemann, P. C., Salvia, M. M., Ruscica, R. C., Sörensson, A. A., Grings, F. M., and Karszenbaum, H.: Land-atmosphere interaction patterns in southeastern South America using satellite products and climate models, Int. J. Appl. Earth Obs. Geoinf., 64, 96–103, https://doi.org/10.1016/j.jag.2017.08.016, 2018.
Sprenger, M., Tetzlaff, D., and Soulsby, C.: Soil water stable isotopes reveal evaporation dynamics at the soil–plant–atmosphere interface of the critical zone, Hydrol. Earth Syst. Sci., 21, 3839–3858, https://doi.org/10.5194/hess-21-3839-2017, 2017.
Sun, H., Sun, X., Wei, X. F., Huang, X., Ke, G., and Wei, H.: Geochemical Characteristics and Origin of Nuanquanzi Geothermal Water in Yudaokou, Chengde, Hebei, North China, J. Earth Sci., 34, 838–856, https://doi.org/10.1007/s12583-022-1635-z, 2023.
Tan, H., Liu, Z., Rao, W., Wei, H., Zhang, Y., and Jin, B.: Stable isotopes of soil water: Implications for soil water and shallow groundwater recharge in hill and gully regions of the Loess Plateau, China, Agricult. Ecosyst. Environ., 243, 1–9, https://doi.org/10.1016/j.agee.2017.04.001, 2017.
Wang, P.: Low-latitude forcing: A new insight into paleo-climate changes, Innovation, 2, 100145, https://doi.org/10.1016/j.xinn.2021.100145, 2021.
Wang, Y. B., Wang G. X., Wu, Q. B., Niu, F. J., Wang, G. X., and Cheng, H. Y.: The Impact of Vegetation Degeneration on Hydrology Features of Alpine Soil, J. Glaciol. Geocryol., 32, 989–998, https://doi.org/10.7522/j.issn.1000-0240.2010.0135, 2010.
Wang, Y. B., Niu, F. J., Wen, J., Wu, Q. B., and Zhang, W.: Study of the Soil Hydrological Process in the Source Regions of the Yangtze River, China, Adv. Mater. Res., 518–523, 4266–4272, https://doi.org/10.4028/www.scientific.net/AMR.518-523.4266, 2012.
Wei, X., Huang, Q., Huang, S., Leng, G., Qu, Y., Deng, M., Han, Z., Zhao, J., Liu, D., and Bai, Q.: Assessing the feedback relationship between vegetation and soil moisture over the Loess Plateau, China, Ecol. Indic., 134, 108493, https://doi.org/10.1016/j.ecolind.2021.108493, 2022.
Wen, J., Qin, R., Zhang, S., Yang, X., and Xu, M.-H.: Effects of long-term warming on the aboveground biomass and species diversity in an alpine meadow on the Qinghai-Tibetan Plateau of China, J. Arid Land, 12, 252–266, https://doi.org/10.1007/s40333-020-0064-z, 2020.
Xiang, L., Wang, H., Steffen, H., Wu, P., Jia, L., Jiang, L., and Shen, Q.: Groundwater storage changes in the Tibetan Plateau and adjacent areas revealed from GRACE satellite gravity data, Earth Planet. Sc. Lett., 449, 228–239, https://doi.org/10.1016/j.epsl.2016.06.002, 2016.
Xue, X., You, Q., Peng, F., Dong, S., and Duan, H.: Experimental Warming Aggravates Degradation-Induced Topsoil Drought in Alpine Meadows of the Qinghai–Tibetan Plateau, Land Degrad. Dev., 28, 2343–2353, https://doi.org/10.1002/ldr.2763, 2017.
Yang, Z., Hua, O., Zhang, X.-Z., Xu, X., Zhou, C.-P., and Yang, W.-B.: Spatial variability of soil moisture at typical alpine meadow and steppe sites in the Qinghai-Tibetan Plateau permafrost region, Environ. Earth Sci., 63, 477–488, https://doi.org/10.1007/s12665-010-0716-y, 2011.
Yue, D., Mu, X., Zhou, Y., Guo, X., Wei, L., and Guo, J.: Coupling relationship between net primary productivity and soil moisture content in the Shule River Basin, J. Lanzhou Univ. Nat. Sci., 57, 518–527 + 536, https://doi.org/10.13885/j.issn.0455-2059.2021.04.012, 2021.
Yue, D., Zhou, Y., Guo, J., Chao, Z., and Guo, X.: Relationship between net primary productivity and soil water content in the Shule River Basin, Catena, 208, 105770, https://doi.org/10.1016/j.catena.2021.105770, 2022.
Zhang, Q., Wang, Y., and Wang, Y. L.: Preliminary study on the components of the lower crust in east China Plateau during Yanshanian Period: Constraints on Sr and Nd isotopic compositions of adakite-like rocks, Acta Petrol. Sin., 17, 505–513, 2001.
Short summary
Precipitation, ground ice, and snow meltwater accounted for approximately 72 %, 20 %, and 8 % of soil water during the early ablation period. Snow is completely melted in the heavy ablation period and the end of the ablation period, and precipitation contributed about 90 % and 94 % of soil water, respectively. These recharges also vary markedly with altitude and vegetation type.
Precipitation, ground ice, and snow meltwater accounted for approximately 72 %, 20 %, and 8 % of...
