Articles | Volume 23, issue 5
Research article 09 May 2019
Research article | 09 May 2019
Modelling of shallow water table dynamics using conceptual and physically based integrated surface-water–groundwater hydrologic models
Mohammad Bizhanimanzar et al.
No articles found.
Jean Bergeron, Gabriela Siles, Robert Leconte, Mélanie Trudel, Damien Desroches, and Daniel L. Peters
Hydrol. Earth Syst. Sci., 24, 5985–6000,Short summary
We want to assess how well the Surface Water and Ocean Topography (SWOT) satellite mission will be able to provide information on lake surface water elevation and how much of an impact wind conditions (speed and direction) can have on these retrievals.
Bruce Davison, Vincent Fortin, Alain Pietroniro, Man K. Yau, and Robert Leconte
Hydrol. Earth Syst. Sci., 23, 741–762,Short summary
This paper explores a new method of predicting streamflow using a complex model. It makes use of streamflow observations to reduce an existing ensemble of model runs for predictive purposes. The study illustrated that the method could work given the proper constraints, which were only possible if there was enough knowledge about how the river responded to precipitation in the previous months. Ideas were discussed to allow the method to be used in a way to predict future streamflow.
Rachel Bazile, Marie-Amélie Boucher, Luc Perreault, and Robert Leconte
Hydrol. Earth Syst. Sci., 21, 5747–5762,Short summary
Meteorological forecasting agencies constantly work on pushing the limit of predictability farther in time. However, some end users need proof that climate model outputs are ready to be implemented operationally. We show that bias correction is crucial for the use of ECMWF System4 forecasts for the studied area and there is a potential for the use of 1-month-ahead forecasts. Beyond this, forecast performance is equivalent to using past climatology series as inputs to the hydrological model.
Jean M. Bergeron, Mélanie Trudel, and Robert Leconte
Hydrol. Earth Syst. Sci., 20, 4375–4389,Short summary
We want to know how combined snow water equivalent (SWE) and streamflow data assimilation (DA) impacts streamflow predictions and how it compares with DA of SWE only and streamflow only. Results show that streamflow DA positively impacts short-term streamflow forecasts, while the impact of SWE DA lasts over a much longer horizon. Simultaneous DA of both SWE and streamflow performs better than its individual counterparts at all forecast horizons.
Related subject area
Subject: Vadose Zone Hydrology | Techniques and Approaches: Modelling approachesComparison of root water uptake models in simulating CO2 and H2O fluxes and growth of wheatUnderstanding the mass, momentum, and energy transfer in the frozen soil with three levels of model complexitiesInvestigating the impact of exit effects on solute transport in macropored porous mediaA field-validated surrogate crop model for predicting root-zone moisture and salt content in regions with shallow groundwaterCharacterizing uncertainty in the hydraulic parameters of oil sands mine reclamation covers and its influence on water balance predictionsSimulating preferential soil water flow and tracer transport using the Lagrangian Soil Water and Solute Transport ModelAssessment of simulated soil moisture from WRF Noah, Noah-MP, and CLM land surface schemes for landslide hazard applicationEfficient estimation of effective hydraulic properties of stratal undulating surface layer using time-lapse multi-channel GPRPartitioning snowmelt and rainfall in the critical zone: effects of climate type and soil propertiesA unique vadose zone model for shallow aquifers: the Hetao irrigation district, ChinaCapturing soil-water and groundwater interactions with an iterative feedback coupling scheme: new HYDRUS package for MODFLOWCaffeine vs. carbamazepine as indicators of wastewater pollution in a karst aquiferPredicting the soil water retention curve from the particle size distribution based on a pore space geometry containing slit-shaped spacesTechnical note: Saturated hydraulic conductivity and textural heterogeneity of soilsWater ages in the critical zone of long-term experimental sites in northern latitudesEcohydrological particle model based on representative domainsImpact of capillary rise and recirculation on simulated crop yieldsSoil hydraulic material properties and layered architecture from time-lapse GPRRoot growth, water uptake, and sap flow of winter wheat in response to different soil water conditionsUsing lagged dependence to identify (de)coupled surface and subsurface soil moisture valuesShallow water table effects on water, sediment, and pesticide transport in vegetative filter strips – Part 1: nonuniform infiltration and soil water redistributionShallow water table effects on water, sediment, and pesticide transport in vegetative filter strips – Part 2: model coupling, application, factor importance, and uncertaintyA pore-size classification for peat bogs derived from unsaturated hydraulic propertiesMonitoring and modeling infiltration–recharge dynamics of managed aquifer recharge with desalinated seawaterEffect of unrepresented model errors on estimated soil hydraulic material propertiesSaturated hydraulic conductivity model computed from bimodal water retention curves for a range of New Zealand soilsRoss scheme, Newton–Raphson iterative methods and time-stepping strategies for solving the mixed form of Richards' equationFeasibility analysis of using inverse modeling for estimating field-scale evapotranspiration in maize and soybean fields from soil water content monitoring networksA case study of field-scale maize irrigation patterns in western Nebraska: implications for water managers and recommendations for hyper-resolution land surface modelingBenchmarking test of empirical root water uptake modelsiCRESTRIGRS: a coupled modeling system for cascading flood–landslide disaster forecastingEnKF with closed-eye period – towards a consistent aggregation of information in soil hydrologyPrediction of biopore- and matrix-dominated flow from X-ray CT-derived macropore network characteristicsA Lagrangian model for soil water dynamics during rainfall-driven conditionsQuantifying shallow subsurface water and heat dynamics using coupled hydrological-thermal-geophysical inversionStem–root flow effect on soil–atmosphere interactions and uncertainty assessmentsThe effect of different evapotranspiration methods on portraying soil water dynamics and ET partitioning in a semi-arid environment in Northwest ChinaSensitivity of water stress in a two-layered sandy grassland soil to variations in groundwater depth and soil hydraulic parametersUnderstanding NMR relaxometry of partially water-saturated rocksEstimating flow and transport parameters in the unsaturated zone with pore water stable isotopesEstimation of temporal and spatial variations in groundwater recharge in unconfined sand aquifers using Scots pine inventoriesPredicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factorCharacterizing coarse-resolution watershed soil moisture heterogeneity using fine-scale simulationsAssimilation of surface soil moisture into a multilayer soil model: design and evaluation at local scaleEstimating root zone soil moisture using near-surface observations from SMOSInfluence of soil, land use and climatic factors on the hydraulic conductivity of soilImproving soil moisture profile reconstruction from ground-penetrating radar data: a maximum likelihood ensemble filter approachSpatial distribution of solute leaching with snowmelt and irrigation: measurements and simulationsLinking soil moisture balance and source-responsive models to estimate diffuse and preferential components of groundwater rechargeSensitivity of groundwater recharge using climatic analogues and HYDRUS-1D
Thuy Huu Nguyen, Matthias Langensiepen, Jan Vanderborght, Hubert Hüging, Cho Miltin Mboh, and Frank Ewert
Hydrol. Earth Syst. Sci., 24, 4943–4969,Short summary
The mechanistic Couvreur root water uptake (RWU) model that is based on plant hydraulics and links root system properties to RWU, water stress, and crop development can evaluate the impact of certain crop properties on crop performance in different environments and soils, while the Feddes RWU approach does not possess such flexibility. This study also shows the importance of modeling root development and how it responds to water deficiency to predict the impact of water stress on crop growth.
Lianyu Yu, Yijian Zeng, and Zhongbo Su
Hydrol. Earth Syst. Sci., 24, 4813–4830,Short summary
Soil mass and heat transfer processes were represented in three levels of model complexities to understand soil freeze–thaw mechanisms. Results indicate that coupled mass and heat transfer models considerably improved simulations of the soil hydrothermal regime. Vapor flow and thermal effects on water flow are the main mechanisms for the improvements. Given the explicit consideration of airflow, vapor flow and its effects on heat transfer were enhanced during the freeze–thaw transition period.
Jérôme Raimbault, Pierre-Emmanuel Peyneau, Denis Courtier-Murias, Thomas Bigot, Jaime Gil Roca, Béatrice Béchet, and Laurent Lassabatère
Hydrol. Earth Syst. Sci. Discuss.,
Revised manuscript accepted for HESSShort summary
Contaminant transport in soils is known to be affected by soil heterogeneities, such as macropores. The transport properties of heterogeneous porous media can be studied in laboratory columns. However, the results reported in this study (a combination of breakthrough experiments, magnetic resonance imaging and computer simulations of transport) show that these properties can be largely affected by the boundary devices of the columns, thus highlighting the need to take their effect into account.
Zhongyi Liu, Zailin Huo, Chaozi Wang, Limin Zhang, Xianghao Wang, Guanhua Huang, Xu Xu, and Tammo Siert Steenhuis
Hydrol. Earth Syst. Sci., 24, 4213–4237,Short summary
We have developed an integrated surrogate model for arid irrigated areas with shallow groundwater that links crop growth with soil water and salinity in the vadose zone. The model recognizes that field capacity is reached when the matric potential is equal to the height above the groundwater table. The model applies areas with shallow groundwater for which only very few surrogate models are available for most surface irrigation systems in the world without suffering from high groundwater.
M. Shahabul Alam, S. Lee Barbour, and Mingbin Huang
Hydrol. Earth Syst. Sci., 24, 735–759,Short summary
This study quantifies uncertainties in the prediction of long-term water balance for mine reclamation soil covers using random sampling of model parameter distributions. Parameter distributions were obtained from model optimization for field monitoring data. Variability in climate is a greater source of uncertainty than the model parameters in evaporation predictions, while climate variability and model parameters exert similar uncertainty on predictions of net percolation.
Alexander Sternagel, Ralf Loritz, Wolfgang Wilcke, and Erwin Zehe
Hydrol. Earth Syst. Sci., 23, 4249–4267,Short summary
We present our hydrological LAST-Model to simulate preferential soil water flow and tracer transport in macroporous soils. It relies on a Lagrangian perspective of the movement of discrete water particles carrying tracer masses through the subsoil and is hence an alternative approach to common models. Sensitivity analyses reveal the physical validity of the model concept and evaluation tests show that LAST can depict well observed tracer mass profiles with fingerprints of preferential flow.
Lu Zhuo, Qiang Dai, Dawei Han, Ningsheng Chen, and Binru Zhao
Hydrol. Earth Syst. Sci., 23, 4199–4218,Short summary
This study assesses the usability of WRF model-simulated soil moisture for landslide monitoring in northern Italy. In particular, three advanced land surface model schemes (Noah, Noah-MP, and CLM4) are used to provide multi-layer soil moisture data. The results have shown Noah-MP can provide the best landslide monitoring performance. It is also demonstrated that a single soil moisture sensor located in plain area has a high correlation with a significant proportion of the study area.
Xicai Pan, Stefan Jaumann, Jiabao Zhang, and Kurt Roth
Hydrol. Earth Syst. Sci., 23, 3653–3663,Short summary
This study suggests an efficient approach to obtain plot-scale soil hydraulic properties for the shallow structural soils via non-invasive ground-penetrating radar measurements. Facilitated by spatial information of lateral water flow, this approach is more efficient than the widely used inversion approaches relying on intensive soil moisture monitoring. The acquisition of such quantitative information is of great interest to fields such as hydrology and precision agriculture.
John C. Hammond, Adrian A. Harpold, Sydney Weiss, and Stephanie K. Kampf
Hydrol. Earth Syst. Sci., 23, 3553–3570,Short summary
Streamflow in high-elevation and high-latitude areas may be vulnerable to snow loss, making it important to quantify how snowmelt and rainfall are divided between soil storage, drainage below plant roots, evapotranspiration and runoff. We examine this separation in different climates and soils using a physically based model. Results show runoff may be reduced with snowpack decline in all climates. The mechanisms responsible help explain recent observations of streamflow sensitivity to snow loss.
Zhongyi Liu, Xingwang Wang, Zailin Huo, and Tammo Siert Steenhuis
Hydrol. Earth Syst. Sci., 23, 3097–3115,Short summary
A novel approach is taken in simulating the hydrology of the vadose zone in areas with shallow groundwater. The model recognizes that field capacity is reached when the matric potential is equal to the height above the groundwater table. The model can be used in areas with shallow groundwater to optimize irrigation water use and minimize tailwater losses.
Jicai Zeng, Jinzhong Yang, Yuanyuan Zha, and Liangsheng Shi
Hydrol. Earth Syst. Sci., 23, 637–655,Short summary
Accurately capturing the soil-water–groundwater interaction is vital for all disciplines related to subsurface flow but is difficult when undergoing significant nonlinearity in the modeling system. A new soil-water flow package is developed to solve the switching-form Richards’ equation. A multi-scale water balance analysis joins unsaturated–saturated models at separated scales. The whole system is solved efficiently with an iterative feedback coupling scheme.
Noam Zach Dvory, Yakov Livshitz, Michael Kuznetsov, Eilon Adar, Guy Gasser, Irena Pankratov, Ovadia Lev, and Alexander Yakirevich
Hydrol. Earth Syst. Sci., 22, 6371–6381,Short summary
This research is paramount given the significance of karst aquifers as essential drinking water sources. While CBZ is considered conservative, CAF is subject to sorption and degradation, and therefore each of these two pollutants can be considered effective tracers for specific assessment of aquifer contamination. The model presented in this paper shows how each of the mentioned contaminants could serve as a better tool for aquifer contamination characterization and its treatment.
Chen-Chao Chang and Dong-Hui Cheng
Hydrol. Earth Syst. Sci., 22, 4621–4632,Short summary
The soil water retention curve (SWRC) is fundamental to researching water flow and chemical transport in unsaturated media. However, the traditional prediction models underestimate the water content in the dry range of the SWRC. A method was therefore proposed to improve the estimation of the SWRC using a pore model containing slit-shaped spaces. The results show that the predicted SWRCs using the improved method reasonably approximated the measured SWRCs.
Carlos García-Gutiérrez, Yakov Pachepsky, and Miguel Ángel Martín
Hydrol. Earth Syst. Sci., 22, 3923–3932,Short summary
Saturated hydraulic conductivity (Ksat) is an important soil parameter that highly depends on soil's particle size distribution (PSD). The nature of this dependency is explored in this work in two ways, (1) by using the information entropy as a heterogeneity parameter of the PSD and (2) by using descriptions of PSD in forms of textural triplets, different than the usual description in terms of the triplet of sand, silt, and clay contents.
Matthias Sprenger, Doerthe Tetzlaff, Jim Buttle, Hjalmar Laudon, and Chris Soulsby
Hydrol. Earth Syst. Sci., 22, 3965–3981,Short summary
We estimated water ages in the upper critical zone with a soil physical model (SWIS) and found that the age of water stored in the soil, as well as of water leaving the soil via evaporation, transpiration, or recharge, was younger the higher soil water storage (inverse storage effect). Travel times of transpiration and evaporation were different. We conceptualized the subsurface into fast and slow flow domains and the water was usually half as young in the fast as in the slow flow domain.
Conrad Jackisch and Erwin Zehe
Hydrol. Earth Syst. Sci., 22, 3639–3662,Short summary
We present a Lagrangian model for non-uniform soil water dynamics. It handles 2-D diffusion (based on a spatial random walk and implicit pore space redistribution) and 1-D advection in representative macropores (as film flow with dynamic interaction with the soil matrix). The interplay between the domains is calculated based on an energy-balance approach which does not require any additional parameterisation. Model tests give insight into the evolution of the non-uniform infiltration patterns.
Joop Kroes, Iwan Supit, Jos van Dam, Paul van Walsum, and Martin Mulder
Hydrol. Earth Syst. Sci., 22, 2937–2952,Short summary
Impact of upward flow by capillary rise and recirculation on crop yields is often neglected or underestimated. Case studies and model experiments are used to illustrate the impact of this upward flow in the Dutch delta. Neglecting upward flow results in yield reductions for grassland, maize and potatoes. Half of the withheld water behind these yield effects comes from recirculated percolation water as occurs in free-drainage conditions; the other half from increased upward capillary rise.
Stefan Jaumann and Kurt Roth
Hydrol. Earth Syst. Sci., 22, 2551–2573,Short summary
Ground-penetrating radar (GPR) is a noninvasive and nondestructive measurement method to monitor the hydraulic processes precisely and efficiently. We analyze synthetic as well as measured data from the ASSESS test site and show that the analysis yields accurate estimates for the soil hydraulic material properties as well as for the subsurface architecture by comparing the results to references derived from time domain reflectometry (TDR) and subsurface architecture ground truth data.
Gaochao Cai, Jan Vanderborght, Matthias Langensiepen, Andrea Schnepf, Hubert Hüging, and Harry Vereecken
Hydrol. Earth Syst. Sci., 22, 2449–2470,Short summary
Different crop growths had consequences for the parameterization of root water uptake models. The root hydraulic parameters of the Couvreur model but not the water stress parameters of the Feddes–Jarvis model could be constrained by the field data measured from rhizotron facilities. The simulated differences in transpiration from the two soils and the different water treatments could be confirmed by sap flow measurements. The Couvreur model predicted the ratios of transpiration fluxes better.
Coleen D. U. Carranza, Martine J. van der Ploeg, and Paul J. J. F. Torfs
Hydrol. Earth Syst. Sci., 22, 2255–2267,Short summary
Remote sensing has been popular for mapping surface soil moisture. However, estimating subsurface values using surface soil moisture remains a challenge, as decoupling can occur. Depth-integrated soil moisture values used in hydrological models are affected by vertical variability. Using statistical methods, we investigate vertical variability between the surface (5 cm) and subsurface (40 cm) to quantify decoupling. We also discuss potential controls for decoupling during wet and dry conditions.
Rafael Muñoz-Carpena, Claire Lauvernet, and Nadia Carluer
Hydrol. Earth Syst. Sci., 22, 53–70,Short summary
Seasonal shallow water tables (WTs) in lowlands limit vegetation-buffer efficiency to control runoff pollution. Mechanistic models are needed to quantify true field efficiency. A new simplified algorithm for soil infiltration over WTs is tested against reference models and lab data showing WT effects depend on local settings but are negligible after 2 m depth. The algorithm is coupled to a complete vegetation buffer model in a companion paper to analyze pesticide and sediment control in situ.
Claire Lauvernet and Rafael Muñoz-Carpena
Hydrol. Earth Syst. Sci., 22, 71–87,Short summary
Vegetation buffers, often placed in lowlands to control runoff pollution, can exhibit limited efficiency due to seasonal shallow water tables (WTs). A new shallow water table infiltration algorithm developed in a companion paper is coupled to a complete vegetation buffer model to quantify pesticide and sediment control in the field. We evaluated the model on two field experiments in France with and without WT conditions and show WTs can control efficiency depending on land and climate settings.
Tobias Karl David Weber, Sascha Christian Iden, and Wolfgang Durner
Hydrol. Earth Syst. Sci., 21, 6185–6200,
Yonatan Ganot, Ran Holtzman, Noam Weisbrod, Ido Nitzan, Yoram Katz, and Daniel Kurtzman
Hydrol. Earth Syst. Sci., 21, 4479–4493,Short summary
We monitor infiltration at multiple scales during managed aquifer recharge with desalinated seawater in an infiltration pond, while groundwater recharge is evaluated by simplified and numerical models. We found that pond-surface clogging is negated by the high-quality desalinated seawater or negligible compared to the low-permeability layers of the unsaturated zone. We show that a numerical model with a 1-D representative sediment profile is able to capture infiltration and recharge dynamics.
Stefan Jaumann and Kurt Roth
Hydrol. Earth Syst. Sci., 21, 4301–4322,Short summary
We investigate the quantitative effect of neglected sensor position, small-scale heterogeneity, and lateral flow on soil hydraulic material properties. Thus, we analyze a fluctuating water table experiment in a 2-D architecture (ASSESS) with increasingly complex studies based on time domain reflectometry and hydraulic potential data. We found that 1-D studies may yield biased parameters and that estimating sensor positions as well as small-scale heterogeneity improves the model significantly.
Joseph Alexander Paul Pollacco, Trevor Webb, Stephen McNeill, Wei Hu, Sam Carrick, Allan Hewitt, and Linda Lilburne
Hydrol. Earth Syst. Sci., 21, 2725–2737,Short summary
Descriptions of soil hydraulic properties, such as soil moisture release curve, θ(h), and saturated hydraulic conductivities, Ks, are a prerequisite for hydrological models. Because it is usually more difficult to describe Ks than θ(h) from pedotransfer functions, we developed a physical unimodal model to compute Ks solely from hydraulic parameters derived from the Kosugi θ(h). We further adaptations to this model to adapt it to dual-porosity structural soils.
Fadji Hassane Maina and Philippe Ackerer
Hydrol. Earth Syst. Sci., 21, 2667–2683,Short summary
In many fields like climate change, hydrology and agronomy, water movement in unsaturated soils is usually simulated using the Richards equation. However, this equation requires lot of computational effort to be solved due to its highly nonlinear behavior, which hampers its use in simulations. In this paper, we analyze and developed some numerical strategies and we evaluate their reliability and efficiency.
Foad Foolad, Trenton E. Franz, Tiejun Wang, Justin Gibson, Ayse Kilic, Richard G. Allen, and Andrew Suyker
Hydrol. Earth Syst. Sci., 21, 1263–1277,Short summary
Estimates of evapotranspiration are vital for validation of models. However, those datasets are often limited to research applications. Here, we explore using vadose zone modeling with widespread and readily available soil water content monitoring networks. While this work focused on one agricultural site, the framework can be used everywhere there is basic data. The resulting evapotranspiration and soil water content measurements are valuable benchmarks for evaluation of land surface models.
Justin Gibson, Trenton E. Franz, Tiejun Wang, John Gates, Patricio Grassini, Haishun Yang, and Dean Eisenhauer
Hydrol. Earth Syst. Sci., 21, 1051–1062,Short summary
The human use of water for irrigation is often ignored in models and operational forecasts. We describe four plausible and relatively simple irrigation routines that can be coupled to the next generation of models. The routines are tested against a unique irrigation dataset from western Nebraska. The most aggressive water-saving irrigation routine indicates a potential irrigation savings of 120 mm yr−1 and yield losses of less than 3 % against the crop model benchmark and historical averages.
Marcos Alex dos Santos, Quirijn de Jong van Lier, Jos C. van Dam, and Andre Herman Freire Bezerra
Hydrol. Earth Syst. Sci., 21, 473–493,Short summary
Some empirical root water uptake (RWU) models were assessed under varying environmental conditions predicted from numerical simulations with a detailed physical model. The widely used empirical RWU model by Feddes only performs well in scenarios of low RWU compensation. The RWU model by Jarvis cannot mimic the RWU patterns predicted by the physical model for high root length density scenarios. The two proposed models are more capable of predicting similar RWU patterns.
Ke Zhang, Xianwu Xue, Yang Hong, Jonathan J. Gourley, Ning Lu, Zhanming Wan, Zhen Hong, and Rick Wooten
Hydrol. Earth Syst. Sci., 20, 5035–5048,Short summary
We developed a new approach to couple a distributed hydrological model, CREST, to a geotechnical landslide model, TRIGRS, to simulate both flood- and rainfall-triggered landslide hazards. By implementing more sophisticated and realistic representations of hydrological processes in the coupled model system, it shows better performance than the standalone landslide model in the case study. It highlights the important physical connection between rainfall, hydrological processes and slope stability.
Hannes H. Bauser, Stefan Jaumann, Daniel Berg, and Kurt Roth
Hydrol. Earth Syst. Sci., 20, 4999–5014,Short summary
The representation of soil water movement comes with uncertainties in all model components. We assess the key uncertainties for the case of a one-dimensional soil proﬁle with measured water contents. We employ a data assimilation method to represent and reduce the key uncertainties. For intermittent phases where model assumptions are violated, we introduce a "closed-eye period" to bridge the gap. We also demonstrate the need to include heterogeneity.
Muhammad Naveed, Per Moldrup, Marcel G. Schaap, Markus Tuller, Ramaprasad Kulkarni, Hans-Jörg Vogel, and Lis Wollesen de Jonge
Hydrol. Earth Syst. Sci., 20, 4017–4030,Short summary
Quantification of rapid flow of water and associated transport of contaminants through large soil pores generated by earthworms or decaying plant roots is of crucial importance for sustaining both soil and water quality. Advanced visualization and analysis techniques based on state-of-the-art X-ray computed tomography have been applied to 65 soil cores extracted from an agricultural field in Silstrup, Denmark, to improve models for the prediction of fast, preferential flow processes in soils.
Erwin Zehe and Conrad Jackisch
Hydrol. Earth Syst. Sci., 20, 3511–3526,
Anh Phuong Tran, Baptiste Dafflon, Susan S. Hubbard, Michael B. Kowalsky, Philip Long, Tetsu K. Tokunaga, and Kenneth H. Williams
Hydrol. Earth Syst. Sci., 20, 3477–3491,Short summary
Quantifying water and heat fluxes in the shallow subsurface is particularly important due to their strong control on recharge, evaporation and biogeochemical processes. This study developed and tested a new inversion scheme to estimate subsurface hydro-thermal parameters by joint using different hydrological, thermal and geophysical data. It is especially useful for the increasing number of studies that are taking advantage of autonomously collected measurements to explore ecosystem dynamics.
Tzu-Hsien Kuo, Jen-Ping Chen, and Yongkang Xue
Hydrol. Earth Syst. Sci., 20, 1509–1522,Short summary
The stem-root flow mechanism was parameterized and incorporated into the Simplified Simple Biosphere model to analyze its impact on soil moisture and land-atmospheric interactions. By testing against the Lien Hua Chih (Taiwan) and HAPEX-Mobilhy (France) measurements, the model shows that stem-root flow reduced the top-soil moisture content and moistened the deeper soil layers. Such soil moisture redistribution results in significant changes in heat flux exchange between land and atmosphere.
Lianyu Yu, Yijian Zeng, Zhongbo Su, Huanjie Cai, and Zhen Zheng
Hydrol. Earth Syst. Sci., 20, 975–990,Short summary
The coupled water vapor and heat transport model using two different ET (ETdir, ETind) methods varied concerning the simulation of soil moisture and ET components, while agreed well for the simulation of soil temperature. Considering aerodynamic and surface resistance terms improved the ETdir method regarding simulating soil evaporation, especially after irrigation. The interactive effect of crop growth parameters with changing environment played an important role in estimating ET components.
M. Rezaei, P. Seuntjens, I. Joris, W. Boënne, S. Van Hoey, P. Campling, and W. M. Cornelis
Hydrol. Earth Syst. Sci., 20, 487–503,Short summary
The sensitivity of the combined model (LINGRA-N and HYDRUS-1D) to hydraulic parameters, water stress, crop yield and lower boundary conditions was assessed. We showed that it is sufficient to estimate limited amount of key parameters in optimization strategies. A combined modelling approach could increase water use efficiency (12–22.5 %) and yield (5–7%) by changing irrigation scheduling. Result calls for taking into account weather forecast and soil water content data in precision agriculture.
O. Mohnke, R. Jorand, C. Nordlund, and N. Klitzsch
Hydrol. Earth Syst. Sci., 19, 2763–2773,
M. Sprenger, T. H. M. Volkmann, T. Blume, and M. Weiler
Hydrol. Earth Syst. Sci., 19, 2617–2635,Short summary
We present a novel approach that includes information about the pore water stable isotopic composition in inverse model approaches to estimate soil hydraulic parameters. Different approaches are presented and their adequacy regarding the model efficiency, realism and parameter identifiability are discussed. The advantages of the new approach are shown by an application of the inverse estimated parameters to infer the water balance and the transit time for three different study sites.
P. Ala-aho, P. M. Rossi, and B. Kløve
Hydrol. Earth Syst. Sci., 19, 1961–1976,Short summary
We present a novel simulation method for estimating spatially distributed and transient groundwater recharge in unconfined sandy aquifers. The approach uses field data for the most important parameters affecting groundwater recharge and accounts for parameter uncertainty. The results show that tree canopy cover is the most important factor in controlling groundwater recharge at our study area. Tree canopy is thinned by forestry, which may lead to a significant increase of groundwater recharge.
F. Meskini-Vishkaee, M. H. Mohammadi, and M. Vanclooster
Hydrol. Earth Syst. Sci., 18, 4053–4063,
W. J. Riley and C. Shen
Hydrol. Earth Syst. Sci., 18, 2463–2483,
M. Parrens, J.-F. Mahfouf, A. L. Barbu, and J.-C. Calvet
Hydrol. Earth Syst. Sci., 18, 673–689,
T. W. Ford, E. Harris, and S. M. Quiring
Hydrol. Earth Syst. Sci., 18, 139–154,
N. Jarvis, J. Koestel, I. Messing, J. Moeys, and A. Lindahl
Hydrol. Earth Syst. Sci., 17, 5185–5195,
A. P. Tran, M. Vanclooster, and S. Lambot
Hydrol. Earth Syst. Sci., 17, 2543–2556,
D. Schotanus, M. J. van der Ploeg, and S. E. A. T. M. van der Zee
Hydrol. Earth Syst. Sci., 17, 1547–1560,
M. O. Cuthbert, R. Mackay, and J. R. Nimmo
Hydrol. Earth Syst. Sci., 17, 1003–1019,
B. Leterme, D. Mallants, and D. Jacques
Hydrol. Earth Syst. Sci., 16, 2485–2497,
Abdul, A. S. and Gillham, R. W.: Laboratory Studies of the Effects of the Capillary Fringe on Streamflow Generation, Water Resour. Res., 20, 691–698, https://doi.org/10.1029/WR020i006p00691, 1984.
Abdul, A. S. and Gillham, R. W.: Field studies of the effects of the capillary fringe on streamflow generation, J. Hydrol, 112, 1–18, https://doi.org/10.1016/0022-1694(89)90177-7, 1989.
Beven, K. J., Lamb, R., Quinn, P., and Freer, R.: TOPMODEL, in: Computer Models of Watershed Hydrology, edited by: Singh, V. P., USA, Water Resources Publication, 627–668, 1995.
Bierkens, M. F. P.: Modeling water table fluctuations by means of a stochastic differential equation, Water Resour. Res., 34, 2485–2499, https://doi.org/10.1029/98WR02298, 1998.
Brooks, R. H. and Corey, A. T.: Hydraulic Properties of Porous Media, Tech. Rep., Agricultural Research Service, Soil and Water Conservation Research Division, and the Agricultural Engineering Dept., Colorado State Univ., Fort Collins, Colorado, 1964.
Castelli, F.: A simplified stochastic model for infiltration into a heterogeneous soil forced by random precipitation, Adv. Water Resour., 19, 133–144, https://doi.org/10.1016/0309-1708(95)00041-0, 1996.
Castelli, F., Menduni, G., and Mazzanti, B.: A distributed package for sustainable water management: a case study in the Arno Basin, in: Proceeding of The role of Hydrology in Water Resources Management, Capri, Italy, October 2008, IAHS, 327, 52–61, 2009.
Castillo, A., Castelli, F., and Entekhabi, D.: Gravitational and capillary soil moisture dynamics for distributed hydrologic models, Hydrol. Earth Syst. Sci., 19, 1857–1869, https://doi.org/10.5194/hess-19-1857-2015, 2015.
Castillo, A. E.: Spatiotemporal variability of hydrologic response: an entropy-based approach using a distributed hydrologic model, PhD thesis, Massachusetts Institute of Technology, USA, 189 pp., 2014.
Centre for High Performance Scientific Computing in Terrestrial System HPSCTerrSys: available at: http://www.hpsc-terrsys.de, last access: 7 April 2019.
Chenjerayi Guzha, A. and Hardy, T. B.: Simulating streamflow and water table depth with a coupled hydrological model, Water Science and Engineering, 3, 241–256, https://doi.org/10.3882/j.issn.1674-2370.2010.03.001, 2010.
Chung, I., Kim, N.-W., Lee, J., and Sophocleous, M.: Assessing distributed groundwater recharge rate using integrated surface water-groundwater modelling: application to Mihocheon watershed, South Korea, Hydrogeol. J., 18, 1253–1264, https://doi.org/10.1007/s10040-010-0593-1, 2010.
Cloke, H. L., Anderson, M. G., McDonnell, J. J., and Renaud, J.-P.: Using numerical modelling to evaluate the capillary fringe groundwater ridging hypothesis of streamflow generation, J. Hydrol., 316, 141–162, https://doi.org/10.1016/j.jhydrol.2005.04.017, 2006.
DHI: MIKE SHE User Manual, Volume 2, Reference Guide, Danish Hydraulic Institute, 372 pp., 2014.
Downer, C. W. and Ogden, F. L.: Appropriate vertical discretization of Richards' equation for two-dimensional watershed-scale modelling, Hydrol. Process., 18, 1–22, https://doi.org/10.1002/hyp.1306, 2004.
Duffy, C. J.: Semi-Discrete Dynamical Model for Mountain-Front Recharge and Water Balance Estimation, Rio Grande of Southern Colorado and New Mexico, in: Groundwater Recharge in a Desert Environment: The Southwestern United States, edited by: Hogan, J. F., Philips, F. M., and Scanlon, B. R., American Geophysical Union (AGU), 255–271, https://doi.org/10.1029/009WSA14, 2013.
Duke, H. R.: Capillary properties of soils-Influence upon specific yield, Trans. ASAE, 15, 688–691, 1972.
Dunne, T. and Black, R. D.: An Experimental Investigation of Runoff Production in Permeable Soils, Water Resour. Res., 6, 478–490, https://doi.org/10.1029/WR006i002p00478, 1970.
Dupuit, J.: Etudes théoriques et pratiques sur le mouvement des eaux courantes suivies de considérations relatives au régime des grandes eaux, au débouché à leur donner, et a la marche des alluvions dans les rivières à fond mobile Carilian-Goeury et Dalmont, France, 1848.
Government of Canada: Historical Climate data, available at: http://climate.weatheroffice.ec.gc.ca, last access: 7 April 2019.
Graham, D. and Butts, M. B.: Flexible Integrated Watershed Modeling with MIKE SHE, in: Watershed models, edited by: Frevert, D. and Singh, V., CRC Press, 245–271, 2005.
Guzha, A.: Integrating Surface and Sub Surface Flow Models of Different Spatial and Temporal Scales Using Potential Coupling Interfaces, PhD thesis, Utah State University, USA, 243 pp., 2008.
Healy, R. W. and Cook, P. G.: Using groundwater levels to estimate recharge, Hydrogeol. J., 10, 91–109, https://doi.org/10.1007/s10040-001-0178-0, 2002.
Hilberts, A. G. J., Troch, P. A., and Paniconi, C.: Storage-dependent drainable porosity for complex hillslopes, Water Resour. Res., 41, W06001, https://doi.org/10.1029/2004WR003725, 2005.
Jayatilaka, C. J. and Gillham, R. W.: A deterministic-empirical model of the effect of the capillary fringe on near-stream area runoff 1. Description of the model, J. Hydrol., 184, 299–315, https://doi.org/10.1016/0022-1694(95)02985-0, 1996.
Jones, J. P., Sudicky, E. A., Brookfield, A. E., and Park, Y.-J.: An assessment of the tracer-based approach to quantifying groundwater contributions to streamflow, Water Resour. Res., 42, W02407, https://doi.org/10.1029/2005WR004130, 2006.
Kollet, S., Sulis, M., Maxwell, R. M., Paniconi, C., Putti, M., Bertoldi, G., and Sudicky, E.: The integrated hydrologic model intercomparison project, IH-MIP2: A second set of benchmark results to diagnose integrated hydrology and feedbacks, Water Resour. Res., 53, 867–890, https://doi.org/10.1002/2016WR019191, 2017.
Kollet, S. J. and Maxwell, R.: Integrated surface–groundwater flow modeling: A free-surface overland flow boundary condition in a parallel groundwater flow model, Adv. Water Resour., 29, 945–958, https://doi.org/10.1016/j.advwatres.2005.08.006, 2006.
Markstrom, S., Niswonger, R., Regan, R., Prudic, D., and Barlow, P.: GSFLOW – Coupled Ground-Water and Surface-Water Flow Model Based on the Integration of the Precipitation-Runoff Modeling System (PRMS) and the Modular Ground-Water Flow Model (MODFLOW-2005), Open File Rep. 6-D1, 254 pp., 2008.
McDonnell, J. J. and Taylor, C. H.: Surface and subsurface water contributions during snowmelt in a small Precambrian Shield watershed, Muskoka, Ontario, Atmos. Ocean, 25, 251–266, https://doi.org/10.1080/07055900.1987.9649274, 1987.
Nachabe, M. H.: Analytical expressions for transient specific yield and shallow water table drainage, Water Resour. Res., 38, 1193, https://doi.org/10.1029/2001WR001071, 2002.
Neitsch, S. L., Arnold, J. G., Kiniry, J. R., and Williams, J. R.: Soil and Water Assessment Tool, Theoritical Documentation Version 2009, Technical Report No. 406, Texas Water Resources Institute, 647 pp., 2011.
Rawls, W. J., Brakensiek, D. L., and Saxtonn, K. E.: Estimation of soil water properties, T. ASAE, 25, 1316–1320, 1982.
Refsgaard, C. J. and Storm, B.: MIKESHE, in: Computer models of catchment hydrology, edited by: Singh, V. P., Water resources publications, 809–846, 1995.
Seibert, J., Rodhe, A., and Bishop, K.: Simulating interactions between saturated and unsaturated storage in a conceptual runoff model, Hydrol. Process., 17, 379–390, https://doi.org/10.1002/hyp.1130, 2003.
Shah, N., Nachabe, M., and Ross, M.: Extinction Depth and Evapotranspiration from Ground Water under Selected Land Covers, Ground Water, 45, 329–338, https://doi.org/10.1111/j.1745-6584.2007.00302.x, 2007.
Storm, B.: Modeling of Saturated Flow and the Coupling of Surface and Subsurface Flow, in: Recent advances in the modelling of hydrologic systems, edited by: Bowles, D. S. and O'Connell, P. E., Springer Netherlands, 185–203, https://doi.org/10.1007/978-94-011-3480-4_10, 1991.
VanderKwaak, J. E.: Numerical simulation of flow and chemical transport in integrated surface-subsurface hydrologic system, PhD thesis, University of Waterloo, Canada, 243 pp., 1999.
Modelling of shallow water table fluctuations is usually carried out using physically based numerical models. These models have notable limitations regarding intensive required data and computational burden. This paper presents an alternative modelling approach for modelling of such cases by introducing modifications to the calculation of groundwater recharge and saturated flow of a conceptual hydrologic model.
Modelling of shallow water table fluctuations is usually carried out using physically based...