Articles | Volume 21, issue 1
https://doi.org/10.5194/hess-21-459-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-21-459-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Towards a simple representation of chalk hydrology in land surface modelling
Department of Civil Engineering, University of Bristol, Bristol, UK
Rafael Rosolem
Department of Civil Engineering, University of Bristol, Bristol, UK
Cabot Institute, University of Bristol, Bristol, UK
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Cited
16 citations as recorded by crossref.
- Improving the Representation of Subsurface Water Movement in Land Models S. Gharari et al. 10.1175/JHM-D-19-0108.1
- Hillslope Hydrology in Global Change Research and Earth System Modeling Y. Fan et al. 10.1029/2018WR023903
- Modelling karst vadose zone hydrology and its relevance for paleoclimate reconstruction A. Hartmann & A. Baker 10.1016/j.earscirev.2017.08.001
- Modelling flow and heat transfer through unsaturated chalk – Validation with experimental data from the ground surface to the aquifer D. Thiéry et al. 10.1016/j.jhydrol.2017.11.041
- Infiltration from the Pedon to Global Grid Scales: An Overview and Outlook for Land Surface Modeling H. Vereecken et al. 10.2136/vzj2018.10.0191
- Land surface model performance using cosmic-ray and point-scale soil moisture measurements for calibration J. Iwema et al. 10.5194/hess-21-2843-2017
- A soil moisture monitoring network to characterize karstic recharge and evapotranspiration at five representative sites across the globe R. Berthelin et al. 10.5194/gi-9-11-2020
- The unexplored role of preferential flow in soil carbon dynamics S. Franklin et al. 10.1016/j.soilbio.2021.108398
- Can hydrological models assess the impact of natural flood management in groundwater‐dominated catchments? H. Badjana et al. 10.1111/jfr3.12912
- Experimental Coupling of TOPMODEL with the National Water Model: Effects of Coupling Interface Complexity on Model Performance D. Kim et al. 10.1111/1752-1688.12953
- Geological controls of discharge variability in the Thames Basin, UK from cross-spectral analyses: Observations versus modelling G. Weedon et al. 10.1016/j.jhydrol.2023.130104
- V2Karst V1.1: a parsimonious large-scale integrated vegetation–recharge model to simulate the impact of climate and land cover change in karst regions F. Sarrazin et al. 10.5194/gmd-11-4933-2018
- An evapotranspiration model driven by remote sensing data for assessing groundwater resource in karst watershed C. Ollivier et al. 10.1016/j.scitotenv.2021.146706
- Perceptual perplexity and parameter parsimony K. Beven & N. Chappell 10.1002/wat2.1530
- Using observed river flow data to improve the hydrological functioning of the JULES land surface model (vn4.3) used for regional coupled modelling in Great Britain (UKC2) A. Martínez-de la Torre et al. 10.5194/gmd-12-765-2019
- Blue and green water re-distribution dependency on precipitation datasets for a tropical Indian River basin A. Dey et al. 10.1016/j.ejrh.2023.101361
16 citations as recorded by crossref.
- Improving the Representation of Subsurface Water Movement in Land Models S. Gharari et al. 10.1175/JHM-D-19-0108.1
- Hillslope Hydrology in Global Change Research and Earth System Modeling Y. Fan et al. 10.1029/2018WR023903
- Modelling karst vadose zone hydrology and its relevance for paleoclimate reconstruction A. Hartmann & A. Baker 10.1016/j.earscirev.2017.08.001
- Modelling flow and heat transfer through unsaturated chalk – Validation with experimental data from the ground surface to the aquifer D. Thiéry et al. 10.1016/j.jhydrol.2017.11.041
- Infiltration from the Pedon to Global Grid Scales: An Overview and Outlook for Land Surface Modeling H. Vereecken et al. 10.2136/vzj2018.10.0191
- Land surface model performance using cosmic-ray and point-scale soil moisture measurements for calibration J. Iwema et al. 10.5194/hess-21-2843-2017
- A soil moisture monitoring network to characterize karstic recharge and evapotranspiration at five representative sites across the globe R. Berthelin et al. 10.5194/gi-9-11-2020
- The unexplored role of preferential flow in soil carbon dynamics S. Franklin et al. 10.1016/j.soilbio.2021.108398
- Can hydrological models assess the impact of natural flood management in groundwater‐dominated catchments? H. Badjana et al. 10.1111/jfr3.12912
- Experimental Coupling of TOPMODEL with the National Water Model: Effects of Coupling Interface Complexity on Model Performance D. Kim et al. 10.1111/1752-1688.12953
- Geological controls of discharge variability in the Thames Basin, UK from cross-spectral analyses: Observations versus modelling G. Weedon et al. 10.1016/j.jhydrol.2023.130104
- V2Karst V1.1: a parsimonious large-scale integrated vegetation–recharge model to simulate the impact of climate and land cover change in karst regions F. Sarrazin et al. 10.5194/gmd-11-4933-2018
- An evapotranspiration model driven by remote sensing data for assessing groundwater resource in karst watershed C. Ollivier et al. 10.1016/j.scitotenv.2021.146706
- Perceptual perplexity and parameter parsimony K. Beven & N. Chappell 10.1002/wat2.1530
- Using observed river flow data to improve the hydrological functioning of the JULES land surface model (vn4.3) used for regional coupled modelling in Great Britain (UKC2) A. Martínez-de la Torre et al. 10.5194/gmd-12-765-2019
- Blue and green water re-distribution dependency on precipitation datasets for a tropical Indian River basin A. Dey et al. 10.1016/j.ejrh.2023.101361
Latest update: 14 Dec 2024
Short summary
Modelling water flow through chalk (a fine-grained porous medium traversed by fractures) is important for optimizing water resource management practices in the UK. However, efficient simulations of water movement through chalk are difficult due to the porous nature of chalk, creating high-velocity preferential flow paths. This paper describes a novel approach to representing chalk hydrology in land surface modelling for large-scale applications.
Modelling water flow through chalk (a fine-grained porous medium traversed by fractures) is...