Articles | Volume 22, issue 6
https://doi.org/10.5194/hess-22-3295-2018
© Author(s) 2018. 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-22-3295-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Jun 2018
Research article |
| 13 Jun 2018
| 13 Jun 2018
On the appropriate definition of soil profile configuration and initial conditions for land surface–hydrology models in cold regions
Gonzalo Sapriza-Azuri
CORRESPONDING AUTHOR
Departamento del Agua, Centro Universitario Regional Litoral Norte,
Universidad de la República, Salto, Uruguay
Pablo Gamazo
Departamento del Agua, Centro Universitario Regional Litoral Norte,
Universidad de la República, Salto, Uruguay
Saman Razavi
Global Institute for Water Security, University of Saskatchewan,
Saskatoon, SK, Canada
School of Environment and Sustainability, University of Saskatchewan,
Saskatoon, SK, Canada
Department of Civil and Geological Engineering, University of
Saskatchewan, Saskatoon, SK, Canada
Howard S. Wheater
Global Institute for Water Security, University of Saskatchewan,
Saskatoon, SK, Canada
School of Environment and Sustainability, University of Saskatchewan,
Saskatoon, SK, Canada
Department of Civil and Geological Engineering, University of
Saskatchewan, Saskatoon, SK, Canada
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- Assimilation of Satellite-Based Snow Cover and Freeze/Thaw Observations Over High Mountain Asia Y. Xue et al. 10.3389/feart.2019.00115
- Multifactorial Principal‐Monotonicity Inference for Macro‐Scale Distributed Hydrologic Modeling G. Cheng et al. 10.1029/2021WR031370
- A New Tool for Mapping Water Yield in Cold Alpine Regions L. Zhao et al. 10.3390/w15162920
- Soil hydrology in the Earth system H. Vereecken et al. 10.1038/s43017-022-00324-6
- Summary and synthesis of Changing Cold Regions Network (CCRN) research in the interior of western Canada – Part 2: Future change in cryosphere, vegetation, and hydrology C. DeBeer et al. 10.5194/hess-25-1849-2021
- Improved ELMv1-ECA simulations of zero-curtain periods and cold-season CH<sub>4</sub> and CO<sub>2</sub> emissions at Alaskan Arctic tundra sites J. Tao et al. 10.5194/tc-15-5281-2021
- Water and heat coupling processes and its simulation in frozen soils: Current status and future research directions G. Hu et al. 10.1016/j.catena.2022.106844
- Impacts of seasonally frozen soil hydrothermal dynamics on the watershed hydrological processes inferred from a spatially distributed numerical modelling approach H. Gao et al. 10.1016/j.jhydrol.2023.129947
- Development of a macroscale distributed hydro-modeling method: Bayesian principal-monotonicity inference G. Cheng et al. 10.1016/j.jhydrol.2022.128803
- On the configuration and initialization of a large-scale hydrological land surface model to represent permafrost M. Elshamy et al. 10.5194/hess-24-349-2020
- Challenges in Hydrologic‐Land Surface Modeling of Permafrost Signatures—A Canadian Perspective M. Abdelhamed et al. 10.1029/2022MS003013
- Representation and improved parameterization of reservoir operation in hydrological and land-surface models F. Yassin et al. 10.5194/hess-23-3735-2019
- Dynamics of the freeze–thaw front of active layer on the Qinghai-Tibet Plateau G. Hu et al. 10.1016/j.geoderma.2023.116353
- Increasing the Depth of a Land Surface Model. Part I: Impacts on the Subsurface Thermal Regime and Energy Storage 10.1175/JHM-D-21-0024.1
- The sources of supra-permafrost water and its hydrological effect based on stable isotopes in the third pole region Z. Li et al. 10.1016/j.scitotenv.2020.136911
- Increasing the Depth of a Land Surface Model. Part II: Temperature Sensitivity to Improved Subsurface Thermodynamics and Associated Permafrost Response 10.1175/JHM-D-21-0023.1
- Hydrologic‐land surface modelling of the Canadian sporadic‐discontinuous permafrost: Initialization and uncertainty propagation M. Abdelhamed et al. 10.1002/hyp.14509
- Advances in modelling large river basins in cold regions with Modélisation Environmentale Communautaire—Surface and Hydrology (MESH), the Canadian hydrological land surface scheme H. Wheater et al. 10.1002/hyp.14557
- On the Spin‐Up Strategy for Spatial Modeling of Permafrost Dynamics: A Case Study on the Qinghai‐Tibet Plateau H. Ji et al. 10.1029/2021MS002750
20 citations as recorded by crossref.
- Permafrost variability over the Northern Hemisphere based on the MERRA-2 reanalysis J. Tao et al. 10.5194/tc-13-2087-2019
- Assimilation of Satellite-Based Snow Cover and Freeze/Thaw Observations Over High Mountain Asia Y. Xue et al. 10.3389/feart.2019.00115
- Multifactorial Principal‐Monotonicity Inference for Macro‐Scale Distributed Hydrologic Modeling G. Cheng et al. 10.1029/2021WR031370
- A New Tool for Mapping Water Yield in Cold Alpine Regions L. Zhao et al. 10.3390/w15162920
- Soil hydrology in the Earth system H. Vereecken et al. 10.1038/s43017-022-00324-6
- Summary and synthesis of Changing Cold Regions Network (CCRN) research in the interior of western Canada – Part 2: Future change in cryosphere, vegetation, and hydrology C. DeBeer et al. 10.5194/hess-25-1849-2021
- Improved ELMv1-ECA simulations of zero-curtain periods and cold-season CH<sub>4</sub> and CO<sub>2</sub> emissions at Alaskan Arctic tundra sites J. Tao et al. 10.5194/tc-15-5281-2021
- Water and heat coupling processes and its simulation in frozen soils: Current status and future research directions G. Hu et al. 10.1016/j.catena.2022.106844
- Impacts of seasonally frozen soil hydrothermal dynamics on the watershed hydrological processes inferred from a spatially distributed numerical modelling approach H. Gao et al. 10.1016/j.jhydrol.2023.129947
- Development of a macroscale distributed hydro-modeling method: Bayesian principal-monotonicity inference G. Cheng et al. 10.1016/j.jhydrol.2022.128803
- On the configuration and initialization of a large-scale hydrological land surface model to represent permafrost M. Elshamy et al. 10.5194/hess-24-349-2020
- Challenges in Hydrologic‐Land Surface Modeling of Permafrost Signatures—A Canadian Perspective M. Abdelhamed et al. 10.1029/2022MS003013
- Representation and improved parameterization of reservoir operation in hydrological and land-surface models F. Yassin et al. 10.5194/hess-23-3735-2019
- Dynamics of the freeze–thaw front of active layer on the Qinghai-Tibet Plateau G. Hu et al. 10.1016/j.geoderma.2023.116353
- Increasing the Depth of a Land Surface Model. Part I: Impacts on the Subsurface Thermal Regime and Energy Storage 10.1175/JHM-D-21-0024.1
- The sources of supra-permafrost water and its hydrological effect based on stable isotopes in the third pole region Z. Li et al. 10.1016/j.scitotenv.2020.136911
- Increasing the Depth of a Land Surface Model. Part II: Temperature Sensitivity to Improved Subsurface Thermodynamics and Associated Permafrost Response 10.1175/JHM-D-21-0023.1
- Hydrologic‐land surface modelling of the Canadian sporadic‐discontinuous permafrost: Initialization and uncertainty propagation M. Abdelhamed et al. 10.1002/hyp.14509
- Advances in modelling large river basins in cold regions with Modélisation Environmentale Communautaire—Surface and Hydrology (MESH), the Canadian hydrological land surface scheme H. Wheater et al. 10.1002/hyp.14557
- On the Spin‐Up Strategy for Spatial Modeling of Permafrost Dynamics: A Case Study on the Qinghai‐Tibet Plateau H. Ji et al. 10.1029/2021MS002750
Latest update: 24 Apr 2024
Short summary
Arctic and subarctic regions are amongst the most susceptible regions on Earth to climate change. There, models require a proper representation of the interactions between climate and hydrology. Typically these model represent the soil with shallow depths, whereas for cold regions, deep soil is needed. To address this, we run model experiments to characterize the effect of soil depth and temperature soil initialization. Our results demonstrate that 20 m of soil profile is essential.
Arctic and subarctic regions are amongst the most susceptible regions on Earth to climate...
