Articles | Volume 19, issue 10
https://doi.org/10.5194/hess-19-4317-2015
© Author(s) 2015. 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-19-4317-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impacts of grid resolution on surface energy fluxes simulated with an integrated surface-groundwater flow model
Meteorological Institute, University of Bonn, Bonn, Germany
Meteorological Institute, University of Bonn, Bonn, Germany
C. Simmer
Meteorological Institute, University of Bonn, Bonn, Germany
Centre for High-Performance Scientific Computing in Terrestrial Systems, Geoverbund ABC/J, Jülich, Germany
S. Kollet
Forschungszentrum Jülich GmbH, Jülich, Germany
Centre for High-Performance Scientific Computing in Terrestrial Systems, Geoverbund ABC/J, Jülich, Germany
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33 citations as recorded by crossref.
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- Modelling convectively induced secondary circulations in the terra incognita with TerrSysMP S. Poll et al. 10.1002/qj.3088
- Why Do Large‐Scale Land Surface Models Produce a Low Ratio of Transpiration to Evapotranspiration? L. Chang et al. 10.1029/2018JD029159
- Estimating dominant runoff modes across the conterminous United States B. Buchanan et al. 10.1002/hyp.13296
- Quantifying the Impact of Subsurface‐Land Surface Physical Processes on the Predictive Skill of Subseasonal Mesoscale Atmospheric Simulations M. Sulis et al. 10.1029/2017JD028187
- Can a Sparse Network of Cosmic Ray Neutron Sensors Improve Soil Moisture and Evapotranspiration Estimation at the Larger Catchment Scale? F. Li et al. 10.1029/2023WR035056
- The effects of applying different DEM resolutions, DEM sources and flow tracing algorithms on LS factor and sediment yield estimation using USLE in Barajin river basin (BRB), Iran A. Azizian & S. Koohi 10.1007/s10333-021-00847-6
- Improvement of soil moisture and groundwater level estimations using a scale‐consistent river parameterization for the coupled ParFlow-CLM hydrological model: A case study of the Upper Rhine Basin S. Soltani et al. 10.1016/j.jhydrol.2022.127991
- Effects of Water-Table Configuration on the Planetary Boundary Layer over the San Joaquin River Watershed, California J. Gilbert et al. 10.1175/JHM-D-16-0134.1
- Accuracy of sedimentgraph modeling from topography map scale and DEM mesh size S. Sadeghi et al. 10.1016/j.iswcr.2019.01.002
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- Coupling Groundwater, Vegetation, and Atmospheric Processes: A Comparison of Two Integrated Models M. Sulis et al. 10.1175/JHM-D-16-0159.1
- The Limits of Homogenization: What Hydrological Dynamics can a Simple Model Represent at the Catchment Scale? H. Wen et al. 10.1029/2020WR029528
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- Continental Hydrologic Intercomparison Project, Phase 1: A Large‐Scale Hydrologic Model Comparison Over the Continental United States D. Tijerina‐Kreuzer et al. 10.1029/2020WR028931
- Continental-scale evaluation of a fully distributed coupled land surface and groundwater model, ParFlow-CLM (v3.6.0), over Europe B. Naz et al. 10.5194/gmd-16-1617-2023
- Connections between groundwater flow and transpiration partitioning R. Maxwell & L. Condon 10.1126/science.aaf7891
- A high-resolution, 3D groundwater-surface water simulation of the contiguous US: Advances in the integrated ParFlow CONUS 2.0 modeling platform C. Yang et al. 10.1016/j.jhydrol.2023.130294
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Saved (final revised paper)
Latest update: 23 Nov 2024
Short summary
This study highlights the grid resolution dependence of energy and water balance of the 3-D physically based integrated surface-groundwater model. The non-local controls of soil moisture were found to be highly grid resolution dependent, but the local vegetation control strongly modulates the scaling behavior of surface energy fluxes. For coupled runs, variability in patterns of surface fluxes due to this scale dependence can affect the simulated atmospheric boundary layer and local circulation.
This study highlights the grid resolution dependence of energy and water balance of the 3-D...