Data Files for Runoff Evaluation in an Earth System Land Model for Permafrost Regions

Modeling of hydrological runoff is essential for accurately capturing spatiotemporal feedbacks within the land–atmosphere system, particularly in sensitive regions such as permafrost landscapes. However, substantial uncertainties persist in the terrestrial runoff parameterization schemes used in Earth system and land surface models. This is particularly true in permafrost regions, where landscape heterogeneity is high and reliable observational data are scarce. In this study, we evaluate the performance of runoff parameterization schemes in the Energy Exascale Earth System Model (E3SM) land model (ELM). Our proposed framework leverages simulation results from the Advanced Terrestrial Simulator (ATS), which is a physics-rich integrated surface/subsurface hydrologic model that has been successfully evaluated previously in Arctic tundra regions. We used ATS to simulate runoff from 22 representative hillslopes in the Sagavanirktok River basin, located on the North Slope of Alaska, then compared the output with ELM’s parameterized representation of total runoff. Results show that 1) ELM’s total runoff was the same order of magnitude as the ATS simulations, and both models were similarly variable over time; 2) minor adjustments to coefficients in ELM’s runoff parameterization improved the match between the ATS simulation and ELM’s parameterized representation of annual and seasonal total runoff; 3) overall, runoff responses in ATS and ELM are more similar in flat hillslope environments compared to steep hillslopes; and 4) shallower active layer thicknesses and higher precipitation simulations resulted in lower correlations between the two models due to greater total runoff. By incorporating the optimized runoff coefficients from the Sagavanirktok River basin into ELM, the simulated total runoff better matched the streamflow observations at a small watershed located on the Seward Peninsula of Alaska. Our findings revealed important insights into the effectiveness of runoff parameterizations in land surface models and pathways for improving runoff coefficients in typical Arctic regions. This data set includes all files that were produced and applied in the paper, which is in review as of July 1 2025 in Geoscientific Model Development (GMD).

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-07-04
DOI
https://doi.org/10.5281/zenodo.15809186
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
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article

Data Files for Runoff Evaluation in an Earth System Land Model for Permafrost Regions

Zenodo (CERN European Organization for Nuclear Research)
Climate change and permafrost
article

Data Files for Runoff Evaluation in an Earth System Land Model for Permafrost Regions

article en

Abstract

Modeling of hydrological runoff is essential for accurately capturing spatiotemporal feedbacks within the land–atmosphere system, particularly in sensitive regions such as permafrost landscapes. However, substantial uncertainties persist in the terrestrial runoff parameterization schemes used in Earth system and land surface models. This is particularly true in permafrost regions, where landscape heterogeneity is high and reliable observational data are scarce. In this study, we evaluate the performance of runoff parameterization schemes in the Energy Exascale Earth System Model (E3SM) land model (ELM). Our proposed framework leverages simulation results from the Advanced Terrestrial Simulator (ATS), which is a physics-rich integrated surface/subsurface hydrologic model that has been successfully evaluated previously in Arctic tundra regions. We used ATS to simulate runoff from 22 representative hillslopes in the Sagavanirktok River basin, located on the North Slope of Alaska, then compared the output with ELM’s parameterized representation of total runoff. Results show that 1) ELM’s total runoff was the same order of magnitude as the ATS simulations, and both models were similarly variable over time; 2) minor adjustments to coefficients in ELM’s runoff parameterization improved the match between the ATS simulation and ELM’s parameterized representation of annual and seasonal total runoff; 3) overall, runoff responses in ATS and ELM are more similar in flat hillslope environments compared to steep hillslopes; and 4) shallower active layer thicknesses and higher precipitation simulations resulted in lower correlations between the two models due to greater total runoff. By incorporating the optimized runoff coefficients from the Sagavanirktok River basin into ELM, the simulated total runoff better matched the streamflow observations at a small watershed located on the Seward Peninsula of Alaska. Our findings revealed important insights into the effectiveness of runoff parameterizations in land surface models and pathways for improving runoff coefficients in typical Arctic regions. This data set includes all files that were produced and applied in the paper, which is in review as of July 1 2025 in Geoscientific Model Development (GMD).

Zenodo (CERN European Organization for Nuclear Research)
Oak Ridge National Laboratory (US), Los Alamos National Laboratory (US), Independent Sector (US)
Life in Land
Openalex Percentile: Top 54%
Climate change and permafrost
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