Articles | Volume 13, issue 5
https://doi.org/10.5194/gmd-13-2259-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-13-2259-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model evaluation paper
| 
13 May 2020
Model evaluation paper |
| 13 May 2020
| 13 May 2020
Evaluating integrated surface/subsurface permafrost thermal hydrology models in ATS (v0.88) against observations from a polygonal tundra site
Ahmad Jan
Climate Change Science Institute and Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA
Ethan T. Coon
Climate Change Science Institute and Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA
Scott L. Painter
CORRESPONDING AUTHOR
Climate Change Science Institute and Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA
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Cited
29 citations as recorded by crossref.
- HydroCAL: A novel integrated surface–subsurface hydrological model based on the Cellular Automata paradigm L. Furnari et al. 10.1016/j.advwatres.2024.104623
- Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw S. Painter et al. 10.1073/pnas.2212171120
- Evaluating integrated surface/subsurface permafrost thermal hydrology models in ATS (v0.88) against observations from a polygonal tundra site A. Jan et al. 10.5194/gmd-13-2259-2020
- Permafrost thermal conditions are sensitive to shifts in snow timing A. Jan & S. Painter 10.1088/1748-9326/ab8ec4
- Numerical modeling and simulation of thermo-hydrologic processes in frozen soils on the Qinghai-Tibet Plateau J. Hu et al. 10.1016/j.ejrh.2022.101050
- Numerical analysis of thermo-water-vapor-carbon coupling in a permafrost region: a case study in the Beiluhe area of the Qinghai-Tibetan Plateau H. WEI et al. 10.1016/j.pedsph.2024.09.006
- Upscaling an Extended Heterogeneous Stefan Problem from the Pore-Scale to the Darcy Scale in Permafrost M. Peszynska et al. 10.1137/23M1552000
- Permafrost modelling with OpenFOAM®: New advancements of the permaFoam solver L. Orgogozo et al. 10.1016/j.cpc.2022.108541
- Simulating site-scale permafrost hydrology: Sensitivity to modelling decisions and air temperature S. Krogh & J. Pomeroy 10.1016/j.jhydrol.2021.126771
- Advances in Permafrost Representation: Biophysical Processes in Earth System Models and the Role of Offline Models H. Matthes et al. 10.1002/ppp.2269
- Continentality determines warming or cooling impact of heavy rainfall events on permafrost A. Hamm et al. 10.1038/s41467-023-39325-4
- The effect of seasonally frozen ground on rainfall infiltration and groundwater discharge in Qinghai Lake Basin, China C. Ding et al. 10.3389/frwa.2024.1495763
- Effects of climate change on depression‐focused groundwater recharge in the Canadian Prairies A. Negm et al. 10.1002/vzj2.20153
- New insights into the drainage of inundated ice-wedge polygons using fundamental hydrologic principles D. Harp et al. 10.5194/tc-15-4005-2021
- Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions X. Yang et al. 10.3389/feart.2021.721009
- The impacts of vegetation on the soil surface freezing-thawing processes at permafrost southern edge simulated by an improved process-based ecosystem model Z. Liu et al. 10.1016/j.ecolmodel.2021.109663
- The importance of freeze–thaw cycles for lateral tracer transport in ice-wedge polygons E. Jafarov et al. 10.5194/tc-16-851-2022
- Limited control of microtopography evolution on ground subsidence in polygonal tundra landscapes A. Khattak & A. Hamm 10.1016/j.scitotenv.2024.174741
- Evaluating simplifications of subsurface process representations for field-scale permafrost hydrology models B. Gao & E. Coon 10.5194/tc-16-4141-2022
- Surface energy balance of sub‐Arctic roads with varying snow regimes and properties in permafrost regions L. Chen et al. 10.1002/ppp.2129
- How does humidity data impact land surface modeling of hydrothermal regimes at a permafrost site in Utqiaġvik, Alaska? X. Huang et al. 10.1016/j.scitotenv.2023.168697
- Explicitly modelling microtopography in permafrost landscapes in a land surface model (JULES vn5.4_microtopography) N. Smith et al. 10.5194/gmd-15-3603-2022
- A hydrogeophysical framework to assess infiltration during a simulated ecosystem-scale flooding experiment M. Adebayo et al. 10.1016/j.jhydrol.2023.130243
- Guidelines for cold‐regions groundwater numerical modeling P. Lamontagne‐Hallé et al. 10.1002/wat2.1467
- Guidelines for Publicly Archiving Terrestrial Model Data to Enhance Usability, Intercomparison, and Synthesis M. Simmonds et al. 10.5334/dsj-2022-003
- Permafrost Promotes Shallow Groundwater Flow and Warmer Headwater Streams Y. Sjöberg et al. 10.1029/2020WR027463
- The thermal response of permafrost to coastal floodplain flooding Y. Zhang et al. 10.1088/1748-9326/acba32
- Impact of Summer Air Temperature on Water and Solute Transport on a Permafrost‐Affected Slope in West Greenland S. Zastruzny et al. 10.1029/2023WR036147
- Solute transport characteristics of columnar volumetric contraction networks with mega column structure and aperture variability J. Honer et al. 10.1016/j.advwatres.2024.104775
27 citations as recorded by crossref.
- HydroCAL: A novel integrated surface–subsurface hydrological model based on the Cellular Automata paradigm L. Furnari et al. 10.1016/j.advwatres.2024.104623
- Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw S. Painter et al. 10.1073/pnas.2212171120
- Evaluating integrated surface/subsurface permafrost thermal hydrology models in ATS (v0.88) against observations from a polygonal tundra site A. Jan et al. 10.5194/gmd-13-2259-2020
- Permafrost thermal conditions are sensitive to shifts in snow timing A. Jan & S. Painter 10.1088/1748-9326/ab8ec4
- Numerical modeling and simulation of thermo-hydrologic processes in frozen soils on the Qinghai-Tibet Plateau J. Hu et al. 10.1016/j.ejrh.2022.101050
- Numerical analysis of thermo-water-vapor-carbon coupling in a permafrost region: a case study in the Beiluhe area of the Qinghai-Tibetan Plateau H. WEI et al. 10.1016/j.pedsph.2024.09.006
- Upscaling an Extended Heterogeneous Stefan Problem from the Pore-Scale to the Darcy Scale in Permafrost M. Peszynska et al. 10.1137/23M1552000
- Permafrost modelling with OpenFOAM®: New advancements of the permaFoam solver L. Orgogozo et al. 10.1016/j.cpc.2022.108541
- Simulating site-scale permafrost hydrology: Sensitivity to modelling decisions and air temperature S. Krogh & J. Pomeroy 10.1016/j.jhydrol.2021.126771
- Advances in Permafrost Representation: Biophysical Processes in Earth System Models and the Role of Offline Models H. Matthes et al. 10.1002/ppp.2269
- Continentality determines warming or cooling impact of heavy rainfall events on permafrost A. Hamm et al. 10.1038/s41467-023-39325-4
- The effect of seasonally frozen ground on rainfall infiltration and groundwater discharge in Qinghai Lake Basin, China C. Ding et al. 10.3389/frwa.2024.1495763
- Effects of climate change on depression‐focused groundwater recharge in the Canadian Prairies A. Negm et al. 10.1002/vzj2.20153
- New insights into the drainage of inundated ice-wedge polygons using fundamental hydrologic principles D. Harp et al. 10.5194/tc-15-4005-2021
- Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions X. Yang et al. 10.3389/feart.2021.721009
- The impacts of vegetation on the soil surface freezing-thawing processes at permafrost southern edge simulated by an improved process-based ecosystem model Z. Liu et al. 10.1016/j.ecolmodel.2021.109663
- The importance of freeze–thaw cycles for lateral tracer transport in ice-wedge polygons E. Jafarov et al. 10.5194/tc-16-851-2022
- Limited control of microtopography evolution on ground subsidence in polygonal tundra landscapes A. Khattak & A. Hamm 10.1016/j.scitotenv.2024.174741
- Evaluating simplifications of subsurface process representations for field-scale permafrost hydrology models B. Gao & E. Coon 10.5194/tc-16-4141-2022
- Surface energy balance of sub‐Arctic roads with varying snow regimes and properties in permafrost regions L. Chen et al. 10.1002/ppp.2129
- How does humidity data impact land surface modeling of hydrothermal regimes at a permafrost site in Utqiaġvik, Alaska? X. Huang et al. 10.1016/j.scitotenv.2023.168697
- Explicitly modelling microtopography in permafrost landscapes in a land surface model (JULES vn5.4_microtopography) N. Smith et al. 10.5194/gmd-15-3603-2022
- A hydrogeophysical framework to assess infiltration during a simulated ecosystem-scale flooding experiment M. Adebayo et al. 10.1016/j.jhydrol.2023.130243
- Guidelines for cold‐regions groundwater numerical modeling P. Lamontagne‐Hallé et al. 10.1002/wat2.1467
- Guidelines for Publicly Archiving Terrestrial Model Data to Enhance Usability, Intercomparison, and Synthesis M. Simmonds et al. 10.5334/dsj-2022-003
- Permafrost Promotes Shallow Groundwater Flow and Warmer Headwater Streams Y. Sjöberg et al. 10.1029/2020WR027463
- The thermal response of permafrost to coastal floodplain flooding Y. Zhang et al. 10.1088/1748-9326/acba32
2 citations as recorded by crossref.
- Impact of Summer Air Temperature on Water and Solute Transport on a Permafrost‐Affected Slope in West Greenland S. Zastruzny et al. 10.1029/2023WR036147
- Solute transport characteristics of columnar volumetric contraction networks with mega column structure and aperture variability J. Honer et al. 10.1016/j.advwatres.2024.104775
Latest update: 29 May 2025
Short summary
Computer simulations are important tools for understanding the response of Arctic permafrost to a warming climate. To build confidence in an emerging class of permafrost simulators, we evaluated the Advanced Terrestrial Simulator against field observations from a frozen tundra site near Utqiaġvik (formerly Barrow), Alaska. The 3-year simulations agree well with observations of snow depth, summer water table, soil temperature at multiple locations, and spatially averaged evaporation.
Computer simulations are important tools for understanding the response of Arctic permafrost to...
