Articles | Volume 13, issue 2
https://doi.org/10.5194/tc-13-591-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-591-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
18 Feb 2019
Research article | Highlight paper |
| 18 Feb 2019
| 18 Feb 2019
Thaw processes in ice-rich permafrost landscapes represented with laterally coupled tiles in a land surface model
Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0316 Oslo, Norway
Léo Martin
Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0316 Oslo, Norway
Jan Nitzbon
Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0316 Oslo, Norway
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A45, 14473 Potsdam, Germany
Geography Department, Humboldt University of Berlin, Unter den Linden 6, 10099 Berlin, Germany
Moritz Langer
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A45, 14473 Potsdam, Germany
Geography Department, Humboldt University of Berlin, Unter den Linden 6, 10099 Berlin, Germany
Julia Boike
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Telegrafenberg A45, 14473 Potsdam, Germany
Geography Department, Humboldt University of Berlin, Unter den Linden 6, 10099 Berlin, Germany
Hanna Lee
Bjerknes Centre for Climate Research, NORCE Norwegian Research Centre, Jahnebakken 5, 5007 Bergen, Norway
Terje K. Berntsen
Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0316 Oslo, Norway
Sebastian Westermann
Department of Geosciences, University of Oslo, Sem Sælands vei 1, 0316 Oslo, Norway
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Cited
42 citations as recorded by crossref.
- Numerical Assessments of Excess Ice Impacts on Permafrost and Greenhouse Gases in a Siberian Tundra Site Under a Warming Climate H. Park et al. 10.3389/feart.2021.704447
- The changing thermal state of permafrost S. Smith et al. 10.1038/s43017-021-00240-1
- Pathways of ice-wedge degradation in polygonal tundra under different hydrological conditions J. Nitzbon et al. 10.5194/tc-13-1089-2019
- Mechanistic Modeling of Microtopographic Impacts on CO2 and CH4 Fluxes in an Alaskan Tundra Ecosystem Using the CLM‐Microbe Model Y. Wang et al. 10.1029/2019MS001771
- Channel Network Control on Seasonal Lake Area Dynamics in Arctic Deltas L. Vulis et al. 10.1029/2019GL086710
- Massive Ice Control on Permafrost Coast Erosion and Sensitivity M. Lim et al. 10.1029/2020GL087917
- Ground subsidence effects on simulating dynamic high-latitude surface inundation under permafrost thaw using CLM5 A. Ekici et al. 10.5194/gmd-12-5291-2019
- Challenges in Hydrologic‐Land Surface Modeling of Permafrost Signatures—A Canadian Perspective M. Abdelhamed et al. 10.1029/2022MS003013
- Automatic Identification of Thaw Slumps Based on Neural Network Methods and Thaw Slumping Susceptibility H. Zhang et al. 10.1007/s13753-023-00504-y
- Permafrost Causes Unique Fine‐Scale Spatial Variability Across Tundra Soils M. Siewert et al. 10.1029/2020GB006659
- 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
- Modellering av biogeokjemiske prosesser i den norske klimamodellen NorESM T. Berntsen 10.18261/issn.1504-3118-2021-05-06
- A strong mitigation scenario maintains climate neutrality of northern peatlands C. Qiu et al. 10.1016/j.oneear.2021.12.008
- Soil moisture and hydrology projections of the permafrost region – a model intercomparison C. Andresen et al. 10.5194/tc-14-445-2020
- Long‐Term, High‐Resolution Permafrost Monitoring Reveals Coupled Energy Balance and Hydrogeologic Controls on Talik Dynamics Near Umiujaq (Nunavik, Québec, Canada) P. Fortier et al. 10.1029/2022WR032456
- 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
- Freeze-thaw induced landslides on grasslands in cold regions J. Yang et al. 10.1016/j.catena.2022.106650
- A 16-year record (2002–2017) of permafrost, active-layer, and meteorological conditions at the Samoylov Island Arctic permafrost research site, Lena River delta, northern Siberia: an opportunity to validate remote-sensing data and land surface, snow, and permafrost models J. Boike et al. 10.5194/essd-11-261-2019
- Effects of multi-scale heterogeneity on the simulated evolution of ice-rich permafrost lowlands under a warming climate J. Nitzbon et al. 10.5194/tc-15-1399-2021
- Arctic geohazard mapping tools for civil infrastructure planning: A systematic review Z. Wang et al. 10.1016/j.coldregions.2023.103969
- Transient Modelling of Permafrost Distribution in Iceland J. Czekirda et al. 10.3389/feart.2019.00130
- Feedbacks Between Surface Deformation and Permafrost Degradation in Ice Wedge Polygons, Arctic Coastal Plain, Alaska C. Abolt et al. 10.1029/2019JF005349
- Climate and environmental changes of the Lateglacial transition and Holocene in northeastern Siberia: Evidence from diatom oxygen isotopes and assemblage composition at Lake Emanda S. Kostrova et al. 10.1016/j.quascirev.2021.106905
- First Quantification of the Permafrost Heat Sink in the Earth's Climate System J. Nitzbon et al. 10.1029/2022GL102053
- Lateral thermokarst patterns in permafrost peat plateaus in northern Norway L. Martin et al. 10.5194/tc-15-3423-2021
- Potash regime for restoration of disturbed lands in the Far North A. Iglovikov et al. 10.1051/e3sconf/202021503006
- Stability Conditions of Peat Plateaus and Palsas in Northern Norway L. Martin et al. 10.1029/2018JF004945
- Assessment of the Ice Wedge Polygon Current State by Means of UAV Imagery Analysis (Samoylov Island, the Lena Delta) A. Kartoziia 10.3390/rs11131627
- The ERA5-Land soil temperature bias in permafrost regions B. Cao et al. 10.5194/tc-14-2581-2020
- Fast response of cold ice-rich permafrost in northeast Siberia to a warming climate J. Nitzbon et al. 10.1038/s41467-020-15725-8
- Permafrost carbon emissions in a changing Arctic K. Miner et al. 10.1038/s43017-021-00230-3
- Reply to: Permafrost thaw and northern development B. Teufel & L. Sushama 10.1038/s41558-020-0861-6
- Consequences of permafrost degradation for Arctic infrastructure – bridging the model gap between regional and engineering scales T. Schneider von Deimling et al. 10.5194/tc-15-2451-2021
- Surface displacement revealed by L-band InSAR analysis in the Mayya area, Central Yakutia, underlain by continuous permafrost T. Abe et al. 10.1186/s40623-020-01266-3
- The Arctic Carbon Cycle and Its Response to Changing Climate L. Bruhwiler et al. 10.1007/s40641-020-00169-5
- Representation of soil hydrology in permafrost regions may explain large part of inter-model spread in simulated Arctic and subarctic climate P. de Vrese et al. 10.5194/tc-17-2095-2023
- Simulating ice segregation and thaw consolidation in permafrost environments with the CryoGrid community model J. Aga et al. 10.5194/tc-17-4179-2023
- A Model of Ice Wedge Polygon Drainage in Changing Arctic Terrain V. Zlotnik et al. 10.3390/w12123376
- Projecting circum-Arctic excess-ground-ice melt with a sub-grid representation in the Community Land Model L. Cai et al. 10.5194/tc-14-4611-2020
- Disproportionate microbial responses to decadal drainage on a Siberian floodplain M. Kwon et al. 10.1111/gcb.15785
- Hydrologic‐land surface modelling of the Canadian sporadic‐discontinuous permafrost: Initialization and uncertainty propagation M. Abdelhamed et al. 10.1002/hyp.14509
- Climate change reduces winter overland travel across the Pan-Arctic even under low-end global warming scenarios A. Gädeke et al. 10.1088/1748-9326/abdcf2
42 citations as recorded by crossref.
- Numerical Assessments of Excess Ice Impacts on Permafrost and Greenhouse Gases in a Siberian Tundra Site Under a Warming Climate H. Park et al. 10.3389/feart.2021.704447
- The changing thermal state of permafrost S. Smith et al. 10.1038/s43017-021-00240-1
- Pathways of ice-wedge degradation in polygonal tundra under different hydrological conditions J. Nitzbon et al. 10.5194/tc-13-1089-2019
- Mechanistic Modeling of Microtopographic Impacts on CO2 and CH4 Fluxes in an Alaskan Tundra Ecosystem Using the CLM‐Microbe Model Y. Wang et al. 10.1029/2019MS001771
- Channel Network Control on Seasonal Lake Area Dynamics in Arctic Deltas L. Vulis et al. 10.1029/2019GL086710
- Massive Ice Control on Permafrost Coast Erosion and Sensitivity M. Lim et al. 10.1029/2020GL087917
- Ground subsidence effects on simulating dynamic high-latitude surface inundation under permafrost thaw using CLM5 A. Ekici et al. 10.5194/gmd-12-5291-2019
- Challenges in Hydrologic‐Land Surface Modeling of Permafrost Signatures—A Canadian Perspective M. Abdelhamed et al. 10.1029/2022MS003013
- Automatic Identification of Thaw Slumps Based on Neural Network Methods and Thaw Slumping Susceptibility H. Zhang et al. 10.1007/s13753-023-00504-y
- Permafrost Causes Unique Fine‐Scale Spatial Variability Across Tundra Soils M. Siewert et al. 10.1029/2020GB006659
- 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
- Modellering av biogeokjemiske prosesser i den norske klimamodellen NorESM T. Berntsen 10.18261/issn.1504-3118-2021-05-06
- A strong mitigation scenario maintains climate neutrality of northern peatlands C. Qiu et al. 10.1016/j.oneear.2021.12.008
- Soil moisture and hydrology projections of the permafrost region – a model intercomparison C. Andresen et al. 10.5194/tc-14-445-2020
- Long‐Term, High‐Resolution Permafrost Monitoring Reveals Coupled Energy Balance and Hydrogeologic Controls on Talik Dynamics Near Umiujaq (Nunavik, Québec, Canada) P. Fortier et al. 10.1029/2022WR032456
- 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
- Freeze-thaw induced landslides on grasslands in cold regions J. Yang et al. 10.1016/j.catena.2022.106650
- A 16-year record (2002–2017) of permafrost, active-layer, and meteorological conditions at the Samoylov Island Arctic permafrost research site, Lena River delta, northern Siberia: an opportunity to validate remote-sensing data and land surface, snow, and permafrost models J. Boike et al. 10.5194/essd-11-261-2019
- Effects of multi-scale heterogeneity on the simulated evolution of ice-rich permafrost lowlands under a warming climate J. Nitzbon et al. 10.5194/tc-15-1399-2021
- Arctic geohazard mapping tools for civil infrastructure planning: A systematic review Z. Wang et al. 10.1016/j.coldregions.2023.103969
- Transient Modelling of Permafrost Distribution in Iceland J. Czekirda et al. 10.3389/feart.2019.00130
- Feedbacks Between Surface Deformation and Permafrost Degradation in Ice Wedge Polygons, Arctic Coastal Plain, Alaska C. Abolt et al. 10.1029/2019JF005349
- Climate and environmental changes of the Lateglacial transition and Holocene in northeastern Siberia: Evidence from diatom oxygen isotopes and assemblage composition at Lake Emanda S. Kostrova et al. 10.1016/j.quascirev.2021.106905
- First Quantification of the Permafrost Heat Sink in the Earth's Climate System J. Nitzbon et al. 10.1029/2022GL102053
- Lateral thermokarst patterns in permafrost peat plateaus in northern Norway L. Martin et al. 10.5194/tc-15-3423-2021
- Potash regime for restoration of disturbed lands in the Far North A. Iglovikov et al. 10.1051/e3sconf/202021503006
- Stability Conditions of Peat Plateaus and Palsas in Northern Norway L. Martin et al. 10.1029/2018JF004945
- Assessment of the Ice Wedge Polygon Current State by Means of UAV Imagery Analysis (Samoylov Island, the Lena Delta) A. Kartoziia 10.3390/rs11131627
- The ERA5-Land soil temperature bias in permafrost regions B. Cao et al. 10.5194/tc-14-2581-2020
- Fast response of cold ice-rich permafrost in northeast Siberia to a warming climate J. Nitzbon et al. 10.1038/s41467-020-15725-8
- Permafrost carbon emissions in a changing Arctic K. Miner et al. 10.1038/s43017-021-00230-3
- Reply to: Permafrost thaw and northern development B. Teufel & L. Sushama 10.1038/s41558-020-0861-6
- Consequences of permafrost degradation for Arctic infrastructure – bridging the model gap between regional and engineering scales T. Schneider von Deimling et al. 10.5194/tc-15-2451-2021
- Surface displacement revealed by L-band InSAR analysis in the Mayya area, Central Yakutia, underlain by continuous permafrost T. Abe et al. 10.1186/s40623-020-01266-3
- The Arctic Carbon Cycle and Its Response to Changing Climate L. Bruhwiler et al. 10.1007/s40641-020-00169-5
- Representation of soil hydrology in permafrost regions may explain large part of inter-model spread in simulated Arctic and subarctic climate P. de Vrese et al. 10.5194/tc-17-2095-2023
- Simulating ice segregation and thaw consolidation in permafrost environments with the CryoGrid community model J. Aga et al. 10.5194/tc-17-4179-2023
- A Model of Ice Wedge Polygon Drainage in Changing Arctic Terrain V. Zlotnik et al. 10.3390/w12123376
- Projecting circum-Arctic excess-ground-ice melt with a sub-grid representation in the Community Land Model L. Cai et al. 10.5194/tc-14-4611-2020
- Disproportionate microbial responses to decadal drainage on a Siberian floodplain M. Kwon et al. 10.1111/gcb.15785
- Hydrologic‐land surface modelling of the Canadian sporadic‐discontinuous permafrost: Initialization and uncertainty propagation M. Abdelhamed et al. 10.1002/hyp.14509
- Climate change reduces winter overland travel across the Pan-Arctic even under low-end global warming scenarios A. Gädeke et al. 10.1088/1748-9326/abdcf2
Discussed (final revised paper)
Latest update: 19 Apr 2024
Short summary
Many permafrost landscapes contain large amounts of excess ground ice, which gives rise to small-scale elevation differences. This results in lateral fluxes of snow, water, and heat, which we investigate and show how it can be accounted for in large-scale models. Using a novel model technique which can account for these differences, we are able to model both the current state of permafrost and how these landscapes change as permafrost thaws, in a way that could not previously be achieved.
Many permafrost landscapes contain large amounts of excess ground ice, which gives rise to...
