Articles | Volume 13, issue 4
The Cryosphere, 13, 1089–1123, 2019
https://doi.org/10.5194/tc-13-1089-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 1089–1123, 2019
https://doi.org/10.5194/tc-13-1089-2019
© 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
04 Apr 2019
Research article
| Highlight paper
| 04 Apr 2019
Pathways of ice-wedge degradation in polygonal tundra under different hydrological conditions
Jan Nitzbon et al.
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Cited
24 citations as recorded by crossref.
- Timescales of the permafrost carbon cycle and legacy effects of temperature overshoot scenarios P. de Vrese & V. Brovkin 10.1038/s41467-021-23010-5
- Lateral thermokarst patterns in permafrost peat plateaus in northern Norway L. Martin et al. 10.5194/tc-15-3423-2021
- Soil moisture and hydrology projections of the permafrost region – a model intercomparison C. Andresen et al. 10.5194/tc-14-445-2020
- Simulating Snow Redistribution and its Effect on Ground Surface Temperature at a High‐Arctic Site on Svalbard R. Zweigel et al. 10.1029/2020JF005673
- A Model of Ice Wedge Polygon Drainage in Changing Arctic Terrain V. Zlotnik et al. 10.3390/w12123376
- A Quantitative Graph-Based Approach to Monitoring Ice-Wedge Trough Dynamics in Polygonal Permafrost Landscapes T. Rettelbach et al. 10.3390/rs13163098
- 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
- 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
- Feedbacks Between Surface Deformation and Permafrost Degradation in Ice Wedge Polygons, Arctic Coastal Plain, Alaska C. Abolt et al. 10.1029/2019JF005349
- Serpentine (Floating) Ice Channels and their Interaction with Riverbed Permafrost in the Lena River Delta, Russia B. Juhls et al. 10.3389/feart.2021.689941
- Functional Lake‐to‐Channel Connectivity Impacts Lake Ice in the Colville Delta, Alaska W. Dolan et al. 10.1029/2021JF006362
- Sensitivity of ecosystem-protected permafrost under changing boreal forest structures S. Stuenzi et al. 10.1088/1748-9326/ac153d
- New insights into the drainage of inundated ice-wedge polygons using fundamental hydrologic principles D. Harp et al. 10.5194/tc-15-4005-2021
- Assessment of the Ice Wedge Polygon Current State by Means of UAV Imagery Analysis (Samoylov Island, the Lena Delta) A. Kartoziia 10.3390/rs11131627
- Debris cover on thaw slumps and its insulative role in a warming climate S. Zwieback et al. 10.1002/esp.4919
- 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
- Fast response of cold ice-rich permafrost in northeast Siberia to a warming climate J. Nitzbon et al. 10.1038/s41467-020-15725-8
- Variability of the surface energy balance in permafrost-underlain boreal forest S. Stuenzi et al. 10.5194/bg-18-343-2021
- 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
- Guidelines for cold‐regions groundwater numerical modeling P. Lamontagne‐Hallé et al. 10.1002/wat2.1467
- High potential for loss of permafrost landforms in a changing climate O. Karjalainen et al. 10.1088/1748-9326/abafd5
- Thaw processes in ice-rich permafrost landscapes represented with laterally coupled tiles in a land surface model K. Aas et al. 10.5194/tc-13-591-2019
- Stability Conditions of Peat Plateaus and Palsas in Northern Norway L. Martin et al. 10.1029/2018JF004945
- 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
21 citations as recorded by crossref.
- Timescales of the permafrost carbon cycle and legacy effects of temperature overshoot scenarios P. de Vrese & V. Brovkin 10.1038/s41467-021-23010-5
- Lateral thermokarst patterns in permafrost peat plateaus in northern Norway L. Martin et al. 10.5194/tc-15-3423-2021
- Soil moisture and hydrology projections of the permafrost region – a model intercomparison C. Andresen et al. 10.5194/tc-14-445-2020
- Simulating Snow Redistribution and its Effect on Ground Surface Temperature at a High‐Arctic Site on Svalbard R. Zweigel et al. 10.1029/2020JF005673
- A Model of Ice Wedge Polygon Drainage in Changing Arctic Terrain V. Zlotnik et al. 10.3390/w12123376
- A Quantitative Graph-Based Approach to Monitoring Ice-Wedge Trough Dynamics in Polygonal Permafrost Landscapes T. Rettelbach et al. 10.3390/rs13163098
- 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
- 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
- Feedbacks Between Surface Deformation and Permafrost Degradation in Ice Wedge Polygons, Arctic Coastal Plain, Alaska C. Abolt et al. 10.1029/2019JF005349
- Serpentine (Floating) Ice Channels and their Interaction with Riverbed Permafrost in the Lena River Delta, Russia B. Juhls et al. 10.3389/feart.2021.689941
- Functional Lake‐to‐Channel Connectivity Impacts Lake Ice in the Colville Delta, Alaska W. Dolan et al. 10.1029/2021JF006362
- Sensitivity of ecosystem-protected permafrost under changing boreal forest structures S. Stuenzi et al. 10.1088/1748-9326/ac153d
- New insights into the drainage of inundated ice-wedge polygons using fundamental hydrologic principles D. Harp et al. 10.5194/tc-15-4005-2021
- Assessment of the Ice Wedge Polygon Current State by Means of UAV Imagery Analysis (Samoylov Island, the Lena Delta) A. Kartoziia 10.3390/rs11131627
- Debris cover on thaw slumps and its insulative role in a warming climate S. Zwieback et al. 10.1002/esp.4919
- 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
- Fast response of cold ice-rich permafrost in northeast Siberia to a warming climate J. Nitzbon et al. 10.1038/s41467-020-15725-8
- Variability of the surface energy balance in permafrost-underlain boreal forest S. Stuenzi et al. 10.5194/bg-18-343-2021
- 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
- Guidelines for cold‐regions groundwater numerical modeling P. Lamontagne‐Hallé et al. 10.1002/wat2.1467
- High potential for loss of permafrost landforms in a changing climate O. Karjalainen et al. 10.1088/1748-9326/abafd5
3 citations as recorded by crossref.
- Thaw processes in ice-rich permafrost landscapes represented with laterally coupled tiles in a land surface model K. Aas et al. 10.5194/tc-13-591-2019
- Stability Conditions of Peat Plateaus and Palsas in Northern Norway L. Martin et al. 10.1029/2018JF004945
- 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
Latest update: 15 May 2022
Short summary
We studied the stability of ice wedges (massive bodies of ground ice in permafrost) under recent climatic conditions in the Lena River delta of northern Siberia. For this we used a novel modelling approach that takes into account lateral transport of heat, water, and snow and the subsidence of the ground surface due to melting of ground ice. We found that wetter conditions have a destabilizing effect on the ice wedges and associated our simulation results with observations from the study area.
We studied the stability of ice wedges (massive bodies of ground ice in permafrost) under recent...
