Articles | Volume 10, issue 2
https://doi.org/10.5194/tc-10-799-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-10-799-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Growth of a young pingo in the Canadian Arctic observed by RADARSAT-2 interferometric satellite radar
Sergey V. Samsonov
CORRESPONDING AUTHOR
Canada Centre for Mapping and Earth Observation, Natural Resources Canada, 560 Rochester Street, Ottawa, ON, Canada
Trevor C. Lantz
School of Environmental Studies, University of Victoria, Victoria, BC, Canada
Steven V. Kokelj
Northwest Territories Geological Survey, Government of the Northwest Territories, Yellowknife, NWT, Canada
Canada Centre for Mapping and Earth Observation, Natural Resources Canada, 560 Rochester Street, Ottawa, ON, Canada
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Cited
17 citations as recorded by crossref.
- Distribution and morphometry of pingos, western Canadian Arctic, Northwest Territories, Canada S. Wolfe et al. 10.1016/j.geomorph.2023.108694
- Multidimensional Small Baseline Subset (MSBAS) for Two-Dimensional Deformation Analysis: Case Study Mexico City S. Samsonov & N. d'Oreye 10.1080/07038992.2017.1344926
- Characterizing marsh wetlands in the Great Lakes Basin with C-band InSAR observations Z. Chen et al. 10.1016/j.rse.2020.111750
- Trends in Satellite Earth Observation for Permafrost Related Analyses—A Review M. Philipp et al. 10.3390/rs13061217
- Possible (closed system) pingo and ice-wedge/thermokarst complexes at the mid latitudes of Utopia Planitia, Mars R. Soare et al. 10.1016/j.icarus.2019.03.010
- Post‐Wildfire Surface Deformation Near Batagay, Eastern Siberia, Detected by L‐Band and C‐Band InSAR K. Yanagiya & M. Furuya 10.1029/2019JF005473
- Towards precise drone-based measurement of elevation change in permafrost terrain experiencing thaw and thermokarst R. Fraser et al. 10.1139/dsa-2022-0036
- Permafrost Terrain Dynamics and Infrastructure Impacts Revealed by UAV Photogrammetry and Thermal Imaging J. Van der Sluijs et al. 10.3390/rs10111734
- Three-dimensional deformation time series of glacier motion from multiple-aperture DInSAR observation S. Samsonov 10.1007/s00190-019-01325-y
- Satellite interferometry for regional assessment of landslide hazard to pipelines in northeastern British Columbia, Canada S. Samsonov & A. Blais-Stevens 10.1016/j.jag.2023.103273
- Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia S. Zolkos et al. 10.3390/geosciences11010021
- Experimental soft‐sediment deformation caused by fluidization and intrusive ice melt in sand P. Bertran et al. 10.1111/sed.12537
- Monitoring Ground Surface Deformation of Ice-Wedge Polygon Areas in Saskylakh, NW Yakutia, Using Interferometric Synthetic Aperture Radar (InSAR) and Google Earth Engine (GEE) W. Wang et al. 10.3390/rs15051335
- Thermal photogrammetry on a permafrost rock wall for the active layer monitoring S. Ponti et al. 10.1016/j.scitotenv.2024.170391
- InSAR Monitoring of Arctic Landfast Sea Ice Deformation Using L-Band ALOS-2, C-Band Radarsat-2 and Sentinel-1 Z. Chen et al. 10.3390/rs13224570
- Multidimensional Small Baseline Subset (MSBAS) for volcano monitoring in two dimensions: Opportunities and challenges. Case study Piton de la Fournaise volcano S. Samsonov et al. 10.1016/j.jvolgeores.2017.04.017
- Source parameters of the 2017Mw 6.2 Yukon earthquake doublet inferred from coseismic GPS and ALOS-2 deformation measurements W. Feng et al. 10.1093/gji/ggy497
16 citations as recorded by crossref.
- Distribution and morphometry of pingos, western Canadian Arctic, Northwest Territories, Canada S. Wolfe et al. 10.1016/j.geomorph.2023.108694
- Multidimensional Small Baseline Subset (MSBAS) for Two-Dimensional Deformation Analysis: Case Study Mexico City S. Samsonov & N. d'Oreye 10.1080/07038992.2017.1344926
- Characterizing marsh wetlands in the Great Lakes Basin with C-band InSAR observations Z. Chen et al. 10.1016/j.rse.2020.111750
- Trends in Satellite Earth Observation for Permafrost Related Analyses—A Review M. Philipp et al. 10.3390/rs13061217
- Possible (closed system) pingo and ice-wedge/thermokarst complexes at the mid latitudes of Utopia Planitia, Mars R. Soare et al. 10.1016/j.icarus.2019.03.010
- Post‐Wildfire Surface Deformation Near Batagay, Eastern Siberia, Detected by L‐Band and C‐Band InSAR K. Yanagiya & M. Furuya 10.1029/2019JF005473
- Towards precise drone-based measurement of elevation change in permafrost terrain experiencing thaw and thermokarst R. Fraser et al. 10.1139/dsa-2022-0036
- Permafrost Terrain Dynamics and Infrastructure Impacts Revealed by UAV Photogrammetry and Thermal Imaging J. Van der Sluijs et al. 10.3390/rs10111734
- Three-dimensional deformation time series of glacier motion from multiple-aperture DInSAR observation S. Samsonov 10.1007/s00190-019-01325-y
- Satellite interferometry for regional assessment of landslide hazard to pipelines in northeastern British Columbia, Canada S. Samsonov & A. Blais-Stevens 10.1016/j.jag.2023.103273
- Detecting and Mapping Gas Emission Craters on the Yamal and Gydan Peninsulas, Western Siberia S. Zolkos et al. 10.3390/geosciences11010021
- Experimental soft‐sediment deformation caused by fluidization and intrusive ice melt in sand P. Bertran et al. 10.1111/sed.12537
- Monitoring Ground Surface Deformation of Ice-Wedge Polygon Areas in Saskylakh, NW Yakutia, Using Interferometric Synthetic Aperture Radar (InSAR) and Google Earth Engine (GEE) W. Wang et al. 10.3390/rs15051335
- Thermal photogrammetry on a permafrost rock wall for the active layer monitoring S. Ponti et al. 10.1016/j.scitotenv.2024.170391
- InSAR Monitoring of Arctic Landfast Sea Ice Deformation Using L-Band ALOS-2, C-Band Radarsat-2 and Sentinel-1 Z. Chen et al. 10.3390/rs13224570
- Multidimensional Small Baseline Subset (MSBAS) for volcano monitoring in two dimensions: Opportunities and challenges. Case study Piton de la Fournaise volcano S. Samsonov et al. 10.1016/j.jvolgeores.2017.04.017
Saved (preprint)
Latest update: 23 Nov 2024
Short summary
We describe the growth of a very large diameter pingo in the Tuktoyaktuk Coastlands. Analysis of historical data showed that ground uplift initiated sometime between 1935 and 1951 following lake drainage and is largely caused by the growth of intrusive ice. This study demonstrates that satellite radar can successfully contribute to understanding the dynamics of terrain uplift in response to permafrost aggradation and ground ice development in remote polar environments.
We describe the growth of a very large diameter pingo in the Tuktoyaktuk Coastlands. Analysis of...