Articles | Volume 19, issue 1
https://doi.org/10.5194/tc-19-401-2025
© Author(s) 2025. 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-19-401-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High-resolution 4D electrical resistivity tomography and below-ground point sensor monitoring of High Arctic deglaciated sediments capture zero-curtain effects, freeze–thaw transitions, and mid-winter thawing
Environmental and Engineering Geophysics, British Geological Survey, Keyworth, United Kingdom
Oliver Kuras
Environmental and Engineering Geophysics, British Geological Survey, Keyworth, United Kingdom
Harry Harrison
Environmental and Engineering Geophysics, British Geological Survey, Keyworth, United Kingdom
Paul B. Wilkinson
Environmental and Engineering Geophysics, British Geological Survey, Keyworth, United Kingdom
Philip Meldrum
Environmental and Engineering Geophysics, British Geological Survey, Keyworth, United Kingdom
Jonathan E. Chambers
Environmental and Engineering Geophysics, British Geological Survey, Keyworth, United Kingdom
Dane Liljestrand
Department of Civil & Environmental Engineering, University of Utah, Salt Lake City, Utah, United States of America
Carlos Oroza
Department of Civil & Environmental Engineering, University of Utah, Salt Lake City, Utah, United States of America
Steven K. Schmidt
Ecology and Evolutionary Biology, University of Colorado Boulder, Boulder, Colorado, United States of America
Pacifica Sommers
Ecology and Evolutionary Biology, University of Colorado Boulder, Boulder, Colorado, United States of America
Lara Vimercati
Ecology and Evolutionary Biology, University of Colorado Boulder, Boulder, Colorado, United States of America
Trevor P. Irons
Department of Geological Engineering, Montana Technological University, Butte, Montana, United States of America
Zhou Lyu
School of Biological and Behavioural Sciences, Queen Mary University of London, London, United Kingdom
Adam Solon
School of Biological and Behavioural Sciences, Queen Mary University of London, London, United Kingdom
James A. Bradley
School of Biological and Behavioural Sciences, Queen Mary University of London, London, United Kingdom
Aix-Marseille University, Université de Toulon, CNRS, IRD, MIO, Marseille, France
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Cited
10 citations as recorded by crossref.
- Observing rock moisture changes using electrical resistivity tomography in frost weathering caves P. Oberender et al. https://doi.org/10.1016/j.geomorph.2025.110048
- Biological soil crust microcolonies reveal how microbial communities assemble following retreat of a High Arctic glacier S. Schmidt et al. https://doi.org/10.1093/femsmc/xtaf007
- Review of geophysical data acquisition methods for underground feature detection and future trends C. Peng et al. https://doi.org/10.1016/j.tust.2025.106731
- An Interpretable framework of Soil moisture estimation based on Mixture-of-Experts (ISMoE): a case study on the Tibetan Plateau J. Yang et al. https://doi.org/10.1016/j.jhydrol.2025.133763
- Rockwall permafrost dynamics evidenced by repeated and Automated Electrical Resistivity Tomography at Aiguille du Midi (3842 m a.s.l., French Alps) F. Abdulsamad et al. https://doi.org/10.5194/tc-20-2181-2026
- Hybrid clustering and hierarchical reconstruction of near-surface air temperature boundary conditions for permafrost highways on the Qinghai-Xizang Plateau Z. Zuo et al. https://doi.org/10.1016/j.coldregions.2026.105000
- Automated Electrical Resistivity Tomography for Continuous Monitoring of Permafrost Dynamics: First Field Application and Validation in Central Asia M. Farzamian et al. https://doi.org/10.3390/s26175621
- Advances in monitoring technologies for CO2 geological sequestration sites J. Ma et al. https://doi.org/10.1016/j.geoen.2026.214571
- Field-validated imaging of decadal and seasonal changes in permafrost bedrock using quantitative electrical resistivity tomography (Zugspitze, Germany/Austria) R. Scandroglio et al. https://doi.org/10.5194/tc-20-4787-2026
- Electrical Resistivity Tomography for the 2D and 3D Investigation of Pingos and Permafrost Mounds in Northern Canada's Mountain and Coastland Areas T. Wiegand et al. https://doi.org/10.1002/ppp.70061
10 citations as recorded by crossref.
- Observing rock moisture changes using electrical resistivity tomography in frost weathering caves P. Oberender et al. https://doi.org/10.1016/j.geomorph.2025.110048
- Biological soil crust microcolonies reveal how microbial communities assemble following retreat of a High Arctic glacier S. Schmidt et al. https://doi.org/10.1093/femsmc/xtaf007
- Review of geophysical data acquisition methods for underground feature detection and future trends C. Peng et al. https://doi.org/10.1016/j.tust.2025.106731
- An Interpretable framework of Soil moisture estimation based on Mixture-of-Experts (ISMoE): a case study on the Tibetan Plateau J. Yang et al. https://doi.org/10.1016/j.jhydrol.2025.133763
- Rockwall permafrost dynamics evidenced by repeated and Automated Electrical Resistivity Tomography at Aiguille du Midi (3842 m a.s.l., French Alps) F. Abdulsamad et al. https://doi.org/10.5194/tc-20-2181-2026
- Hybrid clustering and hierarchical reconstruction of near-surface air temperature boundary conditions for permafrost highways on the Qinghai-Xizang Plateau Z. Zuo et al. https://doi.org/10.1016/j.coldregions.2026.105000
- Automated Electrical Resistivity Tomography for Continuous Monitoring of Permafrost Dynamics: First Field Application and Validation in Central Asia M. Farzamian et al. https://doi.org/10.3390/s26175621
- Advances in monitoring technologies for CO2 geological sequestration sites J. Ma et al. https://doi.org/10.1016/j.geoen.2026.214571
- Field-validated imaging of decadal and seasonal changes in permafrost bedrock using quantitative electrical resistivity tomography (Zugspitze, Germany/Austria) R. Scandroglio et al. https://doi.org/10.5194/tc-20-4787-2026
- Electrical Resistivity Tomography for the 2D and 3D Investigation of Pingos and Permafrost Mounds in Northern Canada's Mountain and Coastland Areas T. Wiegand et al. https://doi.org/10.1002/ppp.70061
Saved (final revised paper)
Latest update: 22 Sep 2026
Short summary
Young Arctic sediments, uncovered by retreating glaciers, are in continuous development, shaped by how water infiltrates and is stored in the near subsurface. Harsh weather conditions at high latitudes make direct observation of these environments very difficult. To address this, we deployed two automated sensor installations in August 2021 on a glacier forefield in Svalbard. These sensors recorded continuously for 1 year, revealing unprecedented images of the ground’s freeze–thaw transition.
Young Arctic sediments, uncovered by retreating glaciers, are in continuous development, shaped...