Articles | Volume 14, issue 3
https://doi.org/10.5194/tc-14-1105-2020
© 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/tc-14-1105-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
25 Mar 2020
Research article |
| 25 Mar 2020
| 25 Mar 2020
Detailed detection of active layer freeze–thaw dynamics using quasi-continuous electrical resistivity tomography (Deception Island, Antarctica)
Mohammad Farzamian
CORRESPONDING AUTHOR
Faculdade de Ciências, IDL, Universidade de Lisboa, Lisbon, Portugal
Instituto Nacional de Investigação Agrária e
Veterinária, Oeiras, Portugal
Gonçalo Vieira
Centre for Geographical Studies, IGOT, Universidade de Lisboa,
Lisbon, Portugal
Fernando A. Monteiro Santos
Faculdade de Ciências, IDL, Universidade de Lisboa, Lisbon, Portugal
Borhan Yaghoobi Tabar
School of Mining, Petroleum and Geophysics, Shahrood University of
Technology, Shahrood, Iran
Christian Hauck
Department of Geosciences, University of Fribourg, Fribourg, Switzerland
Maria Catarina Paz
Faculdade de Ciências, IDL, Universidade de Lisboa, Lisbon, Portugal
CIQuiBio, Barreiro School of Technology, Polytechnic Institute of
Setúbal, Lavradio, Portugal
Ivo Bernardo
Faculdade de Ciências, IDL, Universidade de Lisboa, Lisbon, Portugal
Miguel Ramos
Universidad de Alcalá de Henares, Alcalá de Henares, Spain
Miguel Angel de Pablo
Universidad de Alcalá de Henares, Alcalá de Henares, Spain
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Martin Hoelzle, Christian Hauck, Tamara Mathys, Jeannette Noetzli, Cécile Pellet, and Martin Scherler
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Bernd Etzelmüller, Justyna Czekirda, Florence Magnin, Pierre-Allain Duvillard, Ludovic Ravanel, Emanuelle Malet, Andreas Aspaas, Lene Kristensen, Ingrid Skrede, Gudrun D. Majala, Benjamin Jacobs, Johannes Leinauer, Christian Hauck, Christin Hilbich, Martina Böhme, Reginald Hermanns, Harald Ø. Eriksen, Tom Rune Lauknes, Michael Krautblatter, and Sebastian Westermann
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This paper is a multi-authored study documenting the possible existence of permafrost in permanently monitored rockslides in Norway for the first time by combining a multitude of field data, including geophysical surveys in rock walls. The paper discusses the possible role of thermal regime and rockslide movement, and it evaluates the possible impact of atmospheric warming on rockslide dynamics in Norwegian mountains.
Adrian Wicki, Per-Erik Jansson, Peter Lehmann, Christian Hauck, and Manfred Stähli
Hydrol. Earth Syst. Sci., 25, 4585–4610, https://doi.org/10.5194/hess-25-4585-2021, https://doi.org/10.5194/hess-25-4585-2021, 2021
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Gonçalo Vieira, Carla Mora, Pedro Pina, Ricardo Ramalho, and Rui Fernandes
Earth Syst. Sci. Data, 13, 3179–3201, https://doi.org/10.5194/essd-13-3179-2021, https://doi.org/10.5194/essd-13-3179-2021, 2021
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Fogo in Cabo Verde is one of the most active ocean island volcanoes on Earth, posing important hazards to local populations and at a regional level. The last eruption occurred from November 2014 to February 2015. A survey of the Chã das Caldeiras area was conducted using a fixed-wing unmanned aerial vehicle. A point cloud, digital surface model and orthomosaic with 10 and 25 cm resolutions are provided, together with the full aerial survey projects and datasets.
Djamil Al-Halbouni, Robert A. Watson, Eoghan P. Holohan, Rena Meyer, Ulrich Polom, Fernando M. Dos Santos, Xavier Comas, Hussam Alrshdan, Charlotte M. Krawczyk, and Torsten Dahm
Hydrol. Earth Syst. Sci., 25, 3351–3395, https://doi.org/10.5194/hess-25-3351-2021, https://doi.org/10.5194/hess-25-3351-2021, 2021
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The rapid decline of the Dead Sea level since the 1960s has provoked a dynamic reaction from the coastal groundwater system, with physical and chemical erosion creating subsurface voids and conduits. By combining remote sensing, geophysical methods, and numerical modelling at the Dead Sea’s eastern shore, we link groundwater flow patterns to the formation of surface stream channels, sinkholes and uvalas. Better understanding of this karst system will improve regional hazard assessment.
Mohammad Farzamian, Dario Autovino, Angelo Basile, Roberto De Mascellis, Giovanna Dragonetti, Fernando Monteiro Santos, Andrew Binley, and Antonio Coppola
Hydrol. Earth Syst. Sci., 25, 1509–1527, https://doi.org/10.5194/hess-25-1509-2021, https://doi.org/10.5194/hess-25-1509-2021, 2021
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Soil salinity is a serious threat in numerous arid and semi-arid areas of the world. Given this threat, efficient field assessment methods are needed to monitor the dynamics of soil salinity in salt-affected lands efficiently. We demonstrate that rapid and non-invasive geophysical measurements modelled by advanced numerical analysis of the signals and coupled with hydrological modelling can provide valuable information to assess the spatio-temporal variability in soil salinity over large areas.
Christian Halla, Jan Henrik Blöthe, Carla Tapia Baldis, Dario Trombotto Liaudat, Christin Hilbich, Christian Hauck, and Lothar Schrott
The Cryosphere, 15, 1187–1213, https://doi.org/10.5194/tc-15-1187-2021, https://doi.org/10.5194/tc-15-1187-2021, 2021
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In the semi-arid to arid Andes of Argentina, rock glaciers contain invisible and unknown amounts of ground ice that could become more important in future for the water availability during the dry season. The study shows that the investigated rock glacier represents an important long-term ice reservoir in the dry mountain catchment and that interannual changes of ground ice can store and release significant amounts of annual precipitation.
Maria Catarina Paz, Mohammad Farzamian, Ana Marta Paz, Nádia Luísa Castanheira, Maria Conceição Gonçalves, and Fernando Monteiro Santos
SOIL, 6, 499–511, https://doi.org/10.5194/soil-6-499-2020, https://doi.org/10.5194/soil-6-499-2020, 2020
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In this study electromagnetic induction (EMI) surveys and soil sampling were repeated over time to monitor soil salinity dynamics in an important agricultural area that faces risk of soil salinization. EMI data were converted to electromagnetic conductivity imaging through a mathematical inversion algorithm and converted to 2-D soil salinity maps until a depth of 1.35 m through a regional calibration. This is a non-invasive and cost-effective methodology that can be employed over large areas.
Maximilian Weigand, Florian M. Wagner, Jonas K. Limbrock, Christin Hilbich, Christian Hauck, and Andreas Kemna
Geosci. Instrum. Method. Data Syst., 9, 317–336, https://doi.org/10.5194/gi-9-317-2020, https://doi.org/10.5194/gi-9-317-2020, 2020
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In times of global warming, permafrost is starting to degrade at alarming rates, requiring new and improved characterization approaches. We describe the design and test installation, as well as detailed data quality assessment, of a monitoring system used to capture natural electrical potentials in the subsurface. These self-potential signals are of great interest for the noninvasive investigation of water flow in the non-frozen or partially frozen subsurface.
Jaroslav Obu, Sebastian Westermann, Gonçalo Vieira, Andrey Abramov, Megan Ruby Balks, Annett Bartsch, Filip Hrbáček, Andreas Kääb, and Miguel Ramos
The Cryosphere, 14, 497–519, https://doi.org/10.5194/tc-14-497-2020, https://doi.org/10.5194/tc-14-497-2020, 2020
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Little is known about permafrost in the Antarctic outside of the few research stations. We used a simple equilibrium permafrost model to estimate permafrost temperatures in the whole Antarctic. The lowest permafrost temperature on Earth is −36 °C in the Queen Elizabeth Range in the Transantarctic Mountains. Temperatures are commonly between −23 and −18 °C in mountainous areas rising above the Antarctic Ice Sheet, between −14 and −8 °C in coastal areas, and up to 0 °C on the Antarctic Peninsula.
Coline Mollaret, Christin Hilbich, Cécile Pellet, Adrian Flores-Orozco, Reynald Delaloye, and Christian Hauck
The Cryosphere, 13, 2557–2578, https://doi.org/10.5194/tc-13-2557-2019, https://doi.org/10.5194/tc-13-2557-2019, 2019
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We present a long-term multisite electrical resistivity tomography monitoring network (more than 1000 datasets recorded from six mountain permafrost sites). Despite harsh and remote measurement conditions, the datasets are of good quality and show consistent spatio-temporal variations yielding significant added value to point-scale borehole information. Observed long-term trends are similar for all permafrost sites, showing ongoing permafrost thaw and ground ice loss due to climatic conditions.
Jan Mudler, Andreas Hördt, Anita Przyklenk, Gianluca Fiandaca, Pradip Kumar Maurya, and Christian Hauck
The Cryosphere, 13, 2439–2456, https://doi.org/10.5194/tc-13-2439-2019, https://doi.org/10.5194/tc-13-2439-2019, 2019
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The capacitively coupled resistivity (CCR) method enables the determination of frequency-dependent electrical parameters of the subsurface. CCR is well suited for application in cryospheric areas because it provides logistical advantages regarding coupling on hard surfaces and highly resistive grounds. With our new spectral two-dimensional inversion, we can identify subsurface structures based on full spectral information. We show the first results of the inversion method on the field scale.
Martin Beniston, Daniel Farinotti, Markus Stoffel, Liss M. Andreassen, Erika Coppola, Nicolas Eckert, Adriano Fantini, Florie Giacona, Christian Hauck, Matthias Huss, Hendrik Huwald, Michael Lehning, Juan-Ignacio López-Moreno, Jan Magnusson, Christoph Marty, Enrique Morán-Tejéda, Samuel Morin, Mohamed Naaim, Antonello Provenzale, Antoine Rabatel, Delphine Six, Johann Stötter, Ulrich Strasser, Silvia Terzago, and Christian Vincent
The Cryosphere, 12, 759–794, https://doi.org/10.5194/tc-12-759-2018, https://doi.org/10.5194/tc-12-759-2018, 2018
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This paper makes a rather exhaustive overview of current knowledge of past, current, and future aspects of cryospheric issues in continental Europe and makes a number of reflections of areas of uncertainty requiring more attention in both scientific and policy terms. The review paper is completed by a bibliography containing 350 recent references that will certainly be of value to scholars engaged in the fields of glacier, snow, and permafrost research.
Benjamin Mewes, Christin Hilbich, Reynald Delaloye, and Christian Hauck
The Cryosphere, 11, 2957–2974, https://doi.org/10.5194/tc-11-2957-2017, https://doi.org/10.5194/tc-11-2957-2017, 2017
Gonçalo Vieira, Carla Mora, and Ali Faleh
The Cryosphere, 11, 1691–1705, https://doi.org/10.5194/tc-11-1691-2017, https://doi.org/10.5194/tc-11-1691-2017, 2017
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The Toubkal is the highest massif in North Africa (4167 m). Landforms and deposits above 3000 m show the effects of frost action in the present-day geomorphological dynamics, but data on ground temperatures were lacking. In this study ground surface temperature data measured across an altitudinal transect are presented and analysed for the first time. The highlight is the possible occurrence of permafrost at an elevation of 3800 m, which may be of high ecological and hydrological significance.
Cécile Pellet and Christian Hauck
Hydrol. Earth Syst. Sci., 21, 3199–3220, https://doi.org/10.5194/hess-21-3199-2017, https://doi.org/10.5194/hess-21-3199-2017, 2017
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This paper presents a detailed description of the new Swiss soil moisture monitoring network SOMOMOUNT, which comprises six stations distributed along an elevation gradient ranging from 1205 to 3410 m. The liquid soil moisture (LSM) data collected during the first 3 years are discussed with regard to their soil type and climate dependency as well as their altitudinal distribution. The elevation dependency of the LSM was found to be non-linear with distinct dynamics at high and low elevation.
Jonas Wicky and Christian Hauck
The Cryosphere, 11, 1311–1325, https://doi.org/10.5194/tc-11-1311-2017, https://doi.org/10.5194/tc-11-1311-2017, 2017
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Talus slopes are a widespread geomorphic feature, which may show permafrost conditions even at low elevation due to cold microclimates induced by a gravity-driven internal air circulation. We show for the first time a numerical simulation of this internal air circulation of a field-scale talus slope. Results indicate that convective heat transfer leads to a pronounced ground cooling in the lower part of the talus slope favoring the persistence of permafrost.
Carla Mora, Juan Javier Jiménez, Pedro Pina, João Catalão, and Gonçalo Vieira
The Cryosphere, 11, 139–155, https://doi.org/10.5194/tc-11-139-2017, https://doi.org/10.5194/tc-11-139-2017, 2017
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We evaluate the use of high-resolution microwave satellite images from TerraSAR-X for mapping snow-patch distribution in ice-free areas of the maritime Antarctic (King George Island). The imagery was acquired simultaneously to ground truthing of snow. Image classification resulted in very high accuracy when discriminating between snow, water and bare ground. The method provides a solution for characterizing the snowmelt patterns in the ice-free areas of the Antarctic Peninsula.
Antoine Marmy, Jan Rajczak, Reynald Delaloye, Christin Hilbich, Martin Hoelzle, Sven Kotlarski, Christophe Lambiel, Jeannette Noetzli, Marcia Phillips, Nadine Salzmann, Benno Staub, and Christian Hauck
The Cryosphere, 10, 2693–2719, https://doi.org/10.5194/tc-10-2693-2016, https://doi.org/10.5194/tc-10-2693-2016, 2016
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This paper presents a new semi-automated method to calibrate the 1-D soil model COUP. It is the first time (as far as we know) that this approach is developed for mountain permafrost. It is applied at six test sites in the Swiss Alps. In a second step, the calibrated model is used for RCM-based simulations with specific downscaling of RCM data to the borehole scale. We show projections of the permafrost evolution at the six sites until the end of the century and according to the A1B scenario.
A. Ekici, S. Chadburn, N. Chaudhary, L. H. Hajdu, A. Marmy, S. Peng, J. Boike, E. Burke, A. D. Friend, C. Hauck, G. Krinner, M. Langer, P. A. Miller, and C. Beer
The Cryosphere, 9, 1343–1361, https://doi.org/10.5194/tc-9-1343-2015, https://doi.org/10.5194/tc-9-1343-2015, 2015
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This paper compares the performance of different land models in estimating soil thermal regimes at distinct cold region landscape types. Comparing models with different processes reveal the importance of surface insulation (snow/moss layer) and soil internal processes (heat/water transfer). The importance of model processes also depend on site conditions such as high/low snow cover, dry/wet soil types.
P. Pogliotti, M. Guglielmin, E. Cremonese, U. Morra di Cella, G. Filippa, C. Pellet, and C. Hauck
The Cryosphere, 9, 647–661, https://doi.org/10.5194/tc-9-647-2015, https://doi.org/10.5194/tc-9-647-2015, 2015
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This study presents the thermal state and recent evolution of permafrost at Cime Bianche.
The analysis reveals that (i) spatial variability of MAGST is greater than its interannual variability and is controlled by snow duration and air temperature during the snow-free period, (ii) the ALT has a pronounced spatial variability caused by a different subsurface ice and water content, and (iii) permafrost is warming at significant rates below 8m of depth.
B. Staub, A. Marmy, C. Hauck, C. Hilbich, and R. Delaloye
Geogr. Helv., 70, 45–62, https://doi.org/10.5194/gh-70-45-2015, https://doi.org/10.5194/gh-70-45-2015, 2015
M. Oliva, G. Vieira, P. Pina, P. Pereira, M. Neves, and M. C. Freitas
Solid Earth, 5, 901–914, https://doi.org/10.5194/se-5-901-2014, https://doi.org/10.5194/se-5-901-2014, 2014
M. A. de Pablo, M. Ramos, and A. Molina
Solid Earth, 5, 721–739, https://doi.org/10.5194/se-5-721-2014, https://doi.org/10.5194/se-5-721-2014, 2014
A. Ekici, C. Beer, S. Hagemann, J. Boike, M. Langer, and C. Hauck
Geosci. Model Dev., 7, 631–647, https://doi.org/10.5194/gmd-7-631-2014, https://doi.org/10.5194/gmd-7-631-2014, 2014
M. Scherler, S. Schneider, M. Hoelzle, and C. Hauck
Earth Surf. Dynam., 2, 141–154, https://doi.org/10.5194/esurf-2-141-2014, https://doi.org/10.5194/esurf-2-141-2014, 2014
S. Schneider, S. Daengeli, C. Hauck, and M. Hoelzle
Geogr. Helv., 68, 265–280, https://doi.org/10.5194/gh-68-265-2013, https://doi.org/10.5194/gh-68-265-2013, 2013
Related subject area
Discipline: Frozen ground | Subject: Antarctic
Employing automated electrical resistivity tomography for detecting short- and long-term changes in permafrost and active-layer dynamics in the maritime Antarctic
Thermal legacy of a large paleolake in Taylor Valley, East Antarctica, as evidenced by an airborne electromagnetic survey
Pan-Antarctic map of near-surface permafrost temperatures at 1 km2 scale
Mohammad Farzamian, Teddi Herring, Gonçalo Vieira, Miguel Angel de Pablo, Borhan Yaghoobi Tabar, and Christian Hauck
The Cryosphere, 18, 4197–4213, https://doi.org/10.5194/tc-18-4197-2024, https://doi.org/10.5194/tc-18-4197-2024, 2024
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An automated electrical resistivity tomography (A-ERT) system was developed and deployed in Antarctica to monitor permafrost and active-layer dynamics. The A-ERT, coupled with an efficient processing workflow, demonstrated its capability to monitor real-time thaw depth progression, detect seasonal and surficial freezing–thawing events, and assess permafrost stability. Our study showcased the potential of A-ERT to contribute to global permafrost monitoring networks.
Krista F. Myers, Peter T. Doran, Slawek M. Tulaczyk, Neil T. Foley, Thue S. Bording, Esben Auken, Hilary A. Dugan, Jill A. Mikucki, Nikolaj Foged, Denys Grombacher, and Ross A. Virginia
The Cryosphere, 15, 3577–3593, https://doi.org/10.5194/tc-15-3577-2021, https://doi.org/10.5194/tc-15-3577-2021, 2021
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Lake Fryxell, Antarctica, has undergone hundreds of meters of change in recent geologic history. However, there is disagreement on when lake levels were higher and by how much. This study uses resistivity data to map the subsurface conditions (frozen versus unfrozen ground) to map ancient shorelines. Our models indicate that Lake Fryxell was up to 60 m higher just 1500 to 4000 years ago. This amount of lake level change shows how sensitive these systems are to small changes in temperature.
Jaroslav Obu, Sebastian Westermann, Gonçalo Vieira, Andrey Abramov, Megan Ruby Balks, Annett Bartsch, Filip Hrbáček, Andreas Kääb, and Miguel Ramos
The Cryosphere, 14, 497–519, https://doi.org/10.5194/tc-14-497-2020, https://doi.org/10.5194/tc-14-497-2020, 2020
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Little is known about permafrost in the Antarctic outside of the few research stations. We used a simple equilibrium permafrost model to estimate permafrost temperatures in the whole Antarctic. The lowest permafrost temperature on Earth is −36 °C in the Queen Elizabeth Range in the Transantarctic Mountains. Temperatures are commonly between −23 and −18 °C in mountainous areas rising above the Antarctic Ice Sheet, between −14 and −8 °C in coastal areas, and up to 0 °C on the Antarctic Peninsula.
Cited articles
Biskaborn, B. K., Smith, S. L., Noetzli, J. et al.: Permafrost is warming at a global scale, Nat.
Commun., 10, 264, 2019.
Bockheim, J., Vieira, G., Ramos, M., Lopez-Martinez, J., Serrano, E.,
Guglielmin, M., Wilhelm, K., and Nieuwendam, A.: Climate warming and
permafrost dynamics in the Antarctic Peninsula region, Global Planet. Change,
100, 215–223, https://doi.org/10.1016/j.gloplacha.2012.10.018, 2013.
Dafflon, B., Hubbard, S., Ulrich, C., Peterson, J., Wu, Y., Wainwright, H.,
and Kneafsey, T. J.: Geophysical
estimation of shallow permafrost distribution and properties in an ice-wedge
polygon-dominated Arctic tundra region, Geophysics, 81, WA247–WA263, https://doi.org/10.1190/geo2015-0175.1, 2016.
De Pablo, M. A., Ramos, M., Molina, A., Vieira, G., Hidalgo, M. A., Prieto, M., Jiménez, J. J., Fernández, S., Recondo, C., Calleja, J. F.,
Peón, J. J., and Mora, C.: Frozen ground and snow cover monitoring in
the South Shetland Islands, Antarctica: Instrumentation, effects on ground
thermal behaviour and future research, Cuad. Invest. Geográfica, 42, 475–495, https://doi.org/10.18172/cig.2917, 2016.
Duvillard, P. A., Revil, A., Soueid Ahmed, A., Qi, Y., Coperey, A., and Ravanel, L.: Three dimensional electrical conductivity and induced polarization tomography of a rock glacier, J. Geophys. Res.-Solid Earth, 123, 9528–9554, https://doi.org/10.1029/2018JB015965, 2019.
Farzamian, M., Vieira, G., Monteiro Santos, F. A., Tabar, B. Y., Hauck, C., Paz, M. C., Bernando, I., Ramos, M., de Pablo, M. A.: A-ERT and ground temperature data- 2010- Deception Island/Antarctica, Zenodo, https://doi.org/10.5281/zenodo.3635063, 2020.
Fortier, R., LeBlanc, A.-M., Allard, M., Buteau, S., and Calmels, F.: Internal
structure and conditions of permafrost mounds at Umiujaq in Nunavik, Canada,
inferred from field investigation and electrical resistivity tomography,
Can. J. Earth Sci. , 45, 367–387, https://doi.org/10.1139/E08-004, 2008.
Goyanes, G., Vieira, G., Caselli, A., Cardoso, M., Marmy, A., Santos, F.,
Bernardo, I., and Hauck, C.: Local influences of geothermal anomalies on
permafrost distribution in an active volcanic island (Deception Island,
Antarctica), Geomorphology, 225, 57–68,
https://doi.org/10.1016/j.geomorph.2014.04.010, 2014.
Grimm, R. E. and Stillman, D. E.: Field test of detection and characterization of
subsurface ice using broadband spectral-induced polarisation, Permafrost
Periglac., 26, 28–38, https://doi.org/10.1002/ppp.1833, 2015.
Guglielmin, M. and Dramis, F.: Permafrost as a climatic indicator in
northern Victoria Land, Antarctica, Ann. Glaciol., 29, 131–135,
https://doi.org/10.3189/172756499781821111, 1999.
Guglielmin, M., Biasini, A., and Smiraglia, C.: The contribution of
geoelectrical investigations in the analysis of periglacial and glacial
landforms in ice free areas of the Northern Foothills (Northern Victoria
Land, Antarctica), Geogr. Ann. A, 79, 17–24, https://doi.org/10.1111/j.0435-3676.1997.00003.x, 1997.
Hauck, C.: Frozen ground monitoring using DC resistivity tomography,
Geophys. Res. Lett., 29, 2016, https://doi.org/10.1029/2002GL014995, 2002.
Hauck, C. and Vonder Mühll, D.: Inversion and interpretation
oftwo-dimensional geoelectrical measurements for detecting per-mafrost in
mountainous regions, Permafrost Periglac., 14, 305–318.
https://doi.org/10.1002/ppp.462, 2003.
Hauck, C., Vieira, G., Gruber, S., Blanco, J. J., and Ramos, M.: Geophysical
identification of permafrost in Livingston Island, maritime
Antarctica, J.
Geophys. Res., 112, F02S19, https://doi.org/10.1029/2006JF000544, 2007.
Hauck, C., Böttcher, M., and Maurer, H.: A new model for estimating subsurface ice content based on combined electrical and seismic data sets, The Cryosphere, 5, 453–468, https://doi.org/10.5194/tc-5-453-2011, 2011.
Hilbich, C., Hauck, C., Hoelzle, M., Scherler, M., Schudel, L., Völksch, I., Vonder Mühll, D., and Mäusbacher, R.: Monitoring mountain
permafrost evolution using electrical resistivity tomography: A 7-year study
of seasonal, annual, and long-term variations at Schilthorn, Swiss Alps,
J. Geophys. Res., 113, F01S90, https://doi.org/10.1029/2007JF000799, 2008.
Hilbich, C., Fuss, C., and Hauck, C.: Automated Time-lapse ERT for Improved
Process Analysis and Monitoring of Frozen Ground, Permafrost Periglac., 22,
306–319, https://doi.org/10.1002/ppp.732, 2011.
Keating, K., Binley, A., Bense, V., Van Dam, R. L., and Christiansen, H. H.:
Combined geophysical measurements provide evidence for unfrozen water in
permafrost in the Adventdalen valley in Svalbard, Geophys. Res.
Lett., 45, 7606–761, https://doi.org/10.1029/2017GL076508, 2018.
Keuschnig, M., Krautblatter, M., Hartmeyer, I., Fuss, C., and Schrott, L.:
Automated Electrical Resistivity Tomography Testing for Early Warning in
Unstable Permafrost Rock Walls Around Alpine Infrastructure, Permafrost Periglac., 28, 158–171, https://doi.org/10.1002/ppp.1916
2017.
Kim, J. H., Yi M. J., Park, S. G., and Kim, J. G.: 4-D inversion of DC
resistivity monitoring data acquired over a dynamically changing earth
model, J. Appl. Geophys., 68, 522–532, https://doi.org/10.1016/j.jappgeo.2009.03.002, 2009.
Kneisel, C.: Assessment of subsurface lithology in mountain environments
using 2D resistivity imaging, Geomorphology, 80, 32–44, https://doi.org/10.1016/j.geomorph.2005.09.012, 2006.
Krautblatter, M., Verlcysdonk, S., Flores-Orozco, A., and Kemna A.:
Temperature-calibrated imaging of seasonal changes in permafrost rock walls
by quantitative electrical resistivity tomography (Zugspitze,
German/Austrain Alps), Geophys. Res., 115, F02003,
https://doi.org/10.1029/2008JF001209, 2010.
Loke, M. H.: Tutorial: 2D and 3D Electrical Imaging Surveys, Technical Note,
2nd edn., Geotomo Software, Malaysia, 2002.
Marmy, A., Rajczak, J., Delaloye, R., Hilbich, C., Hoelzle, M., Kotlarski, S., Lambiel, C., Noetzli, J., Phillips, M., Salzmann, N., Staub, B., and Hauck, C.: Semi-automated calibration method for modelling of mountain permafrost evolution in Switzerland, The Cryosphere, 10, 2693–2719, https://doi.org/10.5194/tc-10-2693-2016, 2016.
McGinnis, L. D., Nakao, K., and Clark, C. C.: Geophysical identification of
frozen and unfrozen ground, Antarctica, in: Proceed. 2nd Internat. Conf.
Permafrost, 13–28 July, Yakutsk, Russia, 136–146, 1973.
Melo, R., Vieira, G., Caselli, A., and Ramos, M.: Susceptibility modelling
of hummocky terrain distribution using the information value method
(Deception Island, Antarctic Peninsula), Geomorphology, 155–156, 88–95 https://doi.org/10.1016/j.geomorph.2011.12.027, 2012.
Mewes, B., Hilbich, C., Delaloye, R., and Hauck, C.: Resolution capacity of geophysical monitoring regarding permafrost degradation induced by hydrological processes, The Cryosphere, 11, 2957–2974, https://doi.org/10.5194/tc-11-2957-2017, 2017.
Mollaret, C., Hilbich, C., Pellet, C., Flores-Orozco, A., Delaloye, R., and Hauck, C.: Mountain permafrost degradation documented through a network of permanent electrical resistivity tomography sites, The Cryosphere, 13, 2557–2578, https://doi.org/10.5194/tc-13-2557-2019, 2019.
Oldenborger, G. A. and LeBlanc, A.-M.: Monitoring changes in unfrozen water
content with electrical resistivity surveys in cold continuous permafrost,
Geophys. J. Int., 215, 965–977,
https://doi.org/10.1093/gji/ggy321, 2018.
Oliva, M., Nývlt, D., and Pereira, P.: Recent regional climate cooling
on the Antarctic Peninsula and associated impacts on the cryosphere,
(December), STOTEN, 580, 210–223, https://doi.org/10.1016/j.scitotenv.2016.12.030,
2016.
Ottowitz, D., Jochum, B., Supper, R., Römer, A., Pfeiler, S., and
Keuschnig, M.: Permafrost monitoring at Mölltaler Glacier and
Magnetköp?, Berichte der Geologischen Bundesanstalt, 93, 57–64, 2011.
Ramos, M., Vieira, G., Gruber, S., Blanco, J. J., Hauck, C., Hidalgo, M. A.,
Tome, D., Neves, M., and Trindade, A.: Permafrost and active layer
monitoring in the Maritime Antarctic: Preliminary results from CALM sites on
Livingston and Deception Islands, US Geological Survey and the National
Academies; USGS OF-2007–1047, Short Research Paper 070
https://pubs.usgs.gov/of/2007/1047/srp/srp070/ (last access: 15 February 2019), 2008.
Ramos, M., Vieira, G., De Pablo, M. A., Molina, A., Abramov, A., and
Goyanes, G.: Recent shallowing of the thaw depth at Crater Lake, Deception
Island, Antarctica (2006–2014), Catena, 149, 519–528, https://doi.org/10.1016/j.catena.2016.07.019,
2017.
Rasmussen, L., Zhang, W., Hollesen, J., Cable, S., Christiansen, H.,
Jansson, P. E., and Elberling, B.: Modelling present and future permafrost
thermal regimes in Northeast Greenland, Cold Reg. Sci. Technol.,
146, 199–213, https://doi.org/10.1016/j.coldregions.2017.10.011, 2018.
Scherler, M., Hauck, C., Hoelzle, M., Stähli, M., and Völksch, I.:
Meltwater infiltration into the frozen active layer at an alpine permafrost
site, Permafrost Periglac., 21, 325–334, https://doi.org/10.1002/ppp.694,
2010.
Shur, Y., Hinkel, K. M., and Nelson, F. E.: The transient layer: implications
for geocryology and climate change science, Permafrost Periglac., 16, 5–17, https://doi.org/10.1002/ppp.518, 2005.
Smellie, J. L. and López-Martínez, J.: Geological map of Deception
Island, in: Geology and Geomorphology of Deception Island, edited by:
Smellie, J. L., López-Martínez, J., Serrano, E., and Rey, J., Sheet 6-A, 1:25.000,
BAS GEOMAP Series, British Antarctic Survey, Cambridge, 2002.
Styszynska, A.: The origin of coreless winters in the South Shetlands area
(Antarctica), Pol. Polar Res., 25, 45–66, 2004.
Supper, R., Ottowitz, D., Jochum, B., Romer, A., Pfeiler, S., Gruber, S.,
Keuschnig, M., and Ita, A.: Geoelectrical monitoring of frozen ground
andpermafrost in alpine areas: field studies and considerations towards an
improvedmeasuring technology, Near Surf. Geophys., 12, 93–115, https://doi.org/10.3997/1873-0604.2013057, 2014.
Tomaskovicova, S.: Coupled thermo-geophysical inversion for permafrost
monitoring, PhD thesis, Department of Civil Engineering, Technical
University of Denmark, Technical University of Denmark, Department of Civil Engineering, 2018.
Turner, J., Lu, H.,White, I., King, J. C., Phillips, T., Hosking, J. S.,
Bracegirdle, T. J., Marshall, G. J., Mulvaney, R., and Deb, P.: Absence of 21st
century warming on Antarctic Peninsula consistent with natural variability,
Nature, 535, 411–415, https://doi.org/10.1038/nature18645, 2016.
Vieira, G., López-Martínez, J., Serrano, E., Ramos, M., Gruber, S.,
Hauck, C., and Blanco, J. J., Geomorphological observations of permafrost and
ground-ice degradationon deception and Livingston Islands, Maritime
Antarctica, in: Proceedings of the 9th
International Conference on Permafrost, edited by: Kane, D. and Hinkel, K., 29 June–3 July 2008, Fairbanks,
Alaska, Extended Abstracts, Vol. 1, University of AlaskaPress, Fairbanks,
1839–1844, https://doi.org/10.5167/uzh-3320, 2008.
Vieira, G., Bockheim, J., Guglielmin, M., Balks, M., Abramov, A. A.,
Boelhouwers, J., Cannone, N., Ganzert, L., Gilichinsky, D. A., Goryachkin, G., López-Martínez, J., Meiklejohn, J., Raffi, R., Ramos, M.,
Schaefer, C., Serrano, E., Simas, F., Sletten, R., and Wagner, D.: Thermal
state of permafrost and active-layer monitoring in the Antarctic: advances
during the International Polar Year 2007–2009, Permafrost Periglac.,
21, 182–197, https://doi.org/10.1002/ppp.685, 2010.
Williams, P. J. and Smith, M. W.: The Frozen Earth. Fundamentals of Geocryology,
Cambridge University Press, Cambridge,
https://doi.org/10.1017/CBO9780511564437, 1989.
Short summary
A 2-D automated electrical resistivity tomography (A-ERT) system was installed for the first time in Antarctica at Deception Island to (i) monitor subsurface freezing and thawing processes on a daily and seasonal basis and map the spatial and temporal variability of thaw depth and to (ii) study the impact of short-lived extreme meteorological events on active layer dynamics.
A 2-D automated electrical resistivity tomography (A-ERT) system was installed for the first...
