Permafrost Hydrogeology of Taylor Valley, Antarctica: Insights From Deep Electrical Resistivity Tomography

Abstract Global warming has prompted globally widespread permafrost thawing, resulting in enhanced greenhouse gas release into the atmosphere. Studies conducted in the Northern Hemisphere reveal an alarming increase in permafrost thawing. However, similar data from Antarctica are scarce. We conducted a 2‐D Deep Electrical Resistivity Tomography (DERT) survey in Taylor Valley, Antarctica, to image the distribution of permafrost, its thicknesses, lower boundaries, and hydrogeology. Results show resistive, discontinuous domains that we suggest represent permafrost units. We also find highly conductive layers (5–10 Ω·m), between 300–350 m and 600–650 m below ground level and a shallower (∼50–100 m depth) conductive layer. The combined data set reveals a broad brine system in Taylor Valley, implying multi‐tiered groundwater circulation: a shallow, localized system linked with surface water bodies and a separate deeper, regional circulation system. The arrangement of these brines across different levels, coupled with the uneven permafrost distribution, underscores potential interplay between the two systems.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-09-16
DOI
https://doi.org/10.1029/2023gl106912
Citations
3
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
1.13

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article

Permafrost Hydrogeology of Taylor Valley, Antarctica: Insights From Deep Electrical Resistivity Tomography

Fabio Florindo, G. S. Wilson, Adriano Mazzini, Claudio Mazzoli et al.
3 citations
Geophysical Research Letters
Climate change and permafrost
1.13
article

Permafrost Hydrogeology of Taylor Valley, Antarctica: Insights From Deep Electrical Resistivity Tomography

Fabio Florindo, G. S. Wilson, Adriano Mazzini, Claudio Mazzoli, J. Anderson, Bob Dagg, Livio Ruggiero, Maria Chiara Tartarello, Federico Fischanger, Massimiliano Ascani, Valentina Romanò, Rachel Worthington, Alessandra Sciarra, Richard Hardie
article en
3 citations

Abstract

Abstract Global warming has prompted globally widespread permafrost thawing, resulting in enhanced greenhouse gas release into the atmosphere. Studies conducted in the Northern Hemisphere reveal an alarming increase in permafrost thawing. However, similar data from Antarctica are scarce. We conducted a 2‐D Deep Electrical Resistivity Tomography (DERT) survey in Taylor Valley, Antarctica, to image the distribution of permafrost, its thicknesses, lower boundaries, and hydrogeology. Results show resistive, discontinuous domains that we suggest represent permafrost units. We also find highly conductive layers (5–10 Ω·m), between 300–350 m and 600–650 m below ground level and a shallower (∼50–100 m depth) conductive layer. The combined data set reveals a broad brine system in Taylor Valley, implying multi‐tiered groundwater circulation: a shallow, localized system linked with surface water bodies and a separate deeper, regional circulation system. The arrangement of these brines across different levels, coupled with the uneven permafrost distribution, underscores potential interplay between the two systems.

Geophysical Research LettersVol. 51(18)
GNS Science (NZ), University of Padua (IT), University of Oslo (NO), Government of New Zealand (NZ), Istituto Nazionale di Geofisica e Vulcanologia (IT), Institute for Energy Technology (NO), Consorzio Roma Ricerche (IT), Department of Internal Affairs (NZ), University of Waikato (NZ), University of Otago (NZ), Sapienza University of Rome (IT)
New Zealand Antarctic Research Institute
Openalex Percentile: Top 24%
Climate change and permafrost
1.13
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