Coupled thermo–geophysical inversion for permafrost monitoring

This study explores an alternative way of deriving soil thermal properties from surface geophysical measurements. We combined ground surface temperature time series with time lapse geoelectrical acquisitions measured from the ground surface in a fully coupled inversion scheme to calibrate a heat con...

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Published in:The Cryosphere
Main Authors: Tomaškovičová, Soňa, Ingeman-Nielsen, Thomas
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/tc-18-321-2024
https://tc.copernicus.org/articles/18/321/2024/
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spelling ftcopernicus:oai:publications.copernicus.org:tc110362 2024-09-15T18:30:03+00:00 Coupled thermo–geophysical inversion for permafrost monitoring Tomaškovičová, Soňa Ingeman-Nielsen, Thomas 2024-01-17 application/pdf https://doi.org/10.5194/tc-18-321-2024 https://tc.copernicus.org/articles/18/321/2024/ eng eng doi:10.5194/tc-18-321-2024 https://tc.copernicus.org/articles/18/321/2024/ eISSN: 1994-0424 Text 2024 ftcopernicus https://doi.org/10.5194/tc-18-321-2024 2024-08-28T05:24:15Z This study explores an alternative way of deriving soil thermal properties from surface geophysical measurements. We combined ground surface temperature time series with time lapse geoelectrical acquisitions measured from the ground surface in a fully coupled inversion scheme to calibrate a heat conduction model. The quantitative link between the thermal and geoelectrical parts of the modeling framework is the temperature-dependent unfrozen water content, which is also the main factor influencing electrical response of the ground. The apparent resistivity data were incorporated into the coupled framework without being inverted separately, thus reducing the uncertainty inevitably associated with inverted resistivity models. We show that geoelectrical time lapse data are useful as alternative calibration data and can provide as good results as borehole temperature measurements. The fully coupled modeling framework using field data achieved performance comparable to calibration on borehole temperature records in terms of model fit within 0.6 ∘ C, inversion convergence metrics, as well as the predictive performance of the calibrated model. Text permafrost Copernicus Publications: E-Journals The Cryosphere 18 1 321 340
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description This study explores an alternative way of deriving soil thermal properties from surface geophysical measurements. We combined ground surface temperature time series with time lapse geoelectrical acquisitions measured from the ground surface in a fully coupled inversion scheme to calibrate a heat conduction model. The quantitative link between the thermal and geoelectrical parts of the modeling framework is the temperature-dependent unfrozen water content, which is also the main factor influencing electrical response of the ground. The apparent resistivity data were incorporated into the coupled framework without being inverted separately, thus reducing the uncertainty inevitably associated with inverted resistivity models. We show that geoelectrical time lapse data are useful as alternative calibration data and can provide as good results as borehole temperature measurements. The fully coupled modeling framework using field data achieved performance comparable to calibration on borehole temperature records in terms of model fit within 0.6 ∘ C, inversion convergence metrics, as well as the predictive performance of the calibrated model.
format Text
author Tomaškovičová, Soňa
Ingeman-Nielsen, Thomas
spellingShingle Tomaškovičová, Soňa
Ingeman-Nielsen, Thomas
Coupled thermo–geophysical inversion for permafrost monitoring
author_facet Tomaškovičová, Soňa
Ingeman-Nielsen, Thomas
author_sort Tomaškovičová, Soňa
title Coupled thermo–geophysical inversion for permafrost monitoring
title_short Coupled thermo–geophysical inversion for permafrost monitoring
title_full Coupled thermo–geophysical inversion for permafrost monitoring
title_fullStr Coupled thermo–geophysical inversion for permafrost monitoring
title_full_unstemmed Coupled thermo–geophysical inversion for permafrost monitoring
title_sort coupled thermo–geophysical inversion for permafrost monitoring
publishDate 2024
url https://doi.org/10.5194/tc-18-321-2024
https://tc.copernicus.org/articles/18/321/2024/
genre permafrost
genre_facet permafrost
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-18-321-2024
https://tc.copernicus.org/articles/18/321/2024/
op_doi https://doi.org/10.5194/tc-18-321-2024
container_title The Cryosphere
container_volume 18
container_issue 1
container_start_page 321
op_container_end_page 340
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