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: S. Tomaškovičová, T. Ingeman-Nielsen
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2024
Subjects:
Online Access:https://doi.org/10.5194/tc-18-321-2024
https://doaj.org/article/50f234735aca49ce9d6433b53ae24482
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spelling ftdoajarticles:oai:doaj.org/article:50f234735aca49ce9d6433b53ae24482 2024-02-11T10:07:53+01:00 Coupled thermo–geophysical inversion for permafrost monitoring S. Tomaškovičová T. Ingeman-Nielsen 2024-01-01T00:00:00Z https://doi.org/10.5194/tc-18-321-2024 https://doaj.org/article/50f234735aca49ce9d6433b53ae24482 EN eng Copernicus Publications https://tc.copernicus.org/articles/18/321/2024/tc-18-321-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-321-2024 1994-0416 1994-0424 https://doaj.org/article/50f234735aca49ce9d6433b53ae24482 The Cryosphere, Vol 18, Pp 321-340 (2024) Environmental sciences GE1-350 Geology QE1-996.5 article 2024 ftdoajarticles https://doi.org/10.5194/tc-18-321-2024 2024-01-21T01:40:30Z 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. Article in Journal/Newspaper permafrost The Cryosphere Directory of Open Access Journals: DOAJ Articles The Cryosphere 18 1 321 340
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
S. Tomaškovičová
T. Ingeman-Nielsen
Coupled thermo–geophysical inversion for permafrost monitoring
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
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 Article in Journal/Newspaper
author S. Tomaškovičová
T. Ingeman-Nielsen
author_facet S. Tomaškovičová
T. Ingeman-Nielsen
author_sort S. Tomaškovičová
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
publisher Copernicus Publications
publishDate 2024
url https://doi.org/10.5194/tc-18-321-2024
https://doaj.org/article/50f234735aca49ce9d6433b53ae24482
genre permafrost
The Cryosphere
genre_facet permafrost
The Cryosphere
op_source The Cryosphere, Vol 18, Pp 321-340 (2024)
op_relation https://tc.copernicus.org/articles/18/321/2024/tc-18-321-2024.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-18-321-2024
1994-0416
1994-0424
https://doaj.org/article/50f234735aca49ce9d6433b53ae24482
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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