Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics

International audience Arctic regions are highly impacted by the global temperature rising and its consequences and influences on the thermo-hydro processes and their feedbacks. Theses processes are especially not very well understood in the context of river–permafrost interactions and permafrost de...

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Published in:Remote Sensing
Main Authors: Léger, Emmanuel, Saintenoy, Albane, Grenier, Christophe, Séjourné, Antoine, Pohl, Eric, Bouchard, Frédéric, Pessel, Marc, Bazhin, Kirill, Danilov, Kencheeri, Costard, François, Mugler, Claude, Fedorov, Alexander, Khristoforov, Ivan, Konstantinov, Pavel
Other Authors: Géosciences Paris Saclay (GEOPS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Modélisation Hydrologique (HYDRO), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Department of Geosciences Fribourg, Albert-Ludwigs-Universität Freiburg, Département de géomatique appliquée Sherbrooke (UdeS), Université de Sherbrooke (UdeS), Melnikov Permafrost Institute, Siberian Branch of the Russian Academy of Sciences (SB RAS), ANR-19-CE46-0003,HiPerBorea,Calul haute performance pour la quantification des impacts du changement climatique sur les régions boréales(2019)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://hal.science/hal-04103637
https://hal.science/hal-04103637/document
https://hal.science/hal-04103637/file/remotesensing-15-02524.pdf
https://doi.org/10.3390/rs15102524
id ftuniversailles:oai:HAL:hal-04103637v1
record_format openpolar
institution Open Polar
collection Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ
op_collection_id ftuniversailles
language English
topic near-surface geophysics
river thermal influence
cryosphere
thermal modeling
[SDU]Sciences of the Universe [physics]
spellingShingle near-surface geophysics
river thermal influence
cryosphere
thermal modeling
[SDU]Sciences of the Universe [physics]
Léger, Emmanuel
Saintenoy, Albane
Grenier, Christophe
Séjourné, Antoine
Pohl, Eric
Bouchard, Frédéric
Pessel, Marc
Bazhin, Kirill
Danilov, Kencheeri
Costard, François
Mugler, Claude
Fedorov, Alexander
Khristoforov, Ivan
Konstantinov, Pavel
Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics
topic_facet near-surface geophysics
river thermal influence
cryosphere
thermal modeling
[SDU]Sciences of the Universe [physics]
description International audience Arctic regions are highly impacted by the global temperature rising and its consequences and influences on the thermo-hydro processes and their feedbacks. Theses processes are especially not very well understood in the context of river–permafrost interactions and permafrost degradation. This paper focuses on the thermal characterization of a river–valley system in a continuous permafrost area (Syrdakh, Yakutia, Eastern Siberia) that is subject to intense thawing, with major consequences on water resources and quality. We investigated this Yakutian area through two transects crossing the river using classical tools such as in–situ temperature measurements, direct active layer thickness estimations, unscrewed aerial vehicle (UAV) imagery, heat transfer numerical experiments, Ground-Penetrating Radar (GPR), and Electrical Resistivity Tomography (ERT). Of these two transects, one was closely investigated with a long-term temperature time series from 2012 to 2018, while both of them were surveyed by geophysical and UAV data acquisition in 2017 and 2018. Thermodynamical numerical simulations were run based on the long-term temperature series and are in agreement with river thermal influence on permafrost and active layer extensions retrieved from GPR and ERT profiles. An electrical resistivity-temperature relationship highlights the predominant role of water in such a complicated system and paves the way to coupled thermo-hydro-geophysical modeling for understanding permafrost–river system evolution.
author2 Géosciences Paris Saclay (GEOPS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Modélisation Hydrologique (HYDRO)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Department of Geosciences Fribourg
Albert-Ludwigs-Universität Freiburg
Département de géomatique appliquée Sherbrooke (UdeS)
Université de Sherbrooke (UdeS)
Melnikov Permafrost Institute
Siberian Branch of the Russian Academy of Sciences (SB RAS)
ANR-19-CE46-0003,HiPerBorea,Calul haute performance pour la quantification des impacts du changement climatique sur les régions boréales(2019)
format Article in Journal/Newspaper
author Léger, Emmanuel
Saintenoy, Albane
Grenier, Christophe
Séjourné, Antoine
Pohl, Eric
Bouchard, Frédéric
Pessel, Marc
Bazhin, Kirill
Danilov, Kencheeri
Costard, François
Mugler, Claude
Fedorov, Alexander
Khristoforov, Ivan
Konstantinov, Pavel
author_facet Léger, Emmanuel
Saintenoy, Albane
Grenier, Christophe
Séjourné, Antoine
Pohl, Eric
Bouchard, Frédéric
Pessel, Marc
Bazhin, Kirill
Danilov, Kencheeri
Costard, François
Mugler, Claude
Fedorov, Alexander
Khristoforov, Ivan
Konstantinov, Pavel
author_sort Léger, Emmanuel
title Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics
title_short Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics
title_full Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics
title_fullStr Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics
title_full_unstemmed Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics
title_sort comparing thermal regime stages along a small yakutian fluvial valley with point scale measurements, thermal modeling, and near surface geophysics
publisher HAL CCSD
publishDate 2023
url https://hal.science/hal-04103637
https://hal.science/hal-04103637/document
https://hal.science/hal-04103637/file/remotesensing-15-02524.pdf
https://doi.org/10.3390/rs15102524
genre Active layer thickness
Arctic
permafrost
Yakutia
Siberia
genre_facet Active layer thickness
Arctic
permafrost
Yakutia
Siberia
op_source ISSN: 2072-4292
Remote Sensing
https://hal.science/hal-04103637
Remote Sensing, 2023, 15 (10), pp.2524. ⟨10.3390/rs15102524⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3390/rs15102524
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https://hal.science/hal-04103637/document
https://hal.science/hal-04103637/file/remotesensing-15-02524.pdf
doi:10.3390/rs15102524
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3390/rs15102524
container_title Remote Sensing
container_volume 15
container_issue 10
container_start_page 2524
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spelling ftuniversailles:oai:HAL:hal-04103637v1 2024-05-19T07:27:26+00:00 Comparing Thermal Regime Stages along a Small Yakutian Fluvial Valley with Point Scale Measurements, Thermal Modeling, and Near Surface Geophysics Léger, Emmanuel Saintenoy, Albane Grenier, Christophe Séjourné, Antoine Pohl, Eric Bouchard, Frédéric Pessel, Marc Bazhin, Kirill Danilov, Kencheeri Costard, François Mugler, Claude Fedorov, Alexander Khristoforov, Ivan Konstantinov, Pavel Géosciences Paris Saclay (GEOPS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modélisation Hydrologique (HYDRO) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Department of Geosciences Fribourg Albert-Ludwigs-Universität Freiburg Département de géomatique appliquée Sherbrooke (UdeS) Université de Sherbrooke (UdeS) Melnikov Permafrost Institute Siberian Branch of the Russian Academy of Sciences (SB RAS) ANR-19-CE46-0003,HiPerBorea,Calul haute performance pour la quantification des impacts du changement climatique sur les régions boréales(2019) 2023-05 https://hal.science/hal-04103637 https://hal.science/hal-04103637/document https://hal.science/hal-04103637/file/remotesensing-15-02524.pdf https://doi.org/10.3390/rs15102524 en eng HAL CCSD MDPI info:eu-repo/semantics/altIdentifier/doi/10.3390/rs15102524 hal-04103637 https://hal.science/hal-04103637 https://hal.science/hal-04103637/document https://hal.science/hal-04103637/file/remotesensing-15-02524.pdf doi:10.3390/rs15102524 info:eu-repo/semantics/OpenAccess ISSN: 2072-4292 Remote Sensing https://hal.science/hal-04103637 Remote Sensing, 2023, 15 (10), pp.2524. ⟨10.3390/rs15102524⟩ near-surface geophysics river thermal influence cryosphere thermal modeling [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2023 ftuniversailles https://doi.org/10.3390/rs15102524 2024-05-02T00:02:05Z International audience Arctic regions are highly impacted by the global temperature rising and its consequences and influences on the thermo-hydro processes and their feedbacks. Theses processes are especially not very well understood in the context of river–permafrost interactions and permafrost degradation. This paper focuses on the thermal characterization of a river–valley system in a continuous permafrost area (Syrdakh, Yakutia, Eastern Siberia) that is subject to intense thawing, with major consequences on water resources and quality. We investigated this Yakutian area through two transects crossing the river using classical tools such as in–situ temperature measurements, direct active layer thickness estimations, unscrewed aerial vehicle (UAV) imagery, heat transfer numerical experiments, Ground-Penetrating Radar (GPR), and Electrical Resistivity Tomography (ERT). Of these two transects, one was closely investigated with a long-term temperature time series from 2012 to 2018, while both of them were surveyed by geophysical and UAV data acquisition in 2017 and 2018. Thermodynamical numerical simulations were run based on the long-term temperature series and are in agreement with river thermal influence on permafrost and active layer extensions retrieved from GPR and ERT profiles. An electrical resistivity-temperature relationship highlights the predominant role of water in such a complicated system and paves the way to coupled thermo-hydro-geophysical modeling for understanding permafrost–river system evolution. Article in Journal/Newspaper Active layer thickness Arctic permafrost Yakutia Siberia Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ Remote Sensing 15 10 2524