The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results

Interfrost Team International audience Climate change impacts in permafrost regions have received considerable attention recently due to the pronounced warming trends experienced in recent decades and which have been projected into the future. Large portions of these permafrost regions are character...

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Main Authors: Grenier, Christophe, Rühaak, Wolfram
Other Authors: Biologie Neurovasculaire et Mitochondriale Intégrée (BNMI), Université d'Angers (UA)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS), Technische Universität Darmstadt - Technical University of Darmstadt (TU Darmstadt), Department of Geothermal Science and Technology, Institute of Applied Geosciences Darmstadt (IAG), Darmstadt University of Technology Darmstadt -Darmstadt University of Technology Darmstadt, EGU, InterFrost Team
Format: Conference Object
Language:English
Published: HAL CCSD 2016
Subjects:
Online Access:https://hal.science/hal-01396563
https://hal.science/hal-01396563/document
https://hal.science/hal-01396563/file/EGU2016-11310.pdf
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spelling ftunivangershal:oai:HAL:hal-01396563v1 2024-05-19T07:47:07+00:00 The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results Grenier, Christophe Rühaak, Wolfram Biologie Neurovasculaire et Mitochondriale Intégrée (BNMI) Université d'Angers (UA)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS) Technische Universität Darmstadt - Technical University of Darmstadt (TU Darmstadt) Department of Geothermal Science and Technology Institute of Applied Geosciences Darmstadt (IAG) Darmstadt University of Technology Darmstadt -Darmstadt University of Technology Darmstadt EGU InterFrost Team Viennes, Austria 2016-04-18 https://hal.science/hal-01396563 https://hal.science/hal-01396563/document https://hal.science/hal-01396563/file/EGU2016-11310.pdf en eng HAL CCSD hal-01396563 https://hal.science/hal-01396563 https://hal.science/hal-01396563/document https://hal.science/hal-01396563/file/EGU2016-11310.pdf info:eu-repo/semantics/OpenAccess Geophysical Research Abstracts EGU General Assembly 2016 https://hal.science/hal-01396563 EGU General Assembly 2016, EGU Apr 2016, Viennes, Austria. pp.2016 - 11310 [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/conferenceObject Conference papers 2016 ftunivangershal 2024-04-19T00:49:54Z Interfrost Team International audience Climate change impacts in permafrost regions have received considerable attention recently due to the pronounced warming trends experienced in recent decades and which have been projected into the future. Large portions of these permafrost regions are characterized by surface water bodies (lakes, rivers) that interact with the surrounding permafrost often generating taliks (unfrozen zones) within the permafrost that allow for hydrologic interactions between the surface water bodies and underlying aquifers and thus influence the hydrologic response of a landscape to climate change. Recent field studies and modeling exercises indicate that a fully coupled 2D or 3D Thermo-Hydraulic (TH) approach is required to understand and model past and future evolution such units (Kurylyk et al. 2014). However, there is presently a paucity of 3D numerical studies of permafrost thaw and associated hydrological changes, which can be partly attributed to the difficulty in verifying multi-dimensional results produced by numerical models. A benchmark exercise was initialized at the end of 2014. Participants convened from USA, Canada, Eu-rope, representing 13 simulation codes. The benchmark exercises consist of several test cases inspired by existing literature (e.g. McKenzie et al., 2007) as well as new ones (Kurylyk et al. 2014; Grenier et al. in prep.; Rühaak et al. 2015). They range from simpler, purely thermal 1D cases to more complex, coupled 2D TH cases (benchmarks TH1, TH2, and TH3). Some experimental cases conducted in a cold room complement the validation approach. A web site hosted by LSCE (Laboratoire des Sciences du Climat et de l'Environnement) is an interaction platform for the participants and hosts the test case databases at the following address: https://wiki.lsce.ipsl.fr/interfrost. The results of the first stage of the benchmark exercise will be presented. We will mainly focus on the inter-comparison of participant results for the coupled cases TH2 & TH3. Both cases ... Conference Object permafrost Portail des publications scientifiques de l’Université d’Angers (HAL)
institution Open Polar
collection Portail des publications scientifiques de l’Université d’Angers (HAL)
op_collection_id ftunivangershal
language English
topic [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE]Environmental Sciences
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE]Environmental Sciences
[SDE.MCG]Environmental Sciences/Global Changes
Grenier, Christophe
Rühaak, Wolfram
The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results
topic_facet [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE]Environmental Sciences
[SDE.MCG]Environmental Sciences/Global Changes
description Interfrost Team International audience Climate change impacts in permafrost regions have received considerable attention recently due to the pronounced warming trends experienced in recent decades and which have been projected into the future. Large portions of these permafrost regions are characterized by surface water bodies (lakes, rivers) that interact with the surrounding permafrost often generating taliks (unfrozen zones) within the permafrost that allow for hydrologic interactions between the surface water bodies and underlying aquifers and thus influence the hydrologic response of a landscape to climate change. Recent field studies and modeling exercises indicate that a fully coupled 2D or 3D Thermo-Hydraulic (TH) approach is required to understand and model past and future evolution such units (Kurylyk et al. 2014). However, there is presently a paucity of 3D numerical studies of permafrost thaw and associated hydrological changes, which can be partly attributed to the difficulty in verifying multi-dimensional results produced by numerical models. A benchmark exercise was initialized at the end of 2014. Participants convened from USA, Canada, Eu-rope, representing 13 simulation codes. The benchmark exercises consist of several test cases inspired by existing literature (e.g. McKenzie et al., 2007) as well as new ones (Kurylyk et al. 2014; Grenier et al. in prep.; Rühaak et al. 2015). They range from simpler, purely thermal 1D cases to more complex, coupled 2D TH cases (benchmarks TH1, TH2, and TH3). Some experimental cases conducted in a cold room complement the validation approach. A web site hosted by LSCE (Laboratoire des Sciences du Climat et de l'Environnement) is an interaction platform for the participants and hosts the test case databases at the following address: https://wiki.lsce.ipsl.fr/interfrost. The results of the first stage of the benchmark exercise will be presented. We will mainly focus on the inter-comparison of participant results for the coupled cases TH2 & TH3. Both cases ...
author2 Biologie Neurovasculaire et Mitochondriale Intégrée (BNMI)
Université d'Angers (UA)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS)
Technische Universität Darmstadt - Technical University of Darmstadt (TU Darmstadt)
Department of Geothermal Science and Technology
Institute of Applied Geosciences Darmstadt (IAG)
Darmstadt University of Technology Darmstadt -Darmstadt University of Technology Darmstadt
EGU
InterFrost Team
format Conference Object
author Grenier, Christophe
Rühaak, Wolfram
author_facet Grenier, Christophe
Rühaak, Wolfram
author_sort Grenier, Christophe
title The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results
title_short The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results
title_full The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results
title_fullStr The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results
title_full_unstemmed The InterFrost benchmark of Thermo-Hydraulic codes for cold regions hydrology – first inter-comparison phase results
title_sort interfrost benchmark of thermo-hydraulic codes for cold regions hydrology – first inter-comparison phase results
publisher HAL CCSD
publishDate 2016
url https://hal.science/hal-01396563
https://hal.science/hal-01396563/document
https://hal.science/hal-01396563/file/EGU2016-11310.pdf
op_coverage Viennes, Austria
genre permafrost
genre_facet permafrost
op_source Geophysical Research Abstracts
EGU General Assembly 2016
https://hal.science/hal-01396563
EGU General Assembly 2016, EGU Apr 2016, Viennes, Austria. pp.2016 - 11310
op_relation hal-01396563
https://hal.science/hal-01396563
https://hal.science/hal-01396563/document
https://hal.science/hal-01396563/file/EGU2016-11310.pdf
op_rights info:eu-repo/semantics/OpenAccess
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