Simulated high-latitude soil thermal dynamics during the past 4 decades
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAU International audience Soil temperature (Ts) change is a key indicator of the dynamics of permafrost. On seasonal and interannual timescales, the variability of Ts determines the active-layer depth, which regulates hydrological soil properties and biogeoch...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2016
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Online Access: | https://insu.hal.science/insu-01388162 https://insu.hal.science/insu-01388162/document https://insu.hal.science/insu-01388162/file/CRYOSPHERE%20-%20Simulated%20high-latitude%20soil%20thermal%20dynamics%20during%20the%20past%204%20decades.pdf https://doi.org/10.5194/tc-10-179-2016 |
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Open Polar |
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Météo-France: HAL |
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ftmeteofrance |
language |
English |
topic |
PERMAFROST CLIMATE FORCING HIGH LATITUDES CLIMATE SOIL TEMPERATURE CLIMATE MODEL LAND SURFACE MODEL [SDE]Environmental Sciences |
spellingShingle |
PERMAFROST CLIMATE FORCING HIGH LATITUDES CLIMATE SOIL TEMPERATURE CLIMATE MODEL LAND SURFACE MODEL [SDE]Environmental Sciences Peng, S. Ciais, Philippe Krinner, Gerhard Wang, Tao Gouttevin, Isabelle, Gouttevin Mcguire, A.D Lawrence, D. Burke, E. Chen, X. Decharme, B. Koven, C. Macdougall, A Rinke, A. Saito, K. Zhang, W. Alkama, R. Bohn, T.J Delire, C. Hajima, T Ji, D. Lettenmaier, D. P. Miller, P.A Moore, J.C. Smith, B. Sueyoshi, T Simulated high-latitude soil thermal dynamics during the past 4 decades |
topic_facet |
PERMAFROST CLIMATE FORCING HIGH LATITUDES CLIMATE SOIL TEMPERATURE CLIMATE MODEL LAND SURFACE MODEL [SDE]Environmental Sciences |
description |
[Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAU International audience Soil temperature (Ts) change is a key indicator of the dynamics of permafrost. On seasonal and interannual timescales, the variability of Ts determines the active-layer depth, which regulates hydrological soil properties and biogeochemical processes. On the multi-decadal scale, increasing Ts not only drives permafrost thaw/retreat but can also trigger and accelerate the decomposition of soil organic carbon. The magnitude of permafrost carbon feedbacks is thus closely linked to the rate of change of soil thermal regimes. In this study, we used nine process-based ecosystem models with permafrost processes, all forced by different observation-based climate forcing during the period 1960–2000, to characterize the warming rate of Ts in permafrost regions. There is a large spread of Ts trends at 20 cm depth across the models, with trend values ranging from 0.010 ± 0.003 to 0.031 ± 0.005 °C yr−1. Most models show smaller increase in Ts with increasing depth. Air temperature (Tsub>a) and longwave downward radiation (LWDR) are the main drivers of Ts trends, but their relative contributions differ amongst the models. Different trends of LWDR used in the forcing of models can explain 61 % of their differences in Ts trends, while trends of Ta only explain 5 % of the differences in Ts trends. Uncertain climate forcing contributes a larger uncertainty in Ts trends (0.021 ± 0.008 °C yr−1, mean ± standard deviation) than the uncertainty of model structure (0.012 ± 0.001 °C yr−1), diagnosed from the range of response between different models, normalized to the same forcing. In addition, the loss rate of near-surface permafrost area, defined as total area where the maximum seasonal active-layer thickness (ALT) is less than 3 m loss rate, is found to be significantly correlated with the magnitude of the trends of Ts at 1 m depth across the models (R = −0.85, P = 0.003), but not with the initial total near-surface permafrost area (R = −0.30, P = 0.438). The ... |
author2 |
Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) 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) ICOS-ATC (ICOS-ATC) 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)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) University of Alaska Fairbanks (UAF) National Center for Atmospheric Research Boulder (NCAR) Met Office Hadley Centre (MOHC) United Kingdom Met Office Exeter Department of Civil and Environmental Engineering, University of Washington University of Washington Seattle Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Lawrence Berkeley National Laboratory Berkeley (LBNL) University of Victoria Canada (UVIC) College of Global Change and Earth System Science (GCESS) Beijing Normal University (BNU) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association Research Institute for Global Change (RIGC) Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Department of Physical Geography and Ecosystem Science Lund Skane University Hospital Lund ASU School of Earth and Space Exploration (SESE) Arizona State University Tempe (ASU) National Institute of Polar Research Tokyo (NiPR) |
format |
Article in Journal/Newspaper |
author |
Peng, S. Ciais, Philippe Krinner, Gerhard Wang, Tao Gouttevin, Isabelle, Gouttevin Mcguire, A.D Lawrence, D. Burke, E. Chen, X. Decharme, B. Koven, C. Macdougall, A Rinke, A. Saito, K. Zhang, W. Alkama, R. Bohn, T.J Delire, C. Hajima, T Ji, D. Lettenmaier, D. P. Miller, P.A Moore, J.C. Smith, B. Sueyoshi, T |
author_facet |
Peng, S. Ciais, Philippe Krinner, Gerhard Wang, Tao Gouttevin, Isabelle, Gouttevin Mcguire, A.D Lawrence, D. Burke, E. Chen, X. Decharme, B. Koven, C. Macdougall, A Rinke, A. Saito, K. Zhang, W. Alkama, R. Bohn, T.J Delire, C. Hajima, T Ji, D. Lettenmaier, D. P. Miller, P.A Moore, J.C. Smith, B. Sueyoshi, T |
author_sort |
Peng, S. |
title |
Simulated high-latitude soil thermal dynamics during the past 4 decades |
title_short |
Simulated high-latitude soil thermal dynamics during the past 4 decades |
title_full |
Simulated high-latitude soil thermal dynamics during the past 4 decades |
title_fullStr |
Simulated high-latitude soil thermal dynamics during the past 4 decades |
title_full_unstemmed |
Simulated high-latitude soil thermal dynamics during the past 4 decades |
title_sort |
simulated high-latitude soil thermal dynamics during the past 4 decades |
publisher |
HAL CCSD |
publishDate |
2016 |
url |
https://insu.hal.science/insu-01388162 https://insu.hal.science/insu-01388162/document https://insu.hal.science/insu-01388162/file/CRYOSPHERE%20-%20Simulated%20high-latitude%20soil%20thermal%20dynamics%20during%20the%20past%204%20decades.pdf https://doi.org/10.5194/tc-10-179-2016 |
genre |
Active layer thickness permafrost The Cryosphere |
genre_facet |
Active layer thickness permafrost The Cryosphere |
op_source |
ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://insu.hal.science/insu-01388162 The Cryosphere, 2016, 10 (1), pp.179-192. ⟨10.5194/tc-10-179-2016⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-10-179-2016 insu-01388162 https://insu.hal.science/insu-01388162 https://insu.hal.science/insu-01388162/document https://insu.hal.science/insu-01388162/file/CRYOSPHERE%20-%20Simulated%20high-latitude%20soil%20thermal%20dynamics%20during%20the%20past%204%20decades.pdf doi:10.5194/tc-10-179-2016 IRSTEA: PUB00048373 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/tc-10-179-2016 |
container_title |
The Cryosphere |
container_volume |
10 |
container_issue |
1 |
container_start_page |
179 |
op_container_end_page |
192 |
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1801375670720266240 |
spelling |
ftmeteofrance:oai:HAL:insu-01388162v1 2024-06-09T07:37:50+00:00 Simulated high-latitude soil thermal dynamics during the past 4 decades Peng, S. Ciais, Philippe Krinner, Gerhard Wang, Tao Gouttevin, Isabelle, Gouttevin Mcguire, A.D Lawrence, D. Burke, E. Chen, X. Decharme, B. Koven, C. Macdougall, A Rinke, A. Saito, K. Zhang, W. Alkama, R. Bohn, T.J Delire, C. Hajima, T Ji, D. Lettenmaier, D. P. Miller, P.A Moore, J.C. Smith, B. Sueyoshi, T Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) 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) ICOS-ATC (ICOS-ATC) 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)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) University of Alaska Fairbanks (UAF) National Center for Atmospheric Research Boulder (NCAR) Met Office Hadley Centre (MOHC) United Kingdom Met Office Exeter Department of Civil and Environmental Engineering, University of Washington University of Washington Seattle Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Lawrence Berkeley National Laboratory Berkeley (LBNL) University of Victoria Canada (UVIC) College of Global Change and Earth System Science (GCESS) Beijing Normal University (BNU) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association Research Institute for Global Change (RIGC) Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Department of Physical Geography and Ecosystem Science Lund Skane University Hospital Lund ASU School of Earth and Space Exploration (SESE) Arizona State University Tempe (ASU) National Institute of Polar Research Tokyo (NiPR) 2016-01 https://insu.hal.science/insu-01388162 https://insu.hal.science/insu-01388162/document https://insu.hal.science/insu-01388162/file/CRYOSPHERE%20-%20Simulated%20high-latitude%20soil%20thermal%20dynamics%20during%20the%20past%204%20decades.pdf https://doi.org/10.5194/tc-10-179-2016 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-10-179-2016 insu-01388162 https://insu.hal.science/insu-01388162 https://insu.hal.science/insu-01388162/document https://insu.hal.science/insu-01388162/file/CRYOSPHERE%20-%20Simulated%20high-latitude%20soil%20thermal%20dynamics%20during%20the%20past%204%20decades.pdf doi:10.5194/tc-10-179-2016 IRSTEA: PUB00048373 info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://insu.hal.science/insu-01388162 The Cryosphere, 2016, 10 (1), pp.179-192. ⟨10.5194/tc-10-179-2016⟩ PERMAFROST CLIMATE FORCING HIGH LATITUDES CLIMATE SOIL TEMPERATURE CLIMATE MODEL LAND SURFACE MODEL [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2016 ftmeteofrance https://doi.org/10.5194/tc-10-179-2016 2024-05-16T12:05:20Z [Departement_IRSTEA]Eaux [TR1_IRSTEA]ARCEAU International audience Soil temperature (Ts) change is a key indicator of the dynamics of permafrost. On seasonal and interannual timescales, the variability of Ts determines the active-layer depth, which regulates hydrological soil properties and biogeochemical processes. On the multi-decadal scale, increasing Ts not only drives permafrost thaw/retreat but can also trigger and accelerate the decomposition of soil organic carbon. The magnitude of permafrost carbon feedbacks is thus closely linked to the rate of change of soil thermal regimes. In this study, we used nine process-based ecosystem models with permafrost processes, all forced by different observation-based climate forcing during the period 1960–2000, to characterize the warming rate of Ts in permafrost regions. There is a large spread of Ts trends at 20 cm depth across the models, with trend values ranging from 0.010 ± 0.003 to 0.031 ± 0.005 °C yr−1. Most models show smaller increase in Ts with increasing depth. Air temperature (Tsub>a) and longwave downward radiation (LWDR) are the main drivers of Ts trends, but their relative contributions differ amongst the models. Different trends of LWDR used in the forcing of models can explain 61 % of their differences in Ts trends, while trends of Ta only explain 5 % of the differences in Ts trends. Uncertain climate forcing contributes a larger uncertainty in Ts trends (0.021 ± 0.008 °C yr−1, mean ± standard deviation) than the uncertainty of model structure (0.012 ± 0.001 °C yr−1), diagnosed from the range of response between different models, normalized to the same forcing. In addition, the loss rate of near-surface permafrost area, defined as total area where the maximum seasonal active-layer thickness (ALT) is less than 3 m loss rate, is found to be significantly correlated with the magnitude of the trends of Ts at 1 m depth across the models (R = −0.85, P = 0.003), but not with the initial total near-surface permafrost area (R = −0.30, P = 0.438). The ... Article in Journal/Newspaper Active layer thickness permafrost The Cryosphere Météo-France: HAL The Cryosphere 10 1 179 192 |