Soil moisture and hydrology projections of the permafrost region – a model intercomparison
International audience This study investigates and compares soil moisture and hydrology projections of broadly used land models with permafrost processes and highlights the causes and impacts of permafrost zone soil moisture projections. Climate models project warmer temperatures and increases in pr...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2020
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Subjects: | |
Online Access: | https://hal.inrae.fr/hal-03259447 https://hal.inrae.fr/hal-03259447/document https://hal.inrae.fr/hal-03259447/file/tc-14-445-2020.pdf https://doi.org/10.5194/tc-14-445-2020 |
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ftinsu:oai:HAL:hal-03259447v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
Ice-wedge Degradation Land-surface Model Thermal Dynamics Polygonal Tundra Frozen Soil Carbon Water Co2 Fluxes System [SHS.GEO]Humanities and Social Sciences/Geography |
spellingShingle |
Ice-wedge Degradation Land-surface Model Thermal Dynamics Polygonal Tundra Frozen Soil Carbon Water Co2 Fluxes System [SHS.GEO]Humanities and Social Sciences/Geography Andresen, Christian Lawrence, David Wilson, Cathy Mcguire, A. David Koven, Charles Schaefer, Kevin Jafarov, Elchin Peng, Shushi Chen, Xiaodong Gouttevin, Isabelle Burke, Eleanor Chadburn, Sarah Ji, Duoying Chen, Guangsheng Hayes, Daniel Zhang, Wenxin Soil moisture and hydrology projections of the permafrost region – a model intercomparison |
topic_facet |
Ice-wedge Degradation Land-surface Model Thermal Dynamics Polygonal Tundra Frozen Soil Carbon Water Co2 Fluxes System [SHS.GEO]Humanities and Social Sciences/Geography |
description |
International audience This study investigates and compares soil moisture and hydrology projections of broadly used land models with permafrost processes and highlights the causes and impacts of permafrost zone soil moisture projections. Climate models project warmer temperatures and increases in precipitation (P) which will intensify evapotranspiration (ET) and runoff in land models. However, this study shows that most models project a long-term drying of the surface soil (0-20 cm) for the permafrost region despite increases in the net air-surface water flux (P-ET). Drying is generally explained by infiltration of moisture to deeper soil layers as the active layer deepens or permafrost thaws completely. Although most models agree on drying, the projections vary strongly in magnitude and spatial pattern. Land models tend to agree with decadal runoff trends but underestimate runoff volume when compared to gauge data across the major Arctic river basins, potentially indicating model structural limitations. Coordinated efforts to address the ongoing challenges presented in this study will help reduce uncertainty in our capability to predict the future Arctic hydrological state and associated land-atmosphere biogeochemical processes across spatial and temporal scales. |
author2 |
Department of Geography University of Wisconsin-Madison Earth and Environmental Sciences Division Los Alamos Los Alamos National Laboratory (LANL) National Center for Atmospheric Research Boulder (NCAR) Institute of Arctic Biology University of Alaska Fairbanks (UAF) Climate and Ecosystem Sciences Division Lawrence Berkeley National Laboratory Berkeley (LBNL) Institute of Arctic Alpine Research University of Colorado Boulder (INSTAAR) University of Colorado Boulder Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) College of Urban and Environmental Sciences Beijing Peking University Beijing Department of Civil and Environmental Engineering Seattle University of Washington Seattle Atmospheric Sciences and Global Change Division Pacific Northwest National Laboratory (PNNL) RiverLy - Fonctionnement des hydrosystèmes (RiverLy) Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Met Office Hadley Centre (MOHC) United Kingdom Met Office Exeter School of Earth and Environment Leeds (SEE) University of Leeds College of Global Change and Earth System Science (GCESS) Beijing Normal University (BNU) Environmental Sciences Division Oak Ridge Oak Ridge National Laboratory Oak Ridge (ORNL) UT-Battelle, LLC-UT-Battelle, LLC School of Forest Resources University of Maine Department of Physical Geography and Ecosystem Science Lund Skane University Hospital Lund Center for Permafrost (CENPERM) Department of Geosciences and Natural Resource Management Copenhagen (IGN) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) United States Department of Energy (DOE) : ERKP757 |
format |
Article in Journal/Newspaper |
author |
Andresen, Christian Lawrence, David Wilson, Cathy Mcguire, A. David Koven, Charles Schaefer, Kevin Jafarov, Elchin Peng, Shushi Chen, Xiaodong Gouttevin, Isabelle Burke, Eleanor Chadburn, Sarah Ji, Duoying Chen, Guangsheng Hayes, Daniel Zhang, Wenxin |
author_facet |
Andresen, Christian Lawrence, David Wilson, Cathy Mcguire, A. David Koven, Charles Schaefer, Kevin Jafarov, Elchin Peng, Shushi Chen, Xiaodong Gouttevin, Isabelle Burke, Eleanor Chadburn, Sarah Ji, Duoying Chen, Guangsheng Hayes, Daniel Zhang, Wenxin |
author_sort |
Andresen, Christian |
title |
Soil moisture and hydrology projections of the permafrost region – a model intercomparison |
title_short |
Soil moisture and hydrology projections of the permafrost region – a model intercomparison |
title_full |
Soil moisture and hydrology projections of the permafrost region – a model intercomparison |
title_fullStr |
Soil moisture and hydrology projections of the permafrost region – a model intercomparison |
title_full_unstemmed |
Soil moisture and hydrology projections of the permafrost region – a model intercomparison |
title_sort |
soil moisture and hydrology projections of the permafrost region – a model intercomparison |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.inrae.fr/hal-03259447 https://hal.inrae.fr/hal-03259447/document https://hal.inrae.fr/hal-03259447/file/tc-14-445-2020.pdf https://doi.org/10.5194/tc-14-445-2020 |
genre |
Ice permafrost The Cryosphere Tundra wedge* |
genre_facet |
Ice permafrost The Cryosphere Tundra wedge* |
op_source |
ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal.inrae.fr/hal-03259447 The Cryosphere, 2020, 14 (2), pp.445-459. ⟨10.5194/tc-14-445-2020⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-14-445-2020 hal-03259447 https://hal.inrae.fr/hal-03259447 https://hal.inrae.fr/hal-03259447/document https://hal.inrae.fr/hal-03259447/file/tc-14-445-2020.pdf doi:10.5194/tc-14-445-2020 WOS: 000513000800001 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/tc-14-445-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
2 |
container_start_page |
445 |
op_container_end_page |
459 |
_version_ |
1796944071461175296 |
spelling |
ftinsu:oai:HAL:hal-03259447v1 2024-04-21T08:04:29+00:00 Soil moisture and hydrology projections of the permafrost region – a model intercomparison Andresen, Christian Lawrence, David Wilson, Cathy Mcguire, A. David Koven, Charles Schaefer, Kevin Jafarov, Elchin Peng, Shushi Chen, Xiaodong Gouttevin, Isabelle Burke, Eleanor Chadburn, Sarah Ji, Duoying Chen, Guangsheng Hayes, Daniel Zhang, Wenxin Department of Geography University of Wisconsin-Madison Earth and Environmental Sciences Division Los Alamos Los Alamos National Laboratory (LANL) National Center for Atmospheric Research Boulder (NCAR) Institute of Arctic Biology University of Alaska Fairbanks (UAF) Climate and Ecosystem Sciences Division Lawrence Berkeley National Laboratory Berkeley (LBNL) Institute of Arctic Alpine Research University of Colorado Boulder (INSTAAR) University of Colorado Boulder Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) College of Urban and Environmental Sciences Beijing Peking University Beijing Department of Civil and Environmental Engineering Seattle University of Washington Seattle Atmospheric Sciences and Global Change Division Pacific Northwest National Laboratory (PNNL) RiverLy - Fonctionnement des hydrosystèmes (RiverLy) Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Met Office Hadley Centre (MOHC) United Kingdom Met Office Exeter School of Earth and Environment Leeds (SEE) University of Leeds College of Global Change and Earth System Science (GCESS) Beijing Normal University (BNU) Environmental Sciences Division Oak Ridge Oak Ridge National Laboratory Oak Ridge (ORNL) UT-Battelle, LLC-UT-Battelle, LLC School of Forest Resources University of Maine Department of Physical Geography and Ecosystem Science Lund Skane University Hospital Lund Center for Permafrost (CENPERM) Department of Geosciences and Natural Resource Management Copenhagen (IGN) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) United States Department of Energy (DOE) : ERKP757 2020-02-05 https://hal.inrae.fr/hal-03259447 https://hal.inrae.fr/hal-03259447/document https://hal.inrae.fr/hal-03259447/file/tc-14-445-2020.pdf https://doi.org/10.5194/tc-14-445-2020 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-14-445-2020 hal-03259447 https://hal.inrae.fr/hal-03259447 https://hal.inrae.fr/hal-03259447/document https://hal.inrae.fr/hal-03259447/file/tc-14-445-2020.pdf doi:10.5194/tc-14-445-2020 WOS: 000513000800001 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal.inrae.fr/hal-03259447 The Cryosphere, 2020, 14 (2), pp.445-459. ⟨10.5194/tc-14-445-2020⟩ Ice-wedge Degradation Land-surface Model Thermal Dynamics Polygonal Tundra Frozen Soil Carbon Water Co2 Fluxes System [SHS.GEO]Humanities and Social Sciences/Geography info:eu-repo/semantics/article Journal articles 2020 ftinsu https://doi.org/10.5194/tc-14-445-2020 2024-04-05T00:37:03Z International audience This study investigates and compares soil moisture and hydrology projections of broadly used land models with permafrost processes and highlights the causes and impacts of permafrost zone soil moisture projections. Climate models project warmer temperatures and increases in precipitation (P) which will intensify evapotranspiration (ET) and runoff in land models. However, this study shows that most models project a long-term drying of the surface soil (0-20 cm) for the permafrost region despite increases in the net air-surface water flux (P-ET). Drying is generally explained by infiltration of moisture to deeper soil layers as the active layer deepens or permafrost thaws completely. Although most models agree on drying, the projections vary strongly in magnitude and spatial pattern. Land models tend to agree with decadal runoff trends but underestimate runoff volume when compared to gauge data across the major Arctic river basins, potentially indicating model structural limitations. Coordinated efforts to address the ongoing challenges presented in this study will help reduce uncertainty in our capability to predict the future Arctic hydrological state and associated land-atmosphere biogeochemical processes across spatial and temporal scales. Article in Journal/Newspaper Ice permafrost The Cryosphere Tundra wedge* Institut national des sciences de l'Univers: HAL-INSU The Cryosphere 14 2 445 459 |