Indirect relationship between surface water budget and wetland extent
International audience We used a suite of two models: a global climate model, and a hydrological routing scheme, to estimate the changes in the surface water budget and extent of natural wetlands, at the last interglacial (126000 years ago) and at the last glacial maximum (21000 years ago). At both...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , |
Other Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2002
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Online Access: | https://hal.science/hal-03126828 https://hal.science/hal-03126828/document https://hal.science/hal-03126828/file/2001GL013929.pdf https://doi.org/10.1029/2001GL013929 |
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ftunigrenoble:oai:HAL:hal-03126828v1 |
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openpolar |
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Open Polar |
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Université Grenoble Alpes: HAL |
op_collection_id |
ftunigrenoble |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment de Noblet-Ducoudré, Nathalie Poutou, Estelle Chappellaz, Jérôme, J Coe, Michael Krinner, Gerhard Indirect relationship between surface water budget and wetland extent |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience We used a suite of two models: a global climate model, and a hydrological routing scheme, to estimate the changes in the surface water budget and extent of natural wetlands, at the last interglacial (126000 years ago) and at the last glacial maximum (21000 years ago). At both time periods, in northern tropical Africa as well as in northern South America, our simulations exhibit, in many places, an indirect relationship between the surface water budget and the extent of natural wetlands. In relatively moist regions, decreasing (increasing) rainfall and runoff at the last glacial maximum (last interglacial) result in increased (decreased) wetland area due to the reduction (increase) in lake depth. This counter‐intuitive result has never been hypothesized before and may shed a new light on the interpretation of past changes in atmospheric methane, as derived from ice core analyses. It also points to the importance of using a bottom‐up modelling approach in this field of study. |
author2 |
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) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) 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)) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-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 Joseph Fourier - Grenoble 1 (UJF)-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)-Centre National de la Recherche Scientifique (CNRS) Center for Sustainability and the Global Environment (SAGE) Nelson Institute for Environmental Studies University of Wisconsin-Madison-University of Wisconsin-Madison |
format |
Article in Journal/Newspaper |
author |
de Noblet-Ducoudré, Nathalie Poutou, Estelle Chappellaz, Jérôme, J Coe, Michael Krinner, Gerhard |
author_facet |
de Noblet-Ducoudré, Nathalie Poutou, Estelle Chappellaz, Jérôme, J Coe, Michael Krinner, Gerhard |
author_sort |
de Noblet-Ducoudré, Nathalie |
title |
Indirect relationship between surface water budget and wetland extent |
title_short |
Indirect relationship between surface water budget and wetland extent |
title_full |
Indirect relationship between surface water budget and wetland extent |
title_fullStr |
Indirect relationship between surface water budget and wetland extent |
title_full_unstemmed |
Indirect relationship between surface water budget and wetland extent |
title_sort |
indirect relationship between surface water budget and wetland extent |
publisher |
HAL CCSD |
publishDate |
2002 |
url |
https://hal.science/hal-03126828 https://hal.science/hal-03126828/document https://hal.science/hal-03126828/file/2001GL013929.pdf https://doi.org/10.1029/2001GL013929 |
genre |
ice core |
genre_facet |
ice core |
op_source |
ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-03126828 Geophysical Research Letters, 2002, 29 (4), ⟨10.1029/2001GL013929⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2001GL013929 hal-03126828 https://hal.science/hal-03126828 https://hal.science/hal-03126828/document https://hal.science/hal-03126828/file/2001GL013929.pdf doi:10.1029/2001GL013929 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2001GL013929 |
container_title |
Geophysical Research Letters |
container_volume |
29 |
container_issue |
4 |
_version_ |
1798847472572825600 |
spelling |
ftunigrenoble:oai:HAL:hal-03126828v1 2024-05-12T08:05:12+00:00 Indirect relationship between surface water budget and wetland extent de Noblet-Ducoudré, Nathalie Poutou, Estelle Chappellaz, Jérôme, J Coe, Michael Krinner, Gerhard 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) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) 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)) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-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 Joseph Fourier - Grenoble 1 (UJF)-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)-Centre National de la Recherche Scientifique (CNRS) Center for Sustainability and the Global Environment (SAGE) Nelson Institute for Environmental Studies University of Wisconsin-Madison-University of Wisconsin-Madison 2002 https://hal.science/hal-03126828 https://hal.science/hal-03126828/document https://hal.science/hal-03126828/file/2001GL013929.pdf https://doi.org/10.1029/2001GL013929 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2001GL013929 hal-03126828 https://hal.science/hal-03126828 https://hal.science/hal-03126828/document https://hal.science/hal-03126828/file/2001GL013929.pdf doi:10.1029/2001GL013929 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-03126828 Geophysical Research Letters, 2002, 29 (4), ⟨10.1029/2001GL013929⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2002 ftunigrenoble https://doi.org/10.1029/2001GL013929 2024-04-18T03:22:40Z International audience We used a suite of two models: a global climate model, and a hydrological routing scheme, to estimate the changes in the surface water budget and extent of natural wetlands, at the last interglacial (126000 years ago) and at the last glacial maximum (21000 years ago). At both time periods, in northern tropical Africa as well as in northern South America, our simulations exhibit, in many places, an indirect relationship between the surface water budget and the extent of natural wetlands. In relatively moist regions, decreasing (increasing) rainfall and runoff at the last glacial maximum (last interglacial) result in increased (decreased) wetland area due to the reduction (increase) in lake depth. This counter‐intuitive result has never been hypothesized before and may shed a new light on the interpretation of past changes in atmospheric methane, as derived from ice core analyses. It also points to the importance of using a bottom‐up modelling approach in this field of study. Article in Journal/Newspaper ice core Université Grenoble Alpes: HAL Geophysical Research Letters 29 4 |