ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol
International audience Few Earth system models adequately represent the unique permafrost soil biogeochemistry and its respective processes; this significantly contributes to uncertainty in estimating their responses, and that of the planet at large, to warming. Likewise, the riverine component of w...
Published in: | Geoscientific Model Development |
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Main Authors: | , , , , , , , |
Other Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2019
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Subjects: | |
Online Access: | https://hal.sorbonne-universite.fr/hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177/document https://hal.sorbonne-universite.fr/hal-02276177/file/gmd-12-3503-2019.pdf https://doi.org/10.5194/gmd-12-3503-2019 |
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Open Polar |
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Université de Nantes: HAL-UNIV-NANTES |
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ftunivnantes |
language |
English |
topic |
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
spellingShingle |
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Bowring, Simon, Lauerwald, Ronny Guenet, Bertrand Zhu, Dan Guimberteau, Matthieu Tootchi, Ardalan Ducharne, Agnès Ciais, Philippe ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol |
topic_facet |
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
International audience Few Earth system models adequately represent the unique permafrost soil biogeochemistry and its respective processes; this significantly contributes to uncertainty in estimating their responses, and that of the planet at large, to warming. Likewise, the riverine component of what is known as the "boundless carbon cycle" is seldom recognised in Earth system modelling. The hydrological mobilisation of organic material from a ∼ 1330-1580 PgC carbon stock to the river network results in either sedimentary settling or atmospheric "evasion", processes widely expected to increase with amplified Arctic climate warming. Here, the production , transport, and atmospheric release of dissolved organic carbon (DOC) from high-latitude permafrost soils into inland waters and the ocean are explicitly represented for the first time in the land surface component (ORCHIDEE) of a CMIP6 global climate model (Institut Pierre Simon Laplace-IPSL). The model, ORCHIDEE MICT-LEAK, which represents the merger of previously described ORCHIDEE versions MICT and LEAK, mechanistically represents (a) vegetation and soil physical processes for high-latitude snow, ice, and soil phenomena and (b) the cycling of DOC and CO 2 , including atmospheric evasion, along the terrestrial-aquatic continuum from soils through the river network to the coast at 0.5 to 2° resolution. This paper, the first in a two-part study, presents the rationale for including these processes in a high-latitude-specific land surface model, then describes the model with a focus on novel process implementations, followed by a summary of the model configuration and simulation protocol. The results of these simulation runs, conducted for the Lena River basin, are evaluated against observational data in the second part of this study. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Université libre de Bruxelles (ULB) Milieux Environnementaux, Transferts et Interactions dans les hydrosystèmes et les Sols (METIS) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) ICOS-ATC (ICOS-ATC) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Bowring, Simon, Lauerwald, Ronny Guenet, Bertrand Zhu, Dan Guimberteau, Matthieu Tootchi, Ardalan Ducharne, Agnès Ciais, Philippe |
author_facet |
Bowring, Simon, Lauerwald, Ronny Guenet, Bertrand Zhu, Dan Guimberteau, Matthieu Tootchi, Ardalan Ducharne, Agnès Ciais, Philippe |
author_sort |
Bowring, Simon, |
title |
ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol |
title_short |
ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol |
title_full |
ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol |
title_fullStr |
ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol |
title_full_unstemmed |
ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol |
title_sort |
orchidee mict-leak (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from arctic permafrost regions – part 1: rationale, model description, and simulation protocol |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.sorbonne-universite.fr/hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177/document https://hal.sorbonne-universite.fr/hal-02276177/file/gmd-12-3503-2019.pdf https://doi.org/10.5194/gmd-12-3503-2019 |
long_lat |
ENVELOPE(141.467,141.467,-66.782,-66.782) |
geographic |
Arctic Laplace |
geographic_facet |
Arctic Laplace |
genre |
Arctic Ice lena river permafrost |
genre_facet |
Arctic Ice lena river permafrost |
op_source |
ISSN: 1991-9603 EISSN: 1991-959X Geoscientific Model Development https://hal.sorbonne-universite.fr/hal-02276177 Geoscientific Model Development, 2019, 12 (8), pp.3503-3521. ⟨10.5194/gmd-12-3503-2019⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/gmd-12-3503-2019 hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177/document https://hal.sorbonne-universite.fr/hal-02276177/file/gmd-12-3503-2019.pdf doi:10.5194/gmd-12-3503-2019 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/gmd-12-3503-2019 |
container_title |
Geoscientific Model Development |
container_volume |
12 |
container_issue |
8 |
container_start_page |
3503 |
op_container_end_page |
3521 |
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1766333796276240384 |
spelling |
ftunivnantes:oai:HAL:hal-02276177v1 2023-05-15T15:01:47+02:00 ORCHIDEE MICT-LEAK (r5459), a global model for the production, transport, and transformation of dissolved organic carbon from Arctic permafrost regions – Part 1: Rationale, model description, and simulation protocol Bowring, Simon, Lauerwald, Ronny Guenet, Bertrand Zhu, Dan Guimberteau, Matthieu Tootchi, Ardalan Ducharne, Agnès Ciais, Philippe Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Université libre de Bruxelles (ULB) Milieux Environnementaux, Transferts et Interactions dans les hydrosystèmes et les Sols (METIS) École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) ICOS-ATC (ICOS-ATC) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) 2019 https://hal.sorbonne-universite.fr/hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177/document https://hal.sorbonne-universite.fr/hal-02276177/file/gmd-12-3503-2019.pdf https://doi.org/10.5194/gmd-12-3503-2019 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/gmd-12-3503-2019 hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177 https://hal.sorbonne-universite.fr/hal-02276177/document https://hal.sorbonne-universite.fr/hal-02276177/file/gmd-12-3503-2019.pdf doi:10.5194/gmd-12-3503-2019 info:eu-repo/semantics/OpenAccess ISSN: 1991-9603 EISSN: 1991-959X Geoscientific Model Development https://hal.sorbonne-universite.fr/hal-02276177 Geoscientific Model Development, 2019, 12 (8), pp.3503-3521. ⟨10.5194/gmd-12-3503-2019⟩ [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2019 ftunivnantes https://doi.org/10.5194/gmd-12-3503-2019 2023-01-18T00:54:26Z International audience Few Earth system models adequately represent the unique permafrost soil biogeochemistry and its respective processes; this significantly contributes to uncertainty in estimating their responses, and that of the planet at large, to warming. Likewise, the riverine component of what is known as the "boundless carbon cycle" is seldom recognised in Earth system modelling. The hydrological mobilisation of organic material from a ∼ 1330-1580 PgC carbon stock to the river network results in either sedimentary settling or atmospheric "evasion", processes widely expected to increase with amplified Arctic climate warming. Here, the production , transport, and atmospheric release of dissolved organic carbon (DOC) from high-latitude permafrost soils into inland waters and the ocean are explicitly represented for the first time in the land surface component (ORCHIDEE) of a CMIP6 global climate model (Institut Pierre Simon Laplace-IPSL). The model, ORCHIDEE MICT-LEAK, which represents the merger of previously described ORCHIDEE versions MICT and LEAK, mechanistically represents (a) vegetation and soil physical processes for high-latitude snow, ice, and soil phenomena and (b) the cycling of DOC and CO 2 , including atmospheric evasion, along the terrestrial-aquatic continuum from soils through the river network to the coast at 0.5 to 2° resolution. This paper, the first in a two-part study, presents the rationale for including these processes in a high-latitude-specific land surface model, then describes the model with a focus on novel process implementations, followed by a summary of the model configuration and simulation protocol. The results of these simulation runs, conducted for the Lena River basin, are evaluated against observational data in the second part of this study. Article in Journal/Newspaper Arctic Ice lena river permafrost Université de Nantes: HAL-UNIV-NANTES Arctic Laplace ENVELOPE(141.467,141.467,-66.782,-66.782) Geoscientific Model Development 12 8 3503 3521 |