Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change

We conducted a model-based assessment of changes in permafrost area and carbon storage for simulations driven by RCP4.5 and RCP8.5 projections between 2010 and 2299 for the northern permafrost region. All models simulating carbon represented soil with depth, a critical structural feature needed to r...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: McGuire,A.D., Lawrence, D.M., Koven, C., Clein, J.S., Burke, E., Chen, G., Jafarov, E., MacDougall, A.H., Marchenko, S., Nicolsky, D., Peng, S., Rinke, A., Ciais, P., Gouttevin, I., Hayes, D.J., Ji, D., Krinner, G., Moore, J.C., Romanovsky, V., Schadel, C., Schaefer, K., Schuur, E.A.G., Zhuang, Q.
Other Authors: USGS ALASKA COOPERATIVE FISH AND WILDLIFE RESEARCH UNIT UNIVERSITY OF ALASKA FAIRBANKS USA, CLIMATE AND GLOBAL DYNAMICS LABORATORY NATIONAL CENTER FOR ATMOSPHERIC RESEARCH BOULDER USA, CLIMATE AND ECOSYSTEM SCIENCES DIVISION LAWRENCE BERKELEY NATIONAL LABORATORY USA, INSTITUTE OF ARCTIC BIOLOGY UNIVERSITY OF ALASKA FAIRBANKS USA, MET OFFICE HADLEY CENTRE EXETER GBR, ENVIRONMENTAL SCIENCES DIVISION OAK RIDGE NATIONAL LABORATORY OAK RIDGE USA, EARTH AND ENVIRONMENTAL SCIENCES DIVISION LOS ALAMOS NATIONAL LABORATORY LOS ALAMOS USA, DEPARTMENT OF EARTH SCIENCES ST FRANCIS XAVIER UNIVERSITY ANTIGONISH CAN, GEOPHYSICAL INSTITUTE UNIVERSITY OF ALASKA FAIRBANKS USA, LABORATOIRE DES SCIENCES DU CLIMAT ET DE L'ENVIRONNEMENT COMMISSARIAT A L'ENERGIE ATOMIQUE CNRS UNIVERSITE DE VERSAILLES SAINT QUENTIN EN YVELINES UMR8212 GIF SUR YVETTE FRA, ALFRED WEGENER INSTITUTE HELMHOLTZ CENTRE FOR POLAR AND MARINE RESEARCH POTSDAM DEU, INSTITUT DES GEOSCIENCES DE L'ENVIRONMENT UNIVERSITE GRENOBLE ALPES CNRS GRENOBLE FRA, COLLEGE OF GLOBAL CHANGE AND EARTH SYSTEM SCIENCE BEIJING NORMAL UNIVERSITY BEIJING CHN, CENTER FOR ECOSYSTEM SCIENCE AND SOCIETY NORTHERN ARIZONA UNIVERSITY FLAGSTAFF USA, NATIONAL SNOW AND ICE DATA CENTER UNIVERSITY OF COLORADO BOULDER USA, DEPARTMENT OF EARTH ATMOSPHERIC AND PLANETARY SCIENCES PURDUE UNIVERSITY WEST LAFAYETTE USA
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://irsteadoc.irstea.fr/cemoa/PUB00060051
id ftcemoa:oai:irsteadoc.irstea.fr:PUB00060051
record_format openpolar
institution Open Polar
collection Irstea Publications et Bases documentaires (Irstea@doc/CemOA)
op_collection_id ftcemoa
language English
topic CARBONE
NEIGE
CHANGEMENT CLIMATIQUE
carbon
snow
climatic change
spellingShingle CARBONE
NEIGE
CHANGEMENT CLIMATIQUE
carbon
snow
climatic change
McGuire,A.D.
Lawrence, D.M.
Koven, C.
Clein, J.S.
Burke, E.
Chen, G.
Jafarov, E.
MacDougall, A.H.
Marchenko, S.
Nicolsky, D.
Peng, S.
Rinke, A.
Ciais, P.
Gouttevin, I.
Hayes, D.J.
Ji, D.
Krinner, G.
Moore, J.C.
Romanovsky, V.
Schadel, C.
Schaefer, K.
Schuur, E.A.G.
Zhuang, Q.
Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
topic_facet CARBONE
NEIGE
CHANGEMENT CLIMATIQUE
carbon
snow
climatic change
description We conducted a model-based assessment of changes in permafrost area and carbon storage for simulations driven by RCP4.5 and RCP8.5 projections between 2010 and 2299 for the northern permafrost region. All models simulating carbon represented soil with depth, a critical structural feature needed to represent the permafrost carbon-climate feedback, but that is not a universal feature of all climate models. Between 2010 and 2299, simulations indicated losses of permafrost between 3 and 5 million km2 for the RCP4.5 climate and between 6 and 16 million km2 for the RCP8.5 climate. For the RCP4.5 projection, cumulative change in soil carbon varied between 66-Pg C (1015-g carbon) loss to 70-Pg C gain. For the RCP8.5 projection, losses in soil carbon varied between 74 and 652 Pg C (mean loss, 341 Pg C). For the RCP4.5 projection, gains in vegetation carbon were largely responsible for the overall projected net gains in ecosystem carbon by 2299 (8- to 244-Pg C gains). In contrast, for the RCP8.5 projection, gains in vegetation carbon were not great enough to compensate for the losses of carbon projected by four of the five models; changes in ecosystem carbon ranged from a 641-Pg C loss to a 167-Pg C gain (mean, 208-Pg C loss). The models indicate that substantial net losses of ecosystem carbon would not occur until after 2100. This assessment suggests that effective mitigation efforts during the remainder of this century could attenuate the negative consequences of the permafrost carbon-climate feedback.
author2 USGS ALASKA COOPERATIVE FISH AND WILDLIFE RESEARCH UNIT UNIVERSITY OF ALASKA FAIRBANKS USA
CLIMATE AND GLOBAL DYNAMICS LABORATORY NATIONAL CENTER FOR ATMOSPHERIC RESEARCH BOULDER USA
CLIMATE AND ECOSYSTEM SCIENCES DIVISION LAWRENCE BERKELEY NATIONAL LABORATORY USA
INSTITUTE OF ARCTIC BIOLOGY UNIVERSITY OF ALASKA FAIRBANKS USA
MET OFFICE HADLEY CENTRE EXETER GBR
ENVIRONMENTAL SCIENCES DIVISION OAK RIDGE NATIONAL LABORATORY OAK RIDGE USA
EARTH AND ENVIRONMENTAL SCIENCES DIVISION LOS ALAMOS NATIONAL LABORATORY LOS ALAMOS USA
DEPARTMENT OF EARTH SCIENCES ST FRANCIS XAVIER UNIVERSITY ANTIGONISH CAN
GEOPHYSICAL INSTITUTE UNIVERSITY OF ALASKA FAIRBANKS USA
LABORATOIRE DES SCIENCES DU CLIMAT ET DE L'ENVIRONNEMENT COMMISSARIAT A L'ENERGIE ATOMIQUE CNRS UNIVERSITE DE VERSAILLES SAINT QUENTIN EN YVELINES UMR8212 GIF SUR YVETTE FRA
ALFRED WEGENER INSTITUTE HELMHOLTZ CENTRE FOR POLAR AND MARINE RESEARCH POTSDAM DEU
INSTITUT DES GEOSCIENCES DE L'ENVIRONMENT UNIVERSITE GRENOBLE ALPES CNRS GRENOBLE FRA
COLLEGE OF GLOBAL CHANGE AND EARTH SYSTEM SCIENCE BEIJING NORMAL UNIVERSITY BEIJING CHN
CENTER FOR ECOSYSTEM SCIENCE AND SOCIETY NORTHERN ARIZONA UNIVERSITY FLAGSTAFF USA
NATIONAL SNOW AND ICE DATA CENTER UNIVERSITY OF COLORADO BOULDER USA
DEPARTMENT OF EARTH ATMOSPHERIC AND PLANETARY SCIENCES PURDUE UNIVERSITY WEST LAFAYETTE USA
format Article in Journal/Newspaper
author McGuire,A.D.
Lawrence, D.M.
Koven, C.
Clein, J.S.
Burke, E.
Chen, G.
Jafarov, E.
MacDougall, A.H.
Marchenko, S.
Nicolsky, D.
Peng, S.
Rinke, A.
Ciais, P.
Gouttevin, I.
Hayes, D.J.
Ji, D.
Krinner, G.
Moore, J.C.
Romanovsky, V.
Schadel, C.
Schaefer, K.
Schuur, E.A.G.
Zhuang, Q.
author_facet McGuire,A.D.
Lawrence, D.M.
Koven, C.
Clein, J.S.
Burke, E.
Chen, G.
Jafarov, E.
MacDougall, A.H.
Marchenko, S.
Nicolsky, D.
Peng, S.
Rinke, A.
Ciais, P.
Gouttevin, I.
Hayes, D.J.
Ji, D.
Krinner, G.
Moore, J.C.
Romanovsky, V.
Schadel, C.
Schaefer, K.
Schuur, E.A.G.
Zhuang, Q.
author_sort McGuire,A.D.
title Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
title_short Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
title_full Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
title_fullStr Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
title_full_unstemmed Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
title_sort dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change
publishDate 2018
url https://irsteadoc.irstea.fr/cemoa/PUB00060051
genre permafrost
genre_facet permafrost
op_source 52838
op_relation http://dx.doi.org/10.1073/pnas.1719903115
https://irsteadoc.irstea.fr/cemoa/PUB00060051
op_rights Date de dépôt: 2019-01-30 - Tous les documents et informations contenus dans la base CemOA Publications sont protégés en vertu du droit de propriété intellectuelle, en particulier par le droit d'auteur. La personne consultant la base CemOA Publications peut visualiser, reproduire, ou stocker des copies des publications, à condition que l'information soit seulement pour son usage personnel et non commercial. L'utilisation des travaux universitaires est soumise à autorisation préalable de leurs auteurs. Toute information relative au signalement d'une publication contenue dans CemOA Publications doit inclure la citation bibliographique usuelle : Nom du ou des auteurs, titre et source du document, date et URL de la notice (dc_identifier).
op_doi https://doi.org/10.1073/pnas.1719903115
container_title Proceedings of the National Academy of Sciences
container_volume 115
container_issue 15
container_start_page 3882
op_container_end_page 3887
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spelling ftcemoa:oai:irsteadoc.irstea.fr:PUB00060051 2023-05-15T17:56:12+02:00 Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change McGuire,A.D. Lawrence, D.M. Koven, C. Clein, J.S. Burke, E. Chen, G. Jafarov, E. MacDougall, A.H. Marchenko, S. Nicolsky, D. Peng, S. Rinke, A. Ciais, P. Gouttevin, I. Hayes, D.J. Ji, D. Krinner, G. Moore, J.C. Romanovsky, V. Schadel, C. Schaefer, K. Schuur, E.A.G. Zhuang, Q. USGS ALASKA COOPERATIVE FISH AND WILDLIFE RESEARCH UNIT UNIVERSITY OF ALASKA FAIRBANKS USA CLIMATE AND GLOBAL DYNAMICS LABORATORY NATIONAL CENTER FOR ATMOSPHERIC RESEARCH BOULDER USA CLIMATE AND ECOSYSTEM SCIENCES DIVISION LAWRENCE BERKELEY NATIONAL LABORATORY USA INSTITUTE OF ARCTIC BIOLOGY UNIVERSITY OF ALASKA FAIRBANKS USA MET OFFICE HADLEY CENTRE EXETER GBR ENVIRONMENTAL SCIENCES DIVISION OAK RIDGE NATIONAL LABORATORY OAK RIDGE USA EARTH AND ENVIRONMENTAL SCIENCES DIVISION LOS ALAMOS NATIONAL LABORATORY LOS ALAMOS USA DEPARTMENT OF EARTH SCIENCES ST FRANCIS XAVIER UNIVERSITY ANTIGONISH CAN GEOPHYSICAL INSTITUTE UNIVERSITY OF ALASKA FAIRBANKS USA LABORATOIRE DES SCIENCES DU CLIMAT ET DE L'ENVIRONNEMENT COMMISSARIAT A L'ENERGIE ATOMIQUE CNRS UNIVERSITE DE VERSAILLES SAINT QUENTIN EN YVELINES UMR8212 GIF SUR YVETTE FRA ALFRED WEGENER INSTITUTE HELMHOLTZ CENTRE FOR POLAR AND MARINE RESEARCH POTSDAM DEU INSTITUT DES GEOSCIENCES DE L'ENVIRONMENT UNIVERSITE GRENOBLE ALPES CNRS GRENOBLE FRA COLLEGE OF GLOBAL CHANGE AND EARTH SYSTEM SCIENCE BEIJING NORMAL UNIVERSITY BEIJING CHN CENTER FOR ECOSYSTEM SCIENCE AND SOCIETY NORTHERN ARIZONA UNIVERSITY FLAGSTAFF USA NATIONAL SNOW AND ICE DATA CENTER UNIVERSITY OF COLORADO BOULDER USA DEPARTMENT OF EARTH ATMOSPHERIC AND PLANETARY SCIENCES PURDUE UNIVERSITY WEST LAFAYETTE USA 2018 application/pdf https://irsteadoc.irstea.fr/cemoa/PUB00060051 Anglais eng http://dx.doi.org/10.1073/pnas.1719903115 https://irsteadoc.irstea.fr/cemoa/PUB00060051 Date de dépôt: 2019-01-30 - Tous les documents et informations contenus dans la base CemOA Publications sont protégés en vertu du droit de propriété intellectuelle, en particulier par le droit d'auteur. La personne consultant la base CemOA Publications peut visualiser, reproduire, ou stocker des copies des publications, à condition que l'information soit seulement pour son usage personnel et non commercial. L'utilisation des travaux universitaires est soumise à autorisation préalable de leurs auteurs. Toute information relative au signalement d'une publication contenue dans CemOA Publications doit inclure la citation bibliographique usuelle : Nom du ou des auteurs, titre et source du document, date et URL de la notice (dc_identifier). 52838 CARBONE NEIGE CHANGEMENT CLIMATIQUE carbon snow climatic change Article de revue scientifique à comité de lecture 2018 ftcemoa https://doi.org/10.1073/pnas.1719903115 2021-06-29T12:24:45Z We conducted a model-based assessment of changes in permafrost area and carbon storage for simulations driven by RCP4.5 and RCP8.5 projections between 2010 and 2299 for the northern permafrost region. All models simulating carbon represented soil with depth, a critical structural feature needed to represent the permafrost carbon-climate feedback, but that is not a universal feature of all climate models. Between 2010 and 2299, simulations indicated losses of permafrost between 3 and 5 million km2 for the RCP4.5 climate and between 6 and 16 million km2 for the RCP8.5 climate. For the RCP4.5 projection, cumulative change in soil carbon varied between 66-Pg C (1015-g carbon) loss to 70-Pg C gain. For the RCP8.5 projection, losses in soil carbon varied between 74 and 652 Pg C (mean loss, 341 Pg C). For the RCP4.5 projection, gains in vegetation carbon were largely responsible for the overall projected net gains in ecosystem carbon by 2299 (8- to 244-Pg C gains). In contrast, for the RCP8.5 projection, gains in vegetation carbon were not great enough to compensate for the losses of carbon projected by four of the five models; changes in ecosystem carbon ranged from a 641-Pg C loss to a 167-Pg C gain (mean, 208-Pg C loss). The models indicate that substantial net losses of ecosystem carbon would not occur until after 2100. This assessment suggests that effective mitigation efforts during the remainder of this century could attenuate the negative consequences of the permafrost carbon-climate feedback. Article in Journal/Newspaper permafrost Irstea Publications et Bases documentaires (Irstea@doc/CemOA) Proceedings of the National Academy of Sciences 115 15 3882 3887