A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere
Abstract The current downturn of the arctic cryosphere, such as the strong loss of sea ice, melting of ice sheets and glaciers, and permafrost thaw, affects the marine and terrestrial carbon cycles in numerous interconnected ways. Nonetheless, processes in the ocean and on land have been too often c...
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ftnibiocom:oai:brage.bibsys.no:11250/2499733 2023-05-15T14:30:58+02:00 A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere Parmentier, Frans-Jan Christensen, Torben R. Rysgaard, Søren Bendtsen, Jørgen Glud, Ronnie N Brent, Else van Huissteden, Jacobus Sachs, Torsten Vonk, Jorien E. Sejr, Mikael K 2018-05-30T08:36:58Z http://hdl.handle.net/11250/2499733 https://doi.org/10.1007/s13280-016-0872-8 eng eng Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © The Author(s) 2017. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. CC-BY S53-S69 46 Ambio Sjøis Sea ice Global karbon syklus Global carbon cycle Permafrost Hav Oceans Arktis Arctic Journal article Peer reviewed 2018 ftnibiocom https://doi.org/10.1007/s13280-016-0872-8 2018-08-13T13:09:00Z Abstract The current downturn of the arctic cryosphere, such as the strong loss of sea ice, melting of ice sheets and glaciers, and permafrost thaw, affects the marine and terrestrial carbon cycles in numerous interconnected ways. Nonetheless, processes in the ocean and on land have been too often considered in isolation while it has become increasingly clear that the two environments are strongly connected: Sea ice decline is one of the main causes of the rapid warming of the Arctic, and the flow of carbon from rivers into the Arctic Ocean affects marine processes and the air–sea exchange of CO2. This review, therefore, provides an overview of the current state of knowledge of the arctic terrestrial and marine carbon cycle, connections in between, and how this complex system is affected by climate change and a declining cryosphere. Ultimately, better knowledge of biogeochemical processes combined with improved model representations of ocean–land interactions are essential to accurately predict the development of arctic ecosystems and associated climate feedbacks. publishedVersion Article in Journal/Newspaper arctic cryosphere Arctic Arctic Ocean Arktis Arktis* Climate change Ice permafrost Sea ice Norwegian Institute of Bioeconomy Research: NIBIO Brage Arctic Arctic Ocean Ambio 46 S1 53 69 |
institution |
Open Polar |
collection |
Norwegian Institute of Bioeconomy Research: NIBIO Brage |
op_collection_id |
ftnibiocom |
language |
English |
topic |
Sjøis Sea ice Global karbon syklus Global carbon cycle Permafrost Hav Oceans Arktis Arctic |
spellingShingle |
Sjøis Sea ice Global karbon syklus Global carbon cycle Permafrost Hav Oceans Arktis Arctic Parmentier, Frans-Jan Christensen, Torben R. Rysgaard, Søren Bendtsen, Jørgen Glud, Ronnie N Brent, Else van Huissteden, Jacobus Sachs, Torsten Vonk, Jorien E. Sejr, Mikael K A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
topic_facet |
Sjøis Sea ice Global karbon syklus Global carbon cycle Permafrost Hav Oceans Arktis Arctic |
description |
Abstract The current downturn of the arctic cryosphere, such as the strong loss of sea ice, melting of ice sheets and glaciers, and permafrost thaw, affects the marine and terrestrial carbon cycles in numerous interconnected ways. Nonetheless, processes in the ocean and on land have been too often considered in isolation while it has become increasingly clear that the two environments are strongly connected: Sea ice decline is one of the main causes of the rapid warming of the Arctic, and the flow of carbon from rivers into the Arctic Ocean affects marine processes and the air–sea exchange of CO2. This review, therefore, provides an overview of the current state of knowledge of the arctic terrestrial and marine carbon cycle, connections in between, and how this complex system is affected by climate change and a declining cryosphere. Ultimately, better knowledge of biogeochemical processes combined with improved model representations of ocean–land interactions are essential to accurately predict the development of arctic ecosystems and associated climate feedbacks. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Parmentier, Frans-Jan Christensen, Torben R. Rysgaard, Søren Bendtsen, Jørgen Glud, Ronnie N Brent, Else van Huissteden, Jacobus Sachs, Torsten Vonk, Jorien E. Sejr, Mikael K |
author_facet |
Parmentier, Frans-Jan Christensen, Torben R. Rysgaard, Søren Bendtsen, Jørgen Glud, Ronnie N Brent, Else van Huissteden, Jacobus Sachs, Torsten Vonk, Jorien E. Sejr, Mikael K |
author_sort |
Parmentier, Frans-Jan |
title |
A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
title_short |
A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
title_full |
A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
title_fullStr |
A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
title_full_unstemmed |
A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
title_sort |
synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere |
publishDate |
2018 |
url |
http://hdl.handle.net/11250/2499733 https://doi.org/10.1007/s13280-016-0872-8 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
arctic cryosphere Arctic Arctic Ocean Arktis Arktis* Climate change Ice permafrost Sea ice |
genre_facet |
arctic cryosphere Arctic Arctic Ocean Arktis Arktis* Climate change Ice permafrost Sea ice |
op_source |
S53-S69 46 Ambio |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © The Author(s) 2017. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s13280-016-0872-8 |
container_title |
Ambio |
container_volume |
46 |
container_issue |
S1 |
container_start_page |
53 |
op_container_end_page |
69 |
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1766304719383298048 |