Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales
Ocean-sediment and weathering interactions exert the primary control on how much anthropogenic-emitted CO2 remains in the atmosphere on timescales longer than about 1 kyr. Analytical theory is presented which predicts, from initial conditions, the remaining atmospheric fraction of emitted CO2 after...
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Online Access: | http://eprints.esc.cam.ac.uk/2302/ http://eprints.esc.cam.ac.uk/2302/1/Goodwin_07_2008GB003449.pdf https://doi.org/10.1029/2008GB003449 |
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:2302 2023-05-15T15:52:50+02:00 Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales Goodwin, P. Ridgewell, A. 2010-05 application/pdf http://eprints.esc.cam.ac.uk/2302/ http://eprints.esc.cam.ac.uk/2302/1/Goodwin_07_2008GB003449.pdf https://doi.org/10.1029/2008GB003449 en eng http://eprints.esc.cam.ac.uk/2302/1/Goodwin_07_2008GB003449.pdf Goodwin, P. and Ridgewell, A. (2010) Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales. Global Biogeochemical Cycles, 24. GB2014. DOI https://doi.org/10.1029/2008GB003449 <https://doi.org/10.1029/2008GB003449> 01 - Climate Change and Earth-Ocean Atmosphere Systems Article PeerReviewed 2010 ftucambridgeesc https://doi.org/10.1029/2008GB003449 2020-08-27T18:09:13Z Ocean-sediment and weathering interactions exert the primary control on how much anthropogenic-emitted CO2 remains in the atmosphere on timescales longer than about 1 kyr. Analytical theory is presented which predicts, from initial conditions, the remaining atmospheric fraction of emitted CO2 after equilibrium with CaCO3 burial in deep-sea sediments but before silicate weathering removes all excess CO2 on a >100 kyr timescale. The theoretical predictions of final atmospheric CO2 partial pressure are tested against independent integrations of the GENIE-1 Earth system model and are found to agree to within 10% for total emissions up to about 4000 PgC. The predicted theoretical relationship is linear and is based on the assumptions that ocean carbonate ion concentration is restored when CaCO3 burial reaches a new steady state, and that the steady state change in global ocean CO2* is proportional to the change in atmospheric CO2; where CO2* is the combined concentration of aqueous CO2 and carbonic acid. We find that the residual fraction of anthropogenic CO2 in the atmosphere can be determined without explicit use of ocean [CO32−], even though this concentration is known to be important in controlling the depth interval over which CaCO3-rich sediments accumulate. The simple theory developed here is particularly suited for efficient assessment of events recorded in the geological record as well as anthropogenic CO2 influences on the long-term stability of ice sheets. Article in Journal/Newspaper Carbonic acid University of Cambridge, Department of Earth Sciences: ESC Publications Global Biogeochemical Cycles 24 2 n/a n/a |
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Open Polar |
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University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
spellingShingle |
01 - Climate Change and Earth-Ocean Atmosphere Systems Goodwin, P. Ridgewell, A. Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
topic_facet |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
description |
Ocean-sediment and weathering interactions exert the primary control on how much anthropogenic-emitted CO2 remains in the atmosphere on timescales longer than about 1 kyr. Analytical theory is presented which predicts, from initial conditions, the remaining atmospheric fraction of emitted CO2 after equilibrium with CaCO3 burial in deep-sea sediments but before silicate weathering removes all excess CO2 on a >100 kyr timescale. The theoretical predictions of final atmospheric CO2 partial pressure are tested against independent integrations of the GENIE-1 Earth system model and are found to agree to within 10% for total emissions up to about 4000 PgC. The predicted theoretical relationship is linear and is based on the assumptions that ocean carbonate ion concentration is restored when CaCO3 burial reaches a new steady state, and that the steady state change in global ocean CO2* is proportional to the change in atmospheric CO2; where CO2* is the combined concentration of aqueous CO2 and carbonic acid. We find that the residual fraction of anthropogenic CO2 in the atmosphere can be determined without explicit use of ocean [CO32−], even though this concentration is known to be important in controlling the depth interval over which CaCO3-rich sediments accumulate. The simple theory developed here is particularly suited for efficient assessment of events recorded in the geological record as well as anthropogenic CO2 influences on the long-term stability of ice sheets. |
format |
Article in Journal/Newspaper |
author |
Goodwin, P. Ridgewell, A. |
author_facet |
Goodwin, P. Ridgewell, A. |
author_sort |
Goodwin, P. |
title |
Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
title_short |
Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
title_full |
Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
title_fullStr |
Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
title_full_unstemmed |
Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
title_sort |
ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales |
publishDate |
2010 |
url |
http://eprints.esc.cam.ac.uk/2302/ http://eprints.esc.cam.ac.uk/2302/1/Goodwin_07_2008GB003449.pdf https://doi.org/10.1029/2008GB003449 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_relation |
http://eprints.esc.cam.ac.uk/2302/1/Goodwin_07_2008GB003449.pdf Goodwin, P. and Ridgewell, A. (2010) Ocean-atmosphere partitioning of anthropogenic carbon dioxide on multimillennial timescales. Global Biogeochemical Cycles, 24. GB2014. DOI https://doi.org/10.1029/2008GB003449 <https://doi.org/10.1029/2008GB003449> |
op_doi |
https://doi.org/10.1029/2008GB003449 |
container_title |
Global Biogeochemical Cycles |
container_volume |
24 |
container_issue |
2 |
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n/a |
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n/a |
_version_ |
1766387951014510592 |