Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength

Observation-based surface ocean Δ 14 C distributions and regional inventories for excess, bomb-produced radiocarbon are compared with results of two ocean models of intermediate complexity. By applying current descriptions of the air-sea gas exchange the models produce similar column inventories for...

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Published in:Global Biogeochemical Cycles
Main Authors: Mueller, S. A., Joos, F., Plattner, G.-K., Edwards, N. R., Stocker, T. F.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2008
Subjects:
Online Access:https://oro.open.ac.uk/25683/
https://oro.open.ac.uk/25683/1/mueller08gbc.pdf
http://www.agu.org/pubs/crossref/2008/2007GB003065.shtml
https://doi.org/10.1029/2007GB003065
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author Mueller, S. A.
Joos, F.
Plattner, G.-K.
Edwards, N. R.
Stocker, T. F.
author_facet Mueller, S. A.
Joos, F.
Plattner, G.-K.
Edwards, N. R.
Stocker, T. F.
author_sort Mueller, S. A.
collection The Open University: Open Research Online (ORO)
container_issue 3
container_start_page n/a
container_title Global Biogeochemical Cycles
container_volume 22
description Observation-based surface ocean Δ 14 C distributions and regional inventories for excess, bomb-produced radiocarbon are compared with results of two ocean models of intermediate complexity. By applying current descriptions of the air-sea gas exchange the models produce similar column inventories for excess 14 C among all basins. This result is robust across a wide range of transport parameter settings, but inconsistent with databased inventories. In the absence of evidence of fundamentally different gas exchange mechanisms in the North Atlantic than in the other basins, we infer regional North Atlantic 14 C inventories which are considerably smaller than previous estimates. The results further suggest that the gas exchange velocity field should be reduced by (19 ± 16)%, which corresponds to a global mean air-sea gas transfer rate for CO 2 in seawater of 17.1 ± 3.3 cm/h -1 , to find good agreement of simulated quantities with a range of data-based metrics.
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
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institution Open Polar
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op_doi https://doi.org/10.1029/2007GB003065
op_relation https://oro.open.ac.uk/25683/1/mueller08gbc.pdf
Mueller, S. A.; Joos, F.; Plattner, G.-K.; Edwards, N. R. <http://oro.open.ac.uk/view/person/nre29.html> and Stocker, T. F. (2008). Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength. Global Biogeochemical Cycles, 22(GB3011) pp. 1–14.
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spelling ftopenunivgb:oai:oro.open.ac.uk:25683 2025-01-16T23:34:41+00:00 Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength Mueller, S. A. Joos, F. Plattner, G.-K. Edwards, N. R. Stocker, T. F. 2008-08 application/pdf https://oro.open.ac.uk/25683/ https://oro.open.ac.uk/25683/1/mueller08gbc.pdf http://www.agu.org/pubs/crossref/2008/2007GB003065.shtml https://doi.org/10.1029/2007GB003065 unknown https://oro.open.ac.uk/25683/1/mueller08gbc.pdf Mueller, S. A.; Joos, F.; Plattner, G.-K.; Edwards, N. R. <http://oro.open.ac.uk/view/person/nre29.html> and Stocker, T. F. (2008). Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength. Global Biogeochemical Cycles, 22(GB3011) pp. 1–14. Journal Item Public PeerReviewed 2008 ftopenunivgb https://doi.org/10.1029/2007GB003065 2023-05-28T05:45:25Z Observation-based surface ocean Δ 14 C distributions and regional inventories for excess, bomb-produced radiocarbon are compared with results of two ocean models of intermediate complexity. By applying current descriptions of the air-sea gas exchange the models produce similar column inventories for excess 14 C among all basins. This result is robust across a wide range of transport parameter settings, but inconsistent with databased inventories. In the absence of evidence of fundamentally different gas exchange mechanisms in the North Atlantic than in the other basins, we infer regional North Atlantic 14 C inventories which are considerably smaller than previous estimates. The results further suggest that the gas exchange velocity field should be reduced by (19 ± 16)%, which corresponds to a global mean air-sea gas transfer rate for CO 2 in seawater of 17.1 ± 3.3 cm/h -1 , to find good agreement of simulated quantities with a range of data-based metrics. Article in Journal/Newspaper North Atlantic The Open University: Open Research Online (ORO) Global Biogeochemical Cycles 22 3 n/a n/a
spellingShingle Mueller, S. A.
Joos, F.
Plattner, G.-K.
Edwards, N. R.
Stocker, T. F.
Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength
title Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength
title_full Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength
title_fullStr Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength
title_full_unstemmed Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength
title_short Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength
title_sort modelled natural and excess radiocarbon: sensitivities to the gas exchange formulation and ocean transport strength
url https://oro.open.ac.uk/25683/
https://oro.open.ac.uk/25683/1/mueller08gbc.pdf
http://www.agu.org/pubs/crossref/2008/2007GB003065.shtml
https://doi.org/10.1029/2007GB003065