Mueller, S. A.; Joos, F.; Plattner, G.-K.; Edwards, N. R. and Stocker, T. F.
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|DOI (Digital Object Identifier) Link:||http://doi.org/10.1029/2007GB003065|
|Google Scholar:||Look up in Google Scholar|
Observation-based surface ocean Δ14C 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 14C 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 14C 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 CO2 in seawater of 17.1 ± 3.3 cm/h-1, to find good agreement of simulated quantities with a range of data-based metrics.
|Item Type:||Journal Article|
|Copyright Holders:||2008 by the American Geophysical Union.|
|Keywords:||wind-speed; bomb radiocarbon; carbon-dioxide; global ocean; circulation; oxygen; paleoclimate; inventory; fluxes; budget|
|Academic Unit/Department:||Science > Environment, Earth and Ecosystems
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Neil Edwards|
|Date Deposited:||04 Jan 2011 10:45|
|Last Modified:||25 Feb 2016 05:48|
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Modelled natural and excess radiocarbon: Sensitivities to the gas exchange formulation and ocean transport strength. (deposited 04 Jan 2011 10:46)
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