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U.S. Department of Energy
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Oceanic CO sub 2 uptake and future atmospheric CO sub 2 concentrations

Conference ·
OSTI ID:6583463
Models of the lateral transport of surface water in the Atlantic, Indian, and Pacific oceans are proposed on the basis of the distribution pattern of bomb-produced {sup 14}C in the ocean as observed during the Geochemical Ocean Sections Study program. The global pattern of water column inventories of bomb-produced {sup 14}C suggests that an upwelling of bomb-{sup 14}C-free water takes place in the Antarctic, northern Pacific, and equatorial regions, whereas a downwelling of bomb-{sup 14}C-rich surface waters occurs in the temperate oceans and northern Atlantic. A global model of the closed ocean-atmosphere system is constructed on the basis of these dynamic flows for the purpose of estimating the oceanic uptake of excess CO{sub 2}. The model uses four scenarios of future CO{sub 2} emissions from fossil fuel consumption and tropical deforestation to predict atmospheric CO{sub 2} concentrations. Although the resulting patterns of predicted CO{sub 2} levels are similar to those in the report given by Intergovernmental Panel on Climate Change (IPCC), the uptake of CO{sub 2} from fossil fuel in the lateral transport model is more efficient than that in the general box-diffusion models used by IPCC: that is, all predictions from the model are lower than those given by IPCC. 12 refs., 7 figs., 1 tab.
Research Organization:
Oak Ridge National Lab., TN (USA)
Sponsoring Organization:
DOE/ER
DOE Contract Number:
AC05-84OR21400
OSTI ID:
6583463
Report Number(s):
CONF-9009164-2; ON: DE90017762
Country of Publication:
United States
Language:
English