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U.S. Department of Energy
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Simulations of the carbon cycle in the oceans

Technical Report ·
OSTI ID:5382092
A perturbation approach for simulating carbon dioxide uptake which estimates oceanic uptake of CO{sub 2} in excess of 2 GtC/yr over the last decade is being readied for publication. The recent estimate of <1 GtC/yr is believed to be due to an undersampling bias. A major effort was put into studies of the effect of iron fertilization on uptake of anthropogenic CO{sub 2} by the oceans. We find that while fertilization will reduce the CO{sub 2} increase, it will not reverse the trend. Also, iron fertilization may double nitrous oxide flux out of the ocean, partially canceling the CO{sub 2} reduction and having an unknown effect on the ozone layer. A paper in preparation describes the three-dimensional seasonal variations in nitrogen concentration in the ocean. The model does a reasonable job of matching observations, although performance could be improved by adjusting the biological parameters and increasing the physical resolution. A dual-currency carbon-nitrogen model is being constructed, with a first version recently completed. (MHB)
Research Organization:
Princeton Univ., NJ (United States). Dept. of Geological and Geophysical Sciences
Sponsoring Organization:
DOE; USDOE, Washington, DC (United States)
DOE Contract Number:
FG02-90ER61052
OSTI ID:
5382092
Report Number(s):
DOE/ER/61052-1; ON: DE91018475
Country of Publication:
United States
Language:
English