Preindustrial, historical, and fertilization simulations using a global ocean carbon model with new parameterizations of iron limitation, calcification, and N sub(2) fixation

The Canadian Model of Ocean Carbon (CMOC) has been developed as part of a global coupled climate carbon model. In a stand-alone integration to preindustrial equilibrium, the model ecosystem and global ocean carbon cycle are in general agreement with estimates based on observations. CMOC reproduces global mean estimates and spatial distributions of various indicators of the strength of the biological pump; the spatial distribution of the air-sea exchange of CO sub(2) is consistent with present-day estimates. Agreement with the observed distribution of alkalinity is good, consistent with recent estimates of the mean rain ratio that are lower than historic estimates, and with calcification occurring primarily in the lower latitudes. With anthropogenic emissions and climate forcing from a 1850-2000 climate model simulation, anthropogenic CO sub(2) accumulates at a similar rate and with a similar spatial distribution as estimated from observations. A hypothetical scenario for complete elimination of iron limitation generates maximal rates of uptake of atmospheric CO sub(2) of less than 1PgCy super(-) super(1), or about 11% of 2004 industrial emissions. Even a 'perfect' future of sustained fertilization would have a minor impact on atmospheric CO sub(2) growth. In the long term, the onset of fertilization causes the ocean to take up an additional 77PgC after several thousand years, compared with about 84PgC thought to have occurred during the transition into the last glacial maximum due to iron fertilization associated with increased dust deposition.