Problems with using radiocarbon to infer ocean ventilation rates for past and present climates

The oceanic C-14 distribution reflects mainly the circulation pattern and i ntensity, but is also sensitive to the exchange processes at the air-sea in terface. In order to separate the relative contributions of both effects (t hat might have changed in the past), we incorporate in an ocean general cir culation model two passive tracers, namely, the normalized radiocarbon rati o (Delta(14)C) and the actual age of water. We quantify, for both present a nd glacial conditions, the decoupling between the C-14 ventilation rate and the circulation intensity as the difference between the simulated C-14 age and actual age of water. The C-14 age of the model Antarctic Bottom Water (ABBW) appears systematically older than its actual age, the discrepancy be ing larger for glacial conditions because of the more extensive Antarctic s ea-ice cover. Our results suggest that the AABW flow rate could have been s tronger than today during the Last Glacial Maximum, contrary to what might be inferred from a naive interpretation of C-14 measurements in deep-sea se diment cores. (C) 1999 Elsevier Science B.V. All rights reserved.