SEASONAL VARIABILITY OF SEA-SURFACE DELTA-C-14 IN THE EQUATORIAL PACIFIC IN AN OCEAN CIRCULATION MODEL

The object of this modeling study is to identify the physical mechanis ms responsible for seasonal variability in sea surface Delta(14)C for the equatorial Pacific Ocean. Analyses of Delta(14)C in corals from Gu am, Galapagos, Fanning, and Canton reveal seasonal variability between 30 and 50 per mil during the 1970s and early 1980s. Given that this v ariability occurs on seasonal timescales, whereas air-sea isotopic equ ilibration occurs on a timescale of 5 to 10 years, the variability mus t be due to seasonal variability in the physical circulation of the oc ean. We use the primitive equation ocean circulation model of Gent and Cane [1989], along with the hybrid mixed layer model of Chen et al. [ 1994a], to study the dynamical mechanisms responsible. Upwelling in th e eastern equatorial Pacific brings up Delta(14)C-depleted waters, and air-sea exchange creates high Delta(14)C in the western equatorial Pa cific, establishing horizontal gradients in sea surface Delta(14)C. Se asonally varying lateral advection, acting on these gradients, is the dominant mechanism for Delta(14)C variability in the equatorial Pacifi c. In addition to the runs which were forced with seasonally varying w inds, a run which used interannual winds between 1971 and 1985 was per formed. The substantial interannual Delta(14)C variability present in this run is associated with advective anomalies in the equatorial wave guide.