Probability of a reduction in the formation rate of the subsurface water in the North Pacific during the 1980s and 1990s

Comparing the apparent oxygen utilization (AOU) and apparent CFC tracer age s (tau) between extensive decadal reobservation data along 47 degreesN ('85 -'99) and 165 degreesE ('87-'00) lines, we found that both AOU and tau mark edly increased over the North Pacific between 26.4 - 27.4 sigma (0). The ob served AOU increase was almost consistent with the AOU increase calculated from observed change of tau. Based on a linear trend of increasing AOU over 30 years ('68-'98) in the subpolar region [Ono et al., 2001], we concluded that the formation rate of the subsurface water in the North Pacific has c ontinuously reduced at least during the last fifteen years. In the North Pa cific, the recent uptake rate of oceanic anthropogenic carbon was also esti mated as reduced by as much as 10% from the efficiency of anthropogenic car bon absorption in the middle of 1980s.