Abstract
Recent geochemical estimates of N
2-fixation in the North Atlantic ocean indicate rates that are significantly higher than those derived from direct observations. In this paper different N
2-fixation rate scenarios are explored using a one-dimensional, biogeochemical model that includes an explicit representation of
Trichodesmium. This model reproduces most of the observed interannual variability in phytoplankton production and generates seasonal
Trichodesmium biomass and N
2-fixation cycles similar to those observed at BATS. Two solutions are presented, one where the N
2-fixation rate is increased enough to reproduce the observed summertime drawdown of DIC, and a second where it is tuned to reproduce the observed sediment trap fluxes. The high N
2-fixation solution reproduces the seasonal and interannual variability in DIC concentrations quite accurately and generates N
2-fixation rates that agree with direct rate measurements from 1990 and recent geochemical estimates. However, this solution generates export fluxes that are more than 4 times higher than those observed, and predicts the development of DON and DOC anomalies in late summer/early fall that have not been observed. In contrast, the low N
2-fixation solution generates trap fluxes that are approximately correct, but overestimates the summertime DIC concentrations by 20–
30
μmol/
kg
−1
. Both solutions indicate that there is significant interannual variability in N
2-fixation at BATS and that the rates were much lower in 1995–1996 than in the previous six years. It is suggested that this variability is linked to decadal-scale fluctuations in the North Atlantic climate.
