We investigate the response of a three-dimensional ocean circulation m
odel (Hamburg LSG) coupled on-line with an oceanic carbon cycle model
(HAMMOCC-3) to El Nino-Southern Oscillation (ENSO) induced fluctuation
s of the wind field. During El Nino 1982/1983, when upwelling and biol
ogical productivity in the equatorial Pacific were strongly reduced an
d sea surface temperatures were increased, the oceanic CO2 partial pre
ssure in this region decreased significantly. Consequently, in 1982/19
83 the CO2 flux from the tropical ocean into the atmosphere was reduce
d. However, in 1983 the interannual deviations from the long-term tren
d in atmospheric CO2 showed in January low and in December high values
with a total shift by more that 1.4 GtC. The model simulation support
the oceanic measurements and predicts a temporary uptake of 0.6 GtC d
uring the ENSO year 1983. We conclude that the concurrent release of C
O2 from the land biosphere must have been about 2 GtC.