An automatic measuring system for the partial pressure, pCO 2 , of atmospheric and oceanic carbon dioxide was developed.The system was mounted on a moored buoy for routine observation of maritime meteorology in the East China Sea. CO 2 observations were conducted from 29 June 1997 to 6 January 1998. During the observation period, the atmospheric pCO 2 showed little variation (341 to 365 µatm), whereas pCO 2 in the surface water varied significantly (308 to 408 µatm). In the summer, pCO 2 was higher in the surface water than in the overlying atmosphere, implying that this area was a source for atmospheric CO 2 , though it became a sink after late September. Time series data clearly exhibited significant short-term variations in the oceanic pCO 2 , i.e., sudden variations during the passage of typhoons, and diurnal variations driven by the diurnal variations in the sea-surface temperature under calm conditions. The effects of typhoons on ocean-atmosphere CO 2 exchange at the surface could differ, depending on the relative position of the mooring site with respect to the center of the moving typhoons. These differences result from the different contributions of sea-surface cooling, entrainment, and upwelling. The efflux enhanced by three typhoons accounted for 60% of the efflux of CO 2 in the warm season. It is suggested that typhoons have a significant impact on the carbon cycle in the western subtropical NorthPacific.

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