Measurement technique of CO
2 for coastal seas is developed and applied to elucidate CO
2 dynamics in the coastal regions, where the photosynthetic rate is far larger than that in the open sea and the short-term change is significant. Continuous measurements of salinity, pH and DO were conducted at three stations in Osaka Bay. The values of CO
2 related terms were calculated using a classical method that uses pH and total alkalinity. Dissolved inorganic carbon (DIC) and DO fluctuated with high correlation (R
2 = 0.97). This suggests that CO
2 system can be measured by this method in coastal regions. DO and pCO
2 (CO
2 partial pressure) records in the eastern Osaka Bay, where primary production is significant, indicated prominent diurnal variations which correspond to diurnal irradiation variations. In contrast, magnitudes of DO and pCO
2 variations were smaller in a well mixed reason in the western Osaka Bay.
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