Abstract:The seasonal evolution of dissolved inorganic carbon (DIC) and CO 2 air-sea fluxes in the Jiaozhou Bay was investigated by means of a data set from four cruises covering a seasonal cycle during 2003 and 2004. The results revealed that DIC had no obvious seasonal variation, with an average concentration of 2035 µmol kg-1 C in surface water. However, the sea surface partial pressure of CO 2 changed with the season. pCO 2 was 695 µatm in July and 317 µatm in February. Using the gas exchange coefficient calculated… Show more
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