Abstract. Based upon 14 field surveys conducted between 2003 and 2008, we showed that the seasonal pattern of sea surface partial pressure of CO 2 (pCO 2 ) and sea-air CO 2 fluxes differed among four different physicalbiogeochemical domains in the South China Sea (SCS) proper. The four domains were located between 7 and 23 • N and 110 and 121 • E, covering a surface area of 1344 × 10 3 km 2 and accounting for ∼ 54 % of the SCS proper. In the area off the Pearl River estuary, relatively low pCO 2 values of 320 to 390 µatm were observed in all four seasons and both the biological productivity and CO 2 uptake were enhanced in summer in the Pearl River plume waters. In the northern SCS slope/basin area, a typical seasonal cycle of relatively high pCO 2 in the warm seasons and relatively low pCO 2 in the cold seasons was revealed. In the central/southern SCS area, moderately high sea surface pCO 2 values of 360 to 425 µatm were observed throughout the year. In the area west of the Luzon Strait, a major exchange pathway between the SCS and the Pacific Ocean, pCO 2 was particularly dynamic in winter, when northeast monsoon induced upwelling events and strong outgassing of CO 2 . These episodic events might have dominated the annual sea-air CO 2 flux in this particular area. The estimate of annual sea-air CO 2 fluxes showed that most areas of the SCS proper served as weak to moderate sources of the atmospheric CO 2 , with sea-air CO 2 flux values of 0.46 ± 0.43 mol m −2 yr −1 in the northern SCS slope/basin, 1.37 ± 0.55 mol m −2 yr −1 in the central/southern SCS, and 1.21 ± 1.48 mol m −2 yr −1 in the area west of the Luzon Strait. However, the annual sea-air CO 2 exchange was nearly in equilibrium (−0.44 ± 0.65 mol m −2 yr −1 ) in the area off the Pearl River estuary. Overall the four domains contributed (18 ± 10) × 10 12 g C yr −1 to the atmospheric CO 2 .

Based upon fourteen field surveys conducted between 2003 and 2008, we showed that the seasonal pattern of sea surface partial pressure of CO₂ (pCO₂) and air–sea CO₂ fluxes differed among four different physical-biogeochemical domains in the South China Sea (SCS) proper. The four domains were located between 4 and 23° N and 109 and 121° E, covering ~ 38% of the surface area of the entire SCS. In the area off the Pearl River Estuary, relatively low pCO₂ values of 320 to 390 μatm were observed in all four seasons and both the biological productivity and CO₂ uptake were enhanced in summer in the Pearl River plume waters. In the northern SCS slope/basin area, a typical seasonal cycle of relatively high pCO₂ in the warmer seasons and relatively low pCO₂ in the cold seasons was revealed. In the central/southern SCS area, moderately high sea surface pCO₂ values of 360 to 425 μatm were observed throughout the year. In the area west of the Luzon Strait, a major exchange pathway between the SCS and the Pacific Ocean, pCO₂ was particularly dynamic in winter, when northeast monsoon induced upwelling events and strong outgassing of CO₂. These episodic events might have dominated the annual air–sea CO₂ flux in this particular area. The estimate of annual sea–air CO₂ fluxes showed that, most areas of the SCS proper served as weak sources to the atmospheric CO₂, with sea–air CO₂ flux values of 0.46 ± 0.43 mol m⁻² yr⁻¹ in the northern SCS slope/basin, 1.37 ± 0.55 mol m⁻² yr⁻¹ in the central/southern SCS, and 1.21 ± 1.47 mol m⁻² yr⁻¹ in the area west of the Luzon Strait. However, the annual sea–air CO₂ exchange was nearly in equilibrium (−0.44 ± 0.65 mol m⁻² yr⁻¹) in the area off the Pearl River Estuary. Overall the four domains released (18 ± 10) × 10¹² g C yr⁻¹ into the atmosphere. The CO₂ release rate of the South China Sea essentially exceeded the average CO₂ emission level of most tropical oceans