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• W2224726714 abstract "Abstract Evidence based on four field surveys conducted between July 2009 and April 2011 indicates that both sea surface partial pressures of CO 2 ( p CO 2 ) and sea–air CO 2 fluxes at Luhuitou fringing reef in Sanya, Hainan Island, northern South China Sea (SCS) are subject to significant seasonal variations. The diurnal variation of seawater p CO 2 ranges from 264 to 579 μ atm in summer, which is much larger than that in autumn (152–335 μ atm), in winter (84–260 μ atm), and in spring (114–228 μ atm). The sea‐air CO 2 flux in summer (∼9.6 mmol CO 2 m −2 d −1 ) is also larger than that in other seasons (i.e.,∼3 mmol CO 2 m −2 d −1 in spring, ∼3.5 mmol CO 2 m −2 d −1 in autumn, and ∼2.7 mmol CO 2 m −2 d −1 in winter). The atmospheric p CO 2 in this reef shows small diurnal and seasonal variations. The integration of the time‐series p CO 2 data shows that the reef area is a weak source of atmospheric CO 2 at ∼0.54 mol CO 2 m −2 yr −1 . Further analyses indicate that the seasonal variations of the surface seawater p CO 2 in Luhuitou fringing reef are mainly affected by seasonally‐dependent biological metabolic processes (organic processe and inorganic process), and that the organic process play a more important role than the inorganic process. Seasonal sea surface temperature (SST) variations and hydrodynamic processes may also have some influence on seawater p CO 2 variation." @default.
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• W2224726714 date "2016-01-01" @default.
• W2224726714 modified "2023-10-16" @default.
• W2224726714 title "Seasonal variations of seawater p <scp>CO</scp> ₂ and sea‐air <scp>CO</scp> ₂ fluxes in a fringing coral reef, northern <scp>S</scp> outh <scp>C</scp> hina <scp>S</scp> ea" @default.
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• W2224726714 doi "https://doi.org/10.1002/2015jc011484" @default.
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