![]() ![]() The largest CO 2 emission was observed in the northern part (4.02 ± 1.92 mmol/m 2/d) followed by the southern part (2.28 ± 0.80 mmol/m 2/d) and then the eastern part (0.46 ± 0.28 mmol/m 2/d). The result showed that almost all parts of the Bintan coastal water were carbon sources during first transition season. CO 2 fluxes dynamics were calculated from pCO 2 (surface water and atmosphere), temperature, salinity, and wind speed. In addition, this study was also conducted in the southern and northern parts in April 2016. This study was conducted in the eastern part of Bintan coastal water in April and August 2014. ![]() This study aims to understand the spatio-temporal variation of CO 2 fluxes in Bintan Island coastal water, and the factors influencing it. ![]() Systematic study on variability of CO 2 flux from or to the watern column is essential to understand the whole conditions of Bintan Island coastal water. Spatio-temporal variability of CO 2 flux may shows the whole condition of Bintan Island coastal water, especially in correlation with the primary production. However, flux and partial pressure of CO 2 ( pCO 2) dynamically follows spatio-temporal variability. Eastern part of Bintan coastal water plays a major role as CO 2 sink. ![]() Variation of Air-Sea CO 2 Fluxes in Bintan Island Coastal Water. ![]()
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