Abstract:Abstract. The accumulation of anthropogenic CO2 emissions in the atmosphere has been buffered by the global oceans absorbing CO2 and acting as a net CO2 sink. The CO2 flux between the atmosphere and the ocean, that collectively results in the oceanic carbon sink, is spatially and temporally variable, and fully understanding the driving mechanisms behind this flux is key to assessing how the sink may change in the future. In this study a time series decomposition analysis was applied to satellite observations t… Show more
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