Regulation of surface carbon dioxide distributions and air–sea fluxes by temperature, biology, and mixing along the North American Atlantic Coastal Ocean Margin
The North American Atlantic Coastal Ocean Margin (NAACOM) was recognized as an atmospheric carbon dioxide (CO2) sink, with large uncertainties in its northern areas due to complex dynamics in controlling the spatiotemporal variability of surface partial pressure of CO2 (pCO2) and limited pCO2 observations. Here, we used a regional reconstructed product to investigate the spatial and seasonal variability