- 1Université Libre de Bruxelles (ULB), Dept. of Geoscience-BGEOSYS, Bruxelles, Belgium
- 2Department of Geosciences, Princeton University, Princeton, NJ, USA
- 3Flanders Marine Institute (VLIZ), Ostend,Belgium
- 4School of Oceanography, Shanghai Jiao Tong University, Shanghai, China
- 5High Meadows Environmental Institute, Princeton University, Princeton, NJ, USA
In spite of considerable efforts using approaches combining observations and modeling, the mechanisms governing the exchange of carbon dioxide (CO2) at the air-sea interface and the spatio-temporal variability of this exchange in coastal oceans are not yet fully understood. The present study uses simulations performed over the last decades with the global ocean biogeochemical model MOM6-COBALT to quantify the relative contributions of thermal changes, oceanic transport, freshwater fluxes, and biological processes to the spatial and seasonal variability of CO2 sources and sinks in the coastal ocean worldwide. These results allow identifying five distinct coastal domains each characterized by different behaviors: coastal regions dominated by biological carbon drawdown, regions controlled by vertical transport, influenced by land-derived inputs, regions shaped by intracoastal alongshore currents, and regions with weak CO2 fluxes. Using the spatial distribution of these behaviors, we propose a new, process-based delineation of the global coastal ocean that reflects the dominance of specific controlling processes for the spatial and seasonal dynamics of the CO2 exchange at the air-sea interface.
Our results also reveal that the spatiotemporal variability of CO2 fluxes in coastal regions is primarily driven by exchanges with the open ocean and local intra-coastal processes, while the influence of continental inputs remains confined to specific hotspot areas. In addition, although thermal changes are often associated with seasonal CO2 variability, their dominance stems from compensating effects between larger non-thermal processes, particularly biological drawdown and vertical transport.
The classification of the global coastal ocean presented in our study provides an updated process-based vision of the complex interplay between physical and biogeochemical drivers of CO2 exchange at the air-water interface. These findings provide a more comprehensive framework for understanding coastal CO2 dynamics and their role in the global carbon cycle, offering valuable insights for predicting the responses of coastal regions to both natural and anthropogenic environmental changes.
How to cite: Regnier, P., Roobaert, A., Laruelle, G., Liao, E., and Resplandy, L.: Unraveling the physical and biological controls of the global coastal CO2 sink, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-12048, https://doi.org/10.5194/egusphere-egu25-12048, 2025.