Air-sea CO2 exchange in the Eastern Atlantic and the Mediterranean Sea based on autonomous surface measurements

Introduction The ATL2MED mission, conducted between October 2019 and July 2020, investigated the variability of air–sea CO 2 exchange in the Eastern Atlantic and the Mediterranean Sea. The main objectives were to assess the spatial and temporal variability of the seawater partial pressure of CO 2 ( p CO 2sw ), identify its controlling physical and biogeochemical processes, estimate the CO 2 fluxes across the sea–air interface, and evaluate the performance of neural network-based predictions (CANYON-MED) in contrasting oceanographic regions. Methods High-resolution autonomous measurements were collected using Saildrone Unmanned Surface Vehicles (USVs), complemented by fixed ocean stations, gliders, and research vessels. Data quality was ensured through cross-validation among platforms, despite challenges such as sensor drift caused by biofouling. Results The results reveal pronounced regional differences in p CO 2sw and CO 2 fluxes, driven by thermal effects, biological activity, and physical mixing. In the Eastern Atlantic, upwelling systems off northwest Africa induced strong outgassing, while the western Mediterranean acted as a CO 2 sink during the spring bloom. Conversely, the Adriatic Sea exhibited episodic CO 2 outgassing, particularly in its southern and northern basins, associated with thermal stratification, river plumes, and coastal upwelling. Discussion Saildrone measurements successfully resolved sub-mesoscale processes typically missed by fixed platforms, demonstrating their potential to enhance ocean CO 2 observations in under-sampled or logistically constrained regions. The good agreement with neural network-based estimates further supports the robustness of the dataset. Overall, these findings emphasize the value of high-resolution, multi-platform approaches for accurately quantifying CO 2 fluxes and improving predictive capabilities in a changing ocean.