The Role of Cyclonic Upwelling Eddies in Southern Ocean CO2 Flux

Measurements were made at high spatial and temporal resolution ( ~ 5-km and 1 hour) and include observations of ocean and atmosphere pCO2, air temperature and humidity, wind, ocean skin temperature, SST, salinity, ocean color (Chlorophyll α, CDOM), dissolved oxygen, and ocean current velocity between roughly 13.5°E and 82°E and between the Sub Tropical Front (STF) and the Subantarctic Front (SAF).

The mission track spanned from the Agulhas Return Current south of South Africa to the northern boundary of the Antarctic Circumpolar Current downstream of the Kerguelen Plateau. The primary goal of the mission was to collect data within cyclonic and anticyclonic eddies to quantify CO2 fluxes to better understand physical processes (upwelling and downwelling) that that can contribute to carbon cycling in addition to the biological pump.