Temporal variability of the South Atlantic Meridional Overturning Circulation between 20°S and 35°S
The Meridional Overturning Circulation plays a critical role in global and regional heat and freshwater budgets by carrying water properties northward and southward within individual ocean basins. This COD-supported research, published in Geophysical Research Letters, examines altimetry-derived synthetic temperature and salinity profiles between 20°S and 34.5°S to estimate the Meridional Overturning Circulation and meridional heat transport.