Surface salinity maximum in the western boundary of the Tropical Atlantic as observed from SMOS salinity maps
- 1Marine and Environmental Sciences Centre, University of Lisbon, Portugal
- 2Institut de Ciències del Mar, CSIC, Spain
- 3Instituto Oceanográfico da Universidade de São Paulo, Brasil
The spatiotemporal evolutions of sea surface salinity measurements from the SMOS satellite reveal presence of a local salinity maximum in the northwestern tropical Atlantic beginning in September increasing with a Maximum in October and disappearing in January. Its structure and variability are analyzed through SMOS SSS daily products derived with advanced techniques developed at the Barcelona Expert Centre during 9 years. The results are compared with in situ data along the North Brazil Current (NBC) from the Prediction and Research moored Array in the Tropical Atlantic - PIRATA program. This seasonal tropical SSS maximum, produces the salty signature Northward of the NBC, which is seen as a localized salinity maximum on satellite imagery, in contrast to the fresh signature present in summer-early fall. These changes suggest a change in the composition of water masses that enter in the South Atlantic contributing to an alteration in the dynamics of global circulation.
How to cite: Castellanos, P., Olmedo, E., Campos, E., Santis, W., and Dias, J.: Surface salinity maximum in the western boundary of the Tropical Atlantic as observed from SMOS salinity maps, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-13538, https://doi.org/10.5194/egusphere-egu22-13538, 2022.