https://iopscience.iop.org/article/10.1088/2752-5295/adf251

*Authors*
José Houénoukpo Agada, Casimir Yélognissè Da-Allada, Marius Bocco-Koube,
Ezinvi Baloïtcha, Francis F B K Ayissi, Lydie Gaelle Mekonou-Tamko, Simone
Tilmes and Leonard Olabi Worou

Accepted Manuscript online *21 July 2025 *

DOI 10.1088/2752-5295/adf251

*Abstract*
Stratospheric Aerosol Geoengineering (SAG), which is based on the injection
of sulfur dioxide into the stratosphere, is one of the methods proposed to
mitigate the effects of global warming. In this study, we investigate the
potential impact of SAG on Sea Surface Salinity (SSS) in the Eastern
Tropical Atlantic Ocean and the physical processes involved in SSS changes,
using Geoengineering Large Ensemble (GLENS) simulations performed under the
RCP8.5 scenario. Results reveal that, in the mean state, under global
warming (RCP8.5), SSS decreases (relative to current climate) in the
Northern Gulf of Guinea (NGG) around the Niger River region and in the
Southern Gulf of Guinea (SGG) around the Congo River region, whereas, under
SAG, SSS remains unchanged (relative to current climate) in both regions.
At seasonal time scale, under RCP8.5 (relative to current climate), in the
NGG region, SSS decreases all year round with strongly negative values of -
0.6 PSU (practical salinity unity) in boreal winter (December/January),
whereas under SAG, the decrease in SSS disappears and SSS turns slightly
positive all year round (with SSS values below + 0.2 PSU). In the SGG
region, under RCP8.5, SSS also shows a year-round decrease, as in NGG, with
a maximum negative SSS value (- 0.9 PSU) in May. Under SAG, from December
to June, SSS increases with a maximum positive value (+ 0.4 PSU) in April
and the rest of the year, SSS decreases with a strong negative value (- 0.3
PSU) in September. Using SSS budget in the mixed-layer, the findings
indicate that under RCP8.5 and SAG, in the NGG, changes in SSS are mainly
caused by changes in precipitation and rivers runoffs, whereas in SGG,
changes in rivers runoffs and vertical mixing are responsible for SSS
changes.

*Source: IOP Science*

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