https://link.springer.com/article/10.1007/s12601-025-00261-7

*Authors: *F. F. B. K. Ayissi, C. Y. Da-Allada, E. Baloïtcha, J. Agada, L.
G. Mekonou-Tamko, S. Tilmes & E. Capo-Chichi

*16 January 2026*

*Abstract*
Barrier layer (BL), by reinforcing ocean stratification, can maintain sea
surface waters warming and limit nutrients supply into the euphotic layer,
which is important to marine life. This study investigates the influence of
stratospheric aerosol geoengineering (SAG) on the seasonal variability of
the BL in the northeastern Gulf of Guinea (NEGG) and its causes based on
data from the Geoengineering Large Ensemble project simulated under a high
anthropogenic emission scenario and on observations. Results show that the
model reproduces well the BL pattern according to observations in the
northern Gulf of Guinea. BL is thicker in the NEGG, especially during
boreal autumn, with barrier layer thickness (BLT) reaching a maximum value
of 19 m in October. Under global warming compared to the current climate,
the BLT increases slightly at the beginning of the year and strongly in
boreal autumn by 14% with a maximum of + 4.5 m reached in November. The
largest increase in BLT occurs in the NEGG, but the region of BL thickening
also expands spatially toward the western Gulf of Guinea. The increase of
BLT during boreal autumn is related to a 14% increase in river runoff and
precipitation, with river runoff increasing by 17% and precipitation by 8%.
Under SAG compared to the current climate, the BLT increases by 2% during
boreal autumn in NEGG. This increase in BLT is relatively minor compared to
global warming and is explained partly by a decrease in river runoff and
precipitation of − 7%. Ocean dynamic processes through zonal advection and
vertical mixing contribute to the little increase of BLT.

*Source: Springer Nature Link *

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