https://link.springer.com/article/10.1007/s41810-021-00127-0

Response of the Equatorial Atlantic Cold Tongue to Stratospheric Aerosol
Geoengineering

Y. W. Pomalegni, C. Y. Da-Allada, Z. Sohou, E. Baloïtcha, E. A. Alamou, F.
M. Awo, F. Bonou, I. Biao, E. Obada, J. E. Zandagba, S. Tilmes & P. J.
Irvine

Abstract

By increasing Earth-atmosphere system albedo, Stratospheric Aerosol
Geoengineering (SAG) using sulfur dioxide is an artificial potential means,
with the goal to mitigate the global warming effects. In this study, we
used the simulations from Geoengineering Large Ensemble project realized
under the climate change scenario of Representative Concentration Pathway
8.5 (RCP8.5), to investigate the potential impact of SAG on the Sea Surface
Temperature (SST) in Equatorial Atlantic Cold Tongue (EACT) and the
physical processes driving these changes. Results reveal that in the EACT
region, under RCP8.5, SST warms significantly (compared to present‐day
climate) with a maximum of 1.7 °C in July, and this increase in SST is
mainly due to the local processes related to the weakening of vertical
mixing at the base of the mixed layer. This reduction of the vertical
mixing is associated to the diminution of the vertical shear from July to
April and to the increase of ocean stratification from May to June.
However, under SAG, SST decreases significantly throughout the year
(compared to present‐day climate) with a maximum cooling of − 0.4 °C in the
cold tongue period (May–June). This SST cooling is mainly associated with
the non-local processes related to intensification of the westerly
equatorial Atlantic wind stress. Finally, results show that the use of SAG
to offset all global warming under RCP8.5 results in a slight over
compensation of SST in the EACT region.

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