https://iopscience.iop.org/article/10.1088/2752-5295/ae065a

*Authors*: Carla Gulizia, Ramiro I Saurral and Ines A Camilloni

Accepted Manuscript online *12 September 2025*

DOI 10.1088/2752-5295/ae065a

*Abstract*
This study assesses the potential climate effects of stratospheric aerosol
injection (SAI) across South America using simulations from the
Geoengineering Large Ensemble (GLENS). We analyze and compare projected
changes in mean and extreme temperature and precipitation under a high
radiative forcing scenario (RCP8.5), with and without SAI, for 2021–2050
and 2051–2080. Results indicate that SAI would substantially reduce
warming, particularly in extreme temperatures. Without SAI, maximum and
minimum temperatures in the South American Monsoon (SAM) and Southeastern
South America (SES) regions are projected to increase by over 4 °C by
2051–2080. However, with SAI these increases are limited to below 1 °C with
some regions like SAM, SES, and parts of northern (NSA) and southeastern
(SSA) South America potentially experiencing negative temperature changes.
Precipitation responses under SAI simulations show an overall reduction in
the magnitude of the projected changes in mean and extreme precipitation
compared to the high-forcing scenario without SAI. The mean and wettest
precipitation changes in SES may be reduced, whereas the drought duration
in northeastern South America (NES) and NSA could be shortened. In
addition, SAI could alleviate persistent drought conditions in southwestern
South America (SWS). The compensation and eventual reversal in SWS are
explained by slight increases in precipitation during the cold season
(MAM). While SAI could reduce climate extremes in South America, its uneven
effects introduce uncertainties and raise the need for further research.

*Source: IOP Science *

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