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Potential effects of stratospheric aerosol injection on the mean and extreme climate of South America

Modelling
Argentina | Camilloni
Extreme weather - droughts, Precipitation, Temperature

Summary

Stratospheric aerosol injection (SAI) could substantially reduce future warming and extreme temperatures in South America, limiting increases to below 1°C instead of over 4°C. SAI would also lessen extreme rainfall and drought duration in key regions, but its effects vary locally and may introduce new uncertainties. While SAI could help moderate climate extremes and alleviate droughts, it is not a uniform solution and further research is needed to understand its risks and benefits.

Abstract

This study assesses the potential climate effects of stratospheric aerosol injection (SAI) across South America using simulations from the Geoengineering Large Ensemble. 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 and southeastern 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 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 March–April–May. While SAI could reduce climate extremes in South America, its uneven effects introduce uncertainties and raise the need for further research.

Publication data

Journal: Environmental Research: Climate
Date: 26 September 2025
DOI: 10.1088/2752-5295/ae065a

Authors

Carla Gulizia

University of Buenos Aires & CONICET

Ramiro Saurral

University of Buenos Aires & CONICET

Inés Camilloni

University of Buenos Aires & CONICET

The Degrees Initiative
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