https://iopscience.iop.org/article/10.1088/2752-5295/ada8cb/meta

*Authors*
Thales Chile Baldoni, Michelle Simões Reboita, Natália Machado Crespo, João
Gabriel Martins Ribeiro and Rosmeri Portfírio da Rocha

*10 January 2025*

*Abstract*
The South Atlantic Subtropical Anticyclone (SASA) is a key component of
large-scale atmospheric circulation and is responsible for driving the
climate in eastern Brazil and western Africa. Climate projections under
warming scenarios suggest a strengthening, as well as a westward and
southward expansion of this system. However, little is known about how the
combination of global warming and climate intervention affects this system.
To address this, SASA was identified from 2015 to 2099 in a set of
projections with and without stratospheric aerosol injection (SAI).
Projections were obtained from different initiatives: the Assessing
Responses and Impacts of Solar Climate Intervention on the Earth System
with Stratospheric Aerosol Injection (ARISE) using CESM2 global climate
model, the Stratospheric Aerosol Geoengineering Large Ensemble (GLENS)
using CESM1, and the Geoengineering Model Intercomparison Project
(GeoMIP/G6sulfur) using MPI-ESM1-2-LR. As each project has its own specific
model, scenario, SAI location, etc., no intercomparison was carried out
among them. Instead, there is an indication of what occurs in each project
when comparing the near (2040–2059) and the far future (2080–2099)
projections under SAI and no-SAI scenarios. SASA under no-SAI scenarios,
compared to the reference period (2015-2024), follows the pattern described
in the literature, i.e., a tendency to be stronger and wider. However,
these features are more evident in the GLENS project. This same project
suggests that SAI scenarios contribute to reducing the impact of global
warming on the SASA climatology, as SASA in the future acquires
characteristics similar to those of the reference period. One of the
possibilities for it is that GLENS has the largest SAI forcing, given that
the goal was to cancel out the strong greenhouse gas-induced warming in
RCP8.5.

*Source: IOP SCIENCE*

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