https://acp.copernicus.org/articles/25/13103/2025/

*Authors: *Weijie Fu, Xu Yue, Chenguang Tian, Rongbin Xu, and Yuming Guo

*21 October 2025*

*Abstract*
As global temperature rises, the severity and frequency of droughts are
projected to increase. Stratospheric aerosol injection (SAI) has been
proposed as a potential solution to reduce surface temperatures, but its
effectiveness in alleviating drought extremes remains unclear. Here, we
assess the global impacts of SAI on drought extremes based on experiments
from the Geoengineering Model Intercomparison Project phase 6 (GeoMIP6) and
the Geoengineering Large Ensemble Project (GLENS). By 2100, the frequency
of extreme droughts is projected to increase by 7.33 % under the
high-emission Shared Socioeconomic Pathways 5 (SSP5-8.5) scenario relative
to present day. SAI reduces this increase by 1.99 % in GeoMIP6, and by 1.80
% in GLENS compared with Representative Concentration Pathways 8.5
(RCP8.5). Attribution analyses show that SAI-induced cooling alone reduces
extreme drought frequency by 3.42 % in GeoMIP6 and 4.28 % in GLENS relative
to their respective high-emission scenarios, outweighing the 2.12 %
increase driven by SAI-induced precipitation reductions under the same
conditions. However, these rainfall deficits lead to substantial inequities
in drought exposures. Compared to developed nations, countries with less
development experience smaller reductions, or even increases, in economic
and population exposure to extreme drought under SAI relative to SSP5-8.5
or RCP8.5. These findings suggest that the current SAI strategies in
GeoMIP6 and GLENS may induce the risk of unintentionally worsening regional
hydroclimatic disparities.

*Source: EGU*

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