https://essopenarchive.org/doi/full/10.22541/essoar.174708323.34069174

*Authors*
Abolfazl Rezaei,
John Christopher Moore,
Simone Tilmes,
Khalil Karami

*12 May 2025*

*Abstract*
Stratospheric aerosol intervention (SAI) is being explored for its
potential to reduce greenhouse gas (GHG) induced climate damages. We assess
the effectiveness of two SAI experiments, G6Sulfur and Geo SSP5-8.5 1.5‎
(here called Geo-SAI), using the CESM2(WACCM6) model, to reduce
hydrological changes under high-emission SSP5-8.5 (no mitigation) pathway.
Geo-SAI stabilizes near surface global temperatures at 1.5℃ above
pre-industrial levels, while G6Sulfur limits temperature rises to those
under the SSP2-4.5 scenario. In our findings, Geo-SAI reverts many, but not
all, hydrological changes induced by SSP5-8.5, restoring global and
regional means, seasonal amplitudes, and peak timings. G6Sulfur delivers
smaller restorations, as expected, due to its smaller prescribed forcing.
In hyper-arid regions such as the Middle East, both SAI scenarios improve
water storage compared with both SSP5-8.5 and present conditions. However,
in wetter or cooler climates, such as the Amazon, middle and southern
Africa and east Europe, they only partly reverse the reductions in
available water (AW) and runoff caused by high GHG emissions. Residual
warming and snowmelt dynamics play an important role in runoff at
mid-to-high latitudes. Additionally, SAI does not completely suppress
GHG-induced vegetation expansion and so over-reduces global runoff in three
latitude bands: 45-65°N, 45-65°S, and 30°S to 0, with end‐of‐century
decreases of 4.1% under G6Sulfur and 7.3% under Geo-SAI, despite mean AW
levels remaining close to present-day. These findings emphasize that while
SAI mitigates many climate-driven hydrological disruptions, its unintended
effects on runoff, vegetation feedbacks, and regional water availability
warrants study—especially in regions heavily dependent on surface water
resources.

*Source: ESS OPEN ARCHIVES*

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