https://egusphere.copernicus.org/preprints/2025/egusphere-2025-5742/

*Authors: *Walker Raymond Lee, Daniele Visioni, Benjamin Moore Wagman,
Christopher Robert Wentland, Ben Kravitz, Shingo Watanabe, Takashi Sekiya,
Andy Jones, Jim Haywood, Matthew Henry, and Ewa Monika Bednarz

*Received: 18 Nov 2025 – Discussion started: 21 Nov 2025*

*Abstract*We report initial results for G6-1.5K-SAI, a climate model
experiment proposed by the Geoengineering Model Intercomparison Project
(GeoMIP). G6-1.5K-SAI, which simulates a stratospheric aerosol injection
(SAI) to limit global warming to ∼ 1.5 °C above preindustrial in each
model, features several design updates relative to previous GeoMIP
experiment G6sulfur, such as hemispherically symmetric subtropical
injection (30° N and 30° S) instead of equatorial injection. Due to
differences in climate sensitivity, models disagree on the amount of
warming to be offset, and therefore on the total injection required. While
they agree strongly on the rate of cooling per unit rate of injection (∼
0.1 °C per Tg SO2 yr−1, a similar value to G6sulfur models with interactive
SO2), similarities in aerosol representation and disagreements in aerosol
optical depth (AOD) per rate of unit injection and in rate of cooling per
unit AOD mean this agreement may not imply accuracy. In all participating
models, SAI cools the land surface more than the ocean and offsets mid- and
high-latitude precipitation increases under global warming, but models
disagree on the magnitude of residual Arctic amplification and changes to
tropical precipitation. Relative to G6sulfur, G6-1.5K-SAI cools the Arctic
more strongly, and also decreases precipitation less, especially in the
tropics and over land. All in all, while the new G6-1.5K-SAI experiment
constitutes an update over the older G6sulfur, due to the differences in
scenario across these two experiments, any differences in SAI impacts must
be evaluated carefully.

*Source: EGUsphere *

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