https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1565/

*Authors*
Matthew Henry, Ewa M. Bednarz, and Jim Haywood

*Citations*: Henry, M., Bednarz, E. M., and Haywood, J.: How Does the
Latitude of Stratospheric Aerosol Injection Affect the Climate in UKESM1?,
EGUsphere [preprint], https://doi.org/10.5194/egusphere-2024-1565, 2024.

*Received: 25 May 2024 – Discussion started: 10 Jun 2024*

*Abstract*
Stratospheric Aerosol Injection (SAI) refers to a climate intervention
method by which aerosols are intentionally added to the lower stratosphere
to enhance sunlight reflection and offset some of the adverse effects of
global warming. The climate outcomes of SAI depend on the location, amount,
and timing of injection, as well as the material used. Here, we isolate the
role of the latitude of SO2 injection by comparing different scenarios
which have the same global-mean temperature target, altitude of injection,
and hemispherically symmetric injection rates. These are: injection at the
equator (EQ), and injection at 15° N and S (15N+15S), at 30° N and S
(30N+30S), and at 60° N and S (60N+60S). We show that injection at the
equator leads to many undesirable side effects, such as a residual Arctic
warming, significant reduction in tropical precipitation, reductions in
high-latitude ozone, tropical lower stratospheric heating, and
strengthening of the stratospheric jets in both hemispheres. Additionally,
we find that the most efficient injection locations are the subtropics (15
and 30° N and S), although the 60N+60S strategy only requires around 30 %
more SO2 injection for the same amount of cooling; the latter also leads to
much less stratospheric warming but only marginally increases high-latitude
surface cooling. Finally, while all the SAI strategies come with
trade-offs, we demonstrate that the 30N+30S strategy has, on balance, the
least negative side effects and is easier to implement than a
multi-latitude controller algorithm; thus it is a good candidate strategy
for an inter-model comparison.

*Source: EGUsphere*

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