https://acp.copernicus.org/articles/24/13253/2024/

*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?,
Atmos. Chem. Phys., 24, 13253–13268,
https://doi.org/10.5194/acp-24-13253-2024, 2024.

*Published: 29 November 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 that
have the same global-mean temperature target, altitude of injection, and
hemispherically symmetric injection rates. These are as follows: injection
at the Equator (EQ) and injection at 15° N and S (15N+15S), 30° N and S
(30N+30S), or 60° N and S (60N+60S). We show that injection at the Equator
leads to a substantial undercooling of the Arctic, a significant reduction
in tropical precipitation, reductions in high-latitude ozone, heating in
the tropical lower-stratosphere, 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, our work shows that the
30N+30S strategy is a good candidate strategy for an intermodel comparison
and is easier to implement than a multi-latitude controller algorithm.

*Source: EGU*

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