https://egusphere.copernicus.org/preprints/2025/egusphere-2025-5591/

*Authors: *Alex M. Mason, Matthew Henry, Haruki Hirasawa, Fiona M.
O'Connor, and James Haywood

*25 November 2025*

*Abstract*
Marine Cloud Brightening (MCB) is a proposed method of Solar Radiation
Modification (SRM). MCB proposes the injection of sea salt aerosols into
marine clouds to enhance their reflectivity aiming to counteract greenhouse
gas (GHG) driven warming. Modelling suggests that the climate effect of MCB
depends on the location of deployments, with some regional MCB resulting in
potentially undesirable climate changes. MCB in midlatitude regions was
found to cause a relatively homogeneous temperature and precipitation
change pattern. Here we seek to quantify the trade-offs associated with
different MCB strategies and to design an “optimal” deployment strategy.
This study analyses 42 MCB patch simulations in UKESM1.0, spanning fourteen
different regions and three different injection rates. These simulations
are used to inform deployments with the aim to restore the SSP2-4.5 2040s
mean climate to a baseline of 2014–2033. Multiple climate targets,
consisting of global mean surface air temperature, precipitation, Arctic
September sea ice extent, southern oscillation index, and hemispheric mean
temperatures, are used to inform the design of an optimised 14-region
deployment and a reduced complexity optimised 6-region deployment, which we
compare to the aforementioned 5-region midlatitude MCB deployment. Some
improvements to the midlatitude MCB deployment are observed, in sea ice
restoration and zonal mean temperature response. These results show it may
be possible to design MCB strategies that target several climate responses
simultaneously when combining regional MCB deployments. The results
highlight the importance of including high latitude MCB to achieve Arctic
sea ice restoration in UKESM1.0.

*Source: EGUsphere*

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