https://essopenarchive.org/doi/pdf/10.22541/essoar.175130099.96612620

*Authors*
Haruki Hirasawa, Matthew Henry, Alex M Mason, Philip J Rasch, Sarah J
Doherty, Robert Wood, James Haywood, Knut Von Salzen

*30 June 2025*

*Abstract*
The climate intervention approach Marine Cloud Brightening (MCB) would aim
to reduce climate warming by injecting sea salt aerosol (iSSA) into the
lower troposphere to increase cloud albedo. Due to the short atmospheric
lifetime of tropospheric aerosol, MCB iSSA emissions and their resulting
radiative forcing are regional by nature. This presents a significant
challenge and opportunity, as there are many potential patterns of MCB
implementation that could produce substantially varying climate responses.
Simulations of MCB implementation in the subtropical oceans show global
cooling, but may also show strong, though potentially undesirable, regional
temperature and precipitation responses. Here, we use three Earth System
Models (ESMs) to estimate the impact of MCB implementation in fourteen
different ocean regions, assessing MCB forcing and cooling efficiency in
each region and examining the patterns of temperature response from each
case. We find that iSSA emissions in the midlatitude oceans produce
stronger cloud forcing, greater cooling efficiency, and more spatially
uniform cooling. With this information, we evaluate a novel MCB emission
strategy that places emissions in the midlatitude oceans. The ESMs show
this iSSA emission pattern produces temperature and precipitation responses
across all three ESMs that are quite similar in pattern (but of opposite
sign) to the greenhouse gas (GHG) response. Thus, compared to previously
tested iSSA injection patterns, midlatitude MCB implementations may be more
suitable when intending to maintain climates close to present day
conditions.

*Source: ESS Open Archive*

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