https://journals.ametsoc.org/view/journals/clim/aop/JCLI-D-25-0337.1/JCLI-D-25-0337.1.xml

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

Online Publication: *12 Dec 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, reflect more sunlight, and cool
the surface. 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 MCB implementation patterns that could produce widely
varying climate responses. Previous modeling studies suggest that MCB
implementation in the subtropical oceans can cause global cooling, but
often result in remote regional temperature and precipitation responses
that may be considered undesirable. 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 emits
iSSA 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: AMSO*

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