https://par.nsf.gov/biblio/10538156

*Authors*
Romaric_C Odoulami, Haruki Hirasawa, Kouakou Kouadio, Trisha_D Patel,
Kwesi_A Quagraine, Izidine Pinto, Temitope_S Egbebiyi, Babatunde_J Abiodun,
Christopher Lennard, Mark_G

*01 September 2024*

*Abstract*
Solar climate intervention refers to a group of methods for reducing
climate risks associated with anthropogenic warming by reflecting sunlight.
Marine cloud brightening (MCB), one such approach, proposes to inject
sea‐salt aerosol into one or more regional marine boundary layer to
increase marine cloud reflectivity. Here, we assess the potential influence
of various MCB experiments on Africa's climate using simulations from the
Community Earth System Model (CESM2) with the Community Atmosphere Model
(CAM6) as its atmospheric component. We analyzed four idealized MCB
experiments under a medium‐range background forcing scenario (SSP2‐4.5),
which brighten clouds over three subtropical ocean regions: (a) Northeast
Pacific (MCBNEP); (b) Southeast Pacific (MCBSEP); (c) Southeast Atlantic
(MCBSEA); and (d) these three regions simultaneously (MCBALL). Our results
suggest that the climate impacts of MCB in Africa are highly sensitive to
the deployment region. MCBSEPwould produce the strongest global cooling
effect and thus could be the most effective in decreasing temperatures,
increasing precipitation, and reducing the intensity and frequency of
temperature and precipitation extremes across most parts of Africa,
especially West Africa, in the future (2035–2054) compared to the
historical climate (1995–2014). MCB in other regions produces less cooling
and wetting despite similar radiative forcings. While the projected changes
under MCBALLare similar to those of MCBSEP, MCBNEPand MCBSEAcould see more
residual warming and induce a warmer future than under SSP2‐4.5 in some
regions across Africa. All MCB experiments are more effective in cooling
maximum temperature and related extremes than minimum temperature and
related extremes.

*Source: Nsf*

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