https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GL113914

*Authors*
Jake J. Gristey, Graham Feingold

First published: *21 March 2025*

https://doi.org/10.1029/2024GL113914

*Abstract*
Intentional modification of the sunlight reflected back to space by Earth
has received increasing attention as a potential tool to combat the current
climate crisis. Two approaches have emerged as most viable: Stratospheric
Aerosol Injection (SAI) and Marine Cloud Brightening. This study identifies
a substantial but unrecognized source of cloud brightening caused by SAI,
which we call “diffusion-brightening”; essentially, diffusion of the
radiation field that would accompany SAI can result in sunlight entering
clouds at steeper angles, which increases cloud albedo without actively
injecting aerosols into clouds. We present idealized calculations that
suggest the diffusion-brightening effect can lead to clouds reflecting
about 10% more of the incoming sunlight depending on stratospheric aerosol,
cloud, and Sun conditions. We show that the radiative effect of
diffusion-brightening could exceed that of stratospheric aerosol reflection
in many cloudy scenes, which has global relevance given that clouds cover
around two-thirds of the planet.

*Key Points*
Diffusion of sunlight by stratospheric aerosols can substantially increase
cloud albedo

The radiative effect of stratospheric aerosol injection would be dominated
by inadvertent cloud brightening at many locations and times

This diffusion-brightening effect has important implications for solar
radiation management

*Plain Language Summary*
The deliberate release of particles in the stratosphere—to reflect a small
amount of sunlight back to space and thereby cool the surface—is a
controversial but increasingly common topic of debate in the face of
ongoing global warming. One known side-effect is that the sunlight below
these particles would be spread out into different directions. We
demonstrate that this spreading of sunlight into different directions can
make low-level marine clouds substantially brighter. The importance of this
cloud brightening does not appear to have been appreciated in previous
studies on the topic. Yet, this cloud brightening is crucial to understand
the overall amount of sunlight that would be reflected and has profound
implications for potential implementation of any such approach in the
future.

*Source: AGU*

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