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https://esd.copernicus.org/articles/15/307/2024/

*Authors*
Susanne Baur, Benjamin M. Sanderson, Roland Séférian, and Laurent Terray

*27 March 2024*

https://doi.org/10.5194/esd-15-307-2024

*Abstract*
Solar radiation modification (SRM) is increasingly being discussed as a
potential tool to reduce global and regional temperatures to buy time for
conventional carbon mitigation measures to take effect. However, most
simulations to date assume SRM to be an additive component to the climate
change toolbox, without any physical coupling between mitigation and SRM.
In this study we analyze one aspect of this coupling: how renewable energy
(RE) capacity, and therefore decarbonization rates, may be affected under
SRM deployment by modification of photovoltaic (PV) and concentrated solar
power (CSP) production potential. Simulated 1 h output from the Earth
system model CNRM-ESM2-1 for scenario-based experiments is used for the
assessment. The SRM scenario uses stratospheric aerosol injections (SAIs)
to approximately lower global mean temperature from the high-emission
scenario SSP585 baseline to the moderate-emission scenario SSP245. We find
that by the end of the century, most regions experience an increased number
of low PV and CSP energy weeks per year under SAI compared to SSP245.
Compared to SSP585, while the increase in low energy weeks under SAI is
still dominant on a global scale, certain areas may benefit from SAI and
see fewer low PV or CSP energy weeks. A substantial part of the decrease in
potential with SAI compared to the SSP scenarios is compensated for by
optically thinner upper-tropospheric clouds under SAI, which allow more
radiation to penetrate towards the surface. The largest relative reductions
in PV potential are seen in the Northern and Southern Hemisphere
midlatitudes. Our study suggests that using SAI to reduce high-end global
warming to moderate global warming could pose increased challenges for
meeting energy demand with solar renewable resources.

*Source: EGU*

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