https://academic.oup.com/oocc/advance-article/doi/10.1093/oxfclm/kgaf013/8107970?searchresult=1

*Authors*

Linus Boselius, Alistair Duffey, Peter J Irvine

https://doi.org/10.1093/oxfclm/kgaf013

Published: *07 April 2025*

*Abstract*

Projected rates of emissions reductions are unlikely to keep global
temperatures from crossing the Paris Agreement temperature targets.
Large-scale carbon dioxide removal (CDR) could help recover a target
temperature after it has been exceeded, producing an overshoot scenario.
Solar radiation modification (SRM) is the idea to cool the planet by
increasing the reflection of incoming solar radiation. SRM could be used in
an overshoot scenario for ‘peak shaving’, where SRM is deployed to maintain
a temperature target during the overshoot. Here, we quantify the effect of
SRM peak shaving on the duration of the overshoot using an adapted
extension of the SSP2-4.5 scenario and an ensemble of variants of the FaIR
simple climate model. We find a substantial reduction in overshoot
duration, which ranges from approximately 5% for multi-decade overshoots up
to approximately 20% for multi-century overshoots. The shortening is
predominantly driven by the ocean response to peak shaving. Peak shaving
results in lower ocean temperatures relative to the overshoot scenario,
inducing a stronger surface temperature response to decreasing and negative
emissions, driving overshoot shortening. Thus, SRM, when deployed as a
complement to emissions reductions and CDR, could end overshoot decades
earlier than otherwise.

*Lay Summary*

Recently, scientists have been researching new ways to help tackle climate
change. One idea is ‘solar radiation modification’ (SRM), which involves
cooling the planet by increasing the reflection of incoming sunlight. ‘Peak
shaving’ is a proposed scenario involving SRM, where SRM is used to global
mean target temperature to a target level, such as 2 °C, until SRM is no
longer needed, decades or centuries later, due to large-scale emissions
removals which have gradually reduced the greenhouse gas concentration in
the atmosphere during a period of net negative emissions. This study
investigates the effect of peak shaving on the time taken for temperatures
to drop below the target temperature without the need for continued SRM. We
find that peak shaving reduces this duration by up to approximately 20%,
which we term ‘overshoot shortening’. We find that this is driven by
avoided increases in ocean temperatures, which impact surface temperatures.

*Source: Oxford Open Climate Change*

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