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https://arxiv.org/abs/2402.11992

*Authors*
Ezra Brody, Daniele Visioni, Ewa M. Bednarz, Ben Kravitz, Douglas G.
MacMartin, Jadwiga H. Richter, Mari R. Tye

*18 February 2024*

*Abstract*
Climate change is a prevalent threat, and it is unlikely that current
mitigation efforts will be enough to avoid unwanted impacts. One potential
option to reduce climate change impacts is the use of stratospheric aerosol
injection (SAI). Even if SAI is ultimately deployed, it might be initiated
only after some temperature target is exceeded. The consequences of such a
delay are assessed herein. This study compares two cases, with the same
target global mean temperature of 1.5C above preindustrial, but start dates
of 2035 or a delayed start in 2045. We make use of simulations in the
Community Earth System Model version 2 with the Whole Atmosphere Coupled
Chemistry Model version 6 (CESM2-WACCM6), using SAI under the SSP2-4.5
emissions pathway. We find that delaying the start of deployment (relative
to the target temperature) necessitates lower net radiative forcing (-30%)
and thus larger sulfur dioxide injection rates (+20%), even after surface
temperatures converge, to compensate for the extra energy absorbed by the
Earth system. However, many of the surface climate differences between the
2035 and 2045 start simulations appear to be small during the 10-25 years
following the delayed SAI start, although longer simulations would be
needed to assess any longer-term impacts in this model. In addition,
irreversibilities and tipping points that might be triggered during the
period of increased warming may not be adequately represented in the model
but could change this conclusion in the real world.

*Source: arxiv*

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