https://iopscience.iop.org/article/10.1088/2752-5295/ad53f3

*Authors*
Ezra Brod, Daniele Visioni, Ewa M Bednarz, Ben Kravitz, Douglas G
MacMartin, Jadwiga H Richter and Mari Rachel Tye

*Accepted Manuscript online 4 June 2024*

DOI 10.1088/2752-5295/ad53f3

*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 ~1.5°C 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. Southern hemisphere ozone is higher from 2035
to 2050 in the delayed start scenario, but converges to the same value
later in the century. 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: IOP SCIENCE *

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