https://eartharxiv.org/repository/view/3412/


*Potential for Perceived Failure of Stratospheric Aerosol Injection
Deployment*

Patrick W. Keys, Elizabeth A. Barnes, Noah S. Diffenbaugh, James W. Hurrell
and Curtis M. Bell

*Abstract *
As anthropogenic activities continue to warm the Earth, the fundamental
solution of reducing greenhouse gas emissions remains elusive. Given this
mitigation gap, global warming may lead to intolerable climate changes as
local adaptive capacity is exceeded. Thus, there is emerging interest in
solar radiation management, which is the process of deliberately increasing
Earth's albedo to cool the planet. Stratospheric aerosol injection (SAI) —
the theoretical deployment of particles in the stratosphere to enhance
reflection of incoming solar radiation — is one possible strategy to slow,
pause or reverse global warming. If SAI is ever pursued it will likely be
for a specific aim, such as allowing more time to implement mitigation
strategies, lessening the impacts of extremes, or significantly reducing
the odds of reaching a biogeophysical tipping point. Using an ensemble of
climate model simulations that employ SAI, we quantify the probability that
internal climate variability masks the effectiveness of SAI deployment
regionally. We find that, when global temperature is stabilized,
substantial land areas continue to experience warming temperatures. For
example, up to 55% of the global population experiences rising temperatures
over the decade following SAI deployment, and large areas exhibit
high probability of extremely hot years. These conditions could cause SAI
to be perceived as a failure. Countries with the largest economies
experience some of the largest probabilities of this perceived failure. The
potential for perceived failure of even the most successful SAI strategy
could therefore have major implications for policy decisions in the years
immediately following deployment.

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