Poster's note: significant, in that it removes or moderates a justification
for CE in aggressive mitigation scenarios.

https://www.nature.com/articles/s41586-019-1554-z
Climate and air-quality benefits of a realistic phase-out of fossil fuels
Drew Shindell & Christopher J. Smith
Naturevolume 573, pages408–411 (2019) | Download Citation

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Abstract
The combustion of fossil fuels produces emissions of the long-lived
greenhouse gas carbon dioxide and of short-lived pollutants, including
sulfur dioxide, that contribute to the formation of atmospheric aerosols1.
Atmospheric aerosols can cool the climate, masking some of the warming
effect that results from the emission of greenhouse gases1. However,
aerosol particulates are highly toxic when inhaled, leading to millions of
premature deaths per year2,3. The phasing out of unabated fossil-fuel
combustion will therefore provide health benefits, but will also reduce the
extent to which the warming induced by greenhouse gases is masked by
aerosols. Because aerosol levels respond much more rapidly to changes in
emissions relative to carbon dioxide, large near-term increases in the
magnitude and rate of climate warming are predicted in many idealized
studies that typically assume an instantaneous removal of all anthropogenic
or fossil-fuel-related emissions1,4,5,6,7,8,9. Here we show that more
realistic modelling scenarios do not produce a substantial near-term
increase in either the magnitude or the rate of warming, and in fact can
lead to a decrease in warming rates within two decades of the start of the
fossil-fuel phase-out. Accounting for the time required to transform power
generation, industry and transportation leads to gradually increasing and
largely offsetting climate impacts of carbon dioxide and sulfur dioxide,
with the rate of warming further slowed by reductions in fossil-methane
emissions. Our results indicate that even the most aggressive plausible
transition to a clean-energy society provides benefits for climate change
mitigation and air quality at essentially all decadal to centennial
timescales.

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