Poster's note : is this scenario anywhere near an upper limit for SRM?

http://onlinelibrary.wiley.com/doi/10.1002/2013JD020627/abstract

Keywords:

GeoMIP;Arctic;sulfate aerosols;sea ice;snow

Abstract

[1] We analyzed output from the Geoengineering Model Intercomparison
Project (GeoMIP) for the two most "realistic" scenarios, which use the
Representative Concentration Pathway of 4.5 Wm-2 by 2100 (RCP4.5) as the
control run and inject sulfate aerosol precursors into the stratosphere.
The first experiment, G3, is specified to keep RCP4.5 top of atmosphere
(TOA) net radiation at 2020 values by injection of sulfate aerosols, and
the second, G4, injects 5 Tg SO2 per year. We ask whether geoengineering by
injection of sulfate aerosols into the lower stratosphere from the years
2020 to 2070 is able to prevent the demise of minimum annual sea ice
extent, or slow spring snow cover loss. We show that in all available
models, despite geoengineering efforts, September sea ice extents still
decrease from 2020 to 2070, although not as quickly as in RCP4.5. In two of
five models, total September ice loss occurs before 2060. Spring snow
extent is increased from 2020 to 2070 compared to RCP4.5 although there is
still a negative trend in 3 of 4 models. Because of the climate system lag
in responding to the existing radiative forcing, to stop Arctic sea ice and
snow from continuing to melt, the imposed forcing would have to be large
enough to also counteract the existing radiative imbalance. After the
cessation of sulfate aerosol injection in 2070, the climate system rebounds
to the warmer RCP4.5 state quickly, and thus any sea ice or snow retention
as a result of geoengineering is lost within a decade.

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