Poster's note : other, recent research by the author finds the likelihood
of SRM termination to be low

http://adsabs.harvard.edu/abs/2015EGUGA..17.4810I

Initial Climate Response to a Termination Shock

Irvine, Peter
Affiliation:
AA( [email protected])

EGU General Assembly 2015
04/2015

Abstract

The risk of the termination of a deployment of solar radiation management
(SRM) geoengineering has been raised as one of the key concerns about these
ideas. Early studies demonstrated that a rapid warming of the climate would
follow such a termination with global mean temperatures rapidly rising
towards the levels that would have been expected in the absence of SRM
geoengineering. Further work has noted the contrasting timescale of the
adjustment of global mean temperature and sea-level rise, with sea-levels
responding much slower and not reaching the same levels as would have been
the case in the absence of SRM geoengineering. Whilst these previous
studies have shown the basics of the response to a termination of SRM, a
detailed analysis of the climate response in the first months or years of a
termination has not been investigated. To conduct such an analysis tens of
simulations with a termination of SRM are conducted, starting from the end
of a G1 simulation with the HadCM3 model. The termination is initiated in
Spring, Summer, Autumn and Winter to investigate whether the response
depends on the season. Analyzing these results I find some novel dynamic
responses in the initial months and years following a termination of SRM
which have not been seen in previous studies which employed decadal-scale
averages. These include: A reduction in the global-scale hydrological
cycle's intensity in the first weeks following termination, counter to the
longer-term increase; An almost instantaneous adjustment of land-mean
precipitation to the equilibrium value; And substantial shifts in the
pattern of precipitation in the initial years that are distinct from those
seen in the equilibrium response and which are characterized by large
increases in terrestrial precipitation and runoff in many regions.

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