Poster's note: At 4x CO2 we'd be at risk of an anoxic event, as my
post earlier this week showed.  A 15% rainfall drop would be the least
of our worries...

Paper: http://www.earth-syst-dynam.net/3/63/2012/esd-3-63-2012.pdf (open access)
Press piece: 
http://cordis.europa.eu/fetch?CALLER=EN_NEWS&ACTION=D&SESSION=&RCN=34895

Solar irradiance reduction to counteract radiative forcing from a
quadrupling of CO2: climate responses simulated by four earth
system models

H. Schmidt, K. Alterskjær, D. Bou Karam, O. Boucher, A. Jones, J. E.
Kristjansson ´, U. Niemeier, M. Schulz
A. Aaheim, F. Benduhn, M. Lawrence, and C. Timmreck

Abstract. In this study we compare the response of four
state-of-the-art Earth system models to climate engineering
under scenario G1 of two model intercomparison projects:
GeoMIP (Geoengineering Model Intercomparison Project)
and IMPLICC (EU project “Implications and risks of engineering solar
radiation to limit climate change”). In G1,
the radiative forcing from an instantaneous quadrupling of
the CO2 concentration, starting from the preindustrial level,
is balanced by a reduction of the solar constant. Model responses to
the two counteracting forcings in G1 are compared to the preindustrial
climate in terms of global means
and regional patterns and their robustness. While the global
mean surface air temperature in G1 remains almost unchanged compared
to the control simulation, the meridional
temperature gradient is reduced in all models. Another robust response
is the global reduction of precipitation with
strong effects in particular over North and South America
and northern Eurasia. In comparison to the climate response
to a quadrupling of CO2 alone, the temperature responses are
small in experiment G1. Precipitation responses are, however, in many
regions of comparable magnitude but globally
of opposite sign.

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