Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP)

By Ben Kravitz, K. Caldeira, O. Boucher, A. Robock, Philip J. Rasch, K. Alterskjær, D. Karam, J. Cole, C. Curry, J. Haywood and 14 more. 2013

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An overview of the Earth system science of solar geoengineering (2016, background): “The greatest temperature reductions in these simulations occur in those regions which are expected to show the greatest warming under elevated GHG conditions, that is, at high-latitudes where strong positive feedbacks act on temperature changes.(1,20) In addition to mean temperature changes, the dis”
Impacts, effectiveness and regional inequalities of the GeoMIP G1 to G4 solar radiation management scenarios (2015, background): “Several studies have investigated the climate responses to the GeoMIP G1 (e.g., Schmidt et al., 2012; Kravitz et al., 2013a,b; Tilmes et al., 2013) and G2 (Jones et al., 2013) experiments.”
The Climate Response to Stratospheric Aerosol Geoengineering Can Be Tailored Using Multiple Injection Locations (2017, background): “As an example, a robust result from simulations is that uniformly reducing insolation leads to less polar amplification than in the climate response to greenhouse gases, and hence undercools high latitudes relative to low (Govindasamy & Caldeira, 2000; Kravitz et al., 2013).”