Role of volcanic and anthropogenic aerosols in the recent global surface warming slowdown

By Doug M. Smith, B. Booth, N. Dunstone, R. Eade, L. Hermanson, G. Jones, Adam A. Scaife, Katy L. Sheen, V. Thompson. 2016

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Analyzing the dependence of global cloud feedback on the spatial pattern of sea surface temperature change with a Green's function approach (2017, background): “…Andrews, 2016; Zhou et al., 2016], the latter being affected by decadal climate variability [Watanabe et al., 2014; Meehl et al., 2016], non-CO2 forcings [Takahashi and Watanabe, 2016; Smith et al., 2016] and ocean heat uptake [Marshall et al., 2015; Winton et al., 2013; Rugenstein et al., 2016].”
The Radiative Forcing Model Intercomparison Project (RFMIP): Experimental Protocol for CMIP6 (in open review: 10.5194/gmd-2016-88) (2016, background): “…which aerosol forcing underlies the warming hole in the east-central United States (Leibensperger et al., 2012), shifts in the tropical convergence zones (Bollasina et al., 2011), or phasing of Atlantic (Booth et al., 2012) and Pacific (Meehl et al., 2009; Smith et al., 2016) decadal variability.”