The Role of Atmosphere Feedbacks during ENSO in the CMIP3 Models. Part III: The Shortwave Flux Feedback

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Climate change projections using the IPSL-CM5 Earth System Model: from CMIP3 to CMIP5 (2013, background): “The main atmospheric feedbacks are evaluated following Lloyd et al. (2011, 2012).”
ENSO representation in climate models: from CMIP3 to CMIP5 (2013, methodology): “Yet, these processes are critical for the simulation of the shortwave 332 feedback as showed by Lloyd et al (2011, 2012).”
ENSO stability in coupled climate models and its association with mean state (2013, background): “Although considerable progress has been made towards more realistic ENSO simulation, systematic errors still persist (Capotondi et al. 2006; Guilyardi et al. 2009a; Kim and Jin 2011b; Lloyd et al. 2009; Lin 2007; Zhang and Jin 2012).”
Strong and moderate nonlinear El Niño regimes (2016, background): “5) is dominated by entrainment and surface heat fluxes (not shown), the latter of which would be associated with enhanced cloudiness response during the strong EN (Lloyd et al. 2012), although with the use of a deeper layer (e.”