Tug of war on summertime circulation between radiative forcing and sea surface warming

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The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6. (2016, background): “, 2016), circulation (e.g. He et al., 2014; Zhou et al., 2014; Kamae et al., 2014; Bellomo and Clement, 2015; Shaw and Voigt, 2015) and stability (e.”
An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models (2020, background): “…role in determining regional climate (e.g., Broccoli & Manabe, 1992; Rodwell & Hoskins, 2000) and in projected future regional climate change (e.g., Seager et al., 2014; Shaw & Voigt, 2015; Simpson et al., 2016; Wills et al., 2019) and are, therefore, an important aspect to simulate correctly.”
Extreme weather events in early summer 2018 connected by a recurrent hemispheric wave-7 pattern (2018, background): “Such temperature contrast create an increased zonal temperature gradient at the coastlines and provide a stationary vorticity source that triggers and maintains atmospheric waves (30, 31).”