Circulation response to warming shaped by radiative changes of clouds and water vapour

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The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6. (2016, background): “the ocean, land, seasonal cycle, monsoon and Walker circulations) are not central to understanding intermodel differences in global mean cloud feedbacks and adjustments, and demonstrates the value of aquaplanet experiments for investigating the origin of such differences, as well as differences in z”
Connections Between Clouds, Radiation, and Midlatitude Dynamics: a Review (2015, background): “Using a cloud-locking procedure in two climate models, Voigt and Shaw [47] showed that LW cloud feedbacks also tend to enhance the poleward shift of the midlatitude jets upon an SST increase; they ascribed this result to the stabilization of the tropical troposphere by the LW cloud feedback, which a”
Narrowing of the ITCZ in a warming climate: Physical mechanisms (2016, background): “…and Sobel, 2002], the horizontal diffusivity of moisture [Sobel and Neelin, 2006], cloud-radiative and water vapor-radiative effects [Bretherton and Sobel, 2002; Voigt and Shaw, 2015; Harrop and Hartmann, 2016], and the skewness of the vertical velocity distribution [Pendergrass and Gerber, 2016].”