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Noah D. Brenowitz, Tom Beucler, Michael Pritchard, and Christopher S. Bretherton

). The goal of the NN parameterization ( Rasp et al. 2018 ; Gentine et al. 2018 ) is to emulate how the embedded SAM models vertically redistribute temperature (approximately Q 1 ) and water vapor (approximately Q 2 ) in response to given coarse-grained conditions from the host model’s primitive equation dynamical predictions (i.e., temperature profile, water vapor profile, meridional velocity profile, surface pressure, insolation, surface sensible heat flux, and surface latent heat flux; all

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