The Evolution of Climate Sensitivity and Climate Feedbacks in the Community Atmosphere Model

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DeepMIP: model intercomparison of early Eocene climatic optimum (EECO) large-scale climate features and comparison with proxy data (2020, unknown): “, 2012) and a larger present-day equilibrium climate sensitivity (∼ 4 C) than previous versions (∼ 3 C) (Gettelman et al., 2012).”
The challenge of simulating the warmth of the mid-Miocene climatic optimum in CESM1 (2013, result): “0 model improvements in comparison to older generation models are described in previous work for modern (Bitz et al., 2012; Neale et al., 2010) and for paleoclimate (Shields et al., 2012; Goldner et al., 2013).”
Radiative forcing in the ACCMIP historical and future climate simulations (2013, methodology): “…for the CMIP5 subset of ACCMIP models shows that in this generation of models there is now an anti-correlation between historical aerosol RF and equilibrium climate sensitivity (ECS; taken from Andrews et al., 2012; Bitz et al., 2012; Gettelman et al., 2012) and GISS-E2-R simulations) (Fig.”
Cloud feedback mechanisms and their representation in global climate models (2017, unknown): “It has been proposed that convective processes play a key role in driving inter-model spread in low cloud amount feedback 105-110 .”