This figure from the paper says it all. Global temperatures drop to 11˚C cooler than preindustrial 🥶🥶 way below the proxy estimate of 6˚C for the Last Glacial Maximum. This is all attributable to the SW cloud feedback in CAM6 (CESM2 w/ CAM5 is fine)
This is a simple example of how past climates can help constrain climate sensitivity. Now if only we could do paleoclimate experiments *while* we develop the next-gen climate models, we could improve future projections of climate change.
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