An ocean emulator trained on CESM2's control climate generalizes to midHolocene orbital forcing in the upper ocean but under-shoots amplitude and misses slow interior dynamics.
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Paleoclimate Boundary Conditions as an Out-of-Sample Test for the Forced Response of Ocean Climate Emulators
An ocean emulator trained on CESM2's control climate generalizes to midHolocene orbital forcing in the upper ocean but under-shoots amplitude and misses slow interior dynamics.