Extended Data Fig. 1: Warming along mid-Atlantic Ocean section.
From: Hydrological cycle amplification reshapes warming-driven oxygen loss in the Atlantic Ocean
(a) ESM2M temperature trend due to total climate effect (200-year trend in the Standard experiment, averaged across 5 members), (b) ESM2M temperature trend due to hydrological effect (Difference in 200-year trends between the Standard and Fix- SSS experiments, averaged over 5 members for each experiment), (c) ORAS5 historical temperature trend (1958-2017). SST trend in (d) climate effect, (e) hydrological effect, (f) ORAS5 historical period.
