Supplementary Fig 5. Decadal warming trends for different ocean regions in CMIP6 models and observations. The multi-model mean (in blue) is calculated using one ensemble member for each of 40 different models used. The spread across the models is indicated by dark and light grey shadings (one and two standard deviations, respectively). A 10-year running mean is applied before calculating the spread. To account for mean state biases, all trends are evaluated relative to the 1950-1970 baseline. SST anomalies are estimated for the following regions: (a) Equatorial Indian Ocean: 40o E - 100o E. (b) Equatorial Atlantic: 50oW - 20o W. (c) North Pacific: 120o E to 120o W, 20o N to 65o N. (d) Equatorial West Pacific: 150o E - 180o E. (e) Equatorial East Pacific: 180o E - 80o W. Equatorial variables are averaged between 5o S -5o N.