Extended Data Fig. 3: Relationship between ENSO amplitude change and zonal SST difference.
From: Mid-Pliocene El Niño/Southern Oscillation suppressed by Pacific intertropical convergence zone shift
Zonal SST change evaluated as the difference between the cold tongue (5°S-5°N; 120°W-100°W) and warm pool regions (5°S-5°N; 150°E-170°E) in the equatorial Pacific. PlioMIP1 models are represented by magenta squares while PlioMIP2 models are represented by red circles.
