Fig. 24: Change of the probability distribution function of sea surface temperature anomalies in the Niño 3.4 region for 2071–2100 (red line). Compared to 1870–2014 (black and blue lines), extreme anomalies become more likely while the probability of low to medium anomalies decreases. The range of the model results is shaded. ENSO asymmetry (positive skewness) decreases compared to 1870-2014 (see Fig. 5). All data have been linearly detrended and the seasonal cycle has been removed.
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