Fig. 2: Difference in changes of extreme temperature return levels and changes in event coupling. | Nature Communications

Fig. 2: Difference in changes of extreme temperature return levels and changes in event coupling.

From: Changes in event soil moisture-temperature coupling can intensify very extreme heat beyond expectations

Fig. 2

a, c, e Difference between changes (2076–2100 vs. 1990–2014) in 200-year and 2-year return levels of daily maximum temperature TX for MPI-ESM1-2-LR (top), ACCESS-ESM1-5 (middle) and MIROC6 (bottom). Results for further return levels are shown in Supplementary Fig. S3. b, d, f Changes in the corresponding soil moisture-temperature coupling strength. Differences/changes in hatched regions are not significant at the 95% level (see Methods for detail).

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