Fig. 2.

Lowest-frequency patterns of change in daily temperature variability from individual CMIP-6 climate models under greenhouse forcing (1950–2015: historical; 2015–2100: SSP-585), detected with LFCA. Results from 5 of the 10 models are shown for the annual (A–F), the boreal winter (DJF; G–L), and the boreal summer (JJA; M–R) response; see SI Appendix, Fig. S6 for the remaining 5 models. Interdecadal changes (1950–1960 to 2090–2100) due to the lowest-frequency component (Materials and Methods) are shown as colored maps, the time evolution of which are shown in the bottom panels in gray, with a 10-y running mean in black.