Fig. 6: Spatiotemporal pattern of temperature change.
From: Temperature overshoot responses to ambitious forestation in an Earth System Model
The differences in 10th percentile (low temperature extremes, left), mean (mid), and 90th percentile (high temperature extremes, right) of 2 m air temperature between AR and REF simulations during 2030–2050 (top), the period around peak warming (2050–2070) (mid), and end-of-century (2090–2100) are shown. A negative difference (blue color) indicates that temperature is lower in the AR scenario. Dots indicate regions where the difference is statistically insignificant at the 5% level, estimated with a two-tailed Student’s t-test after correcting for lag-1 temporal autocorrelation123 (see ”Methods”).
