Fig. 7: Spatiotemporal pattern of changes in hydroclimate.
From: Temperature overshoot responses to ambitious forestation in an Earth System Model
From left to right, the differences in mean precipitation (mm/day), evapotranspiration (mm/day), cloud cover fraction, and relative humidity (%) between AR and REF simulations during 2030–2050 (top), the period around peak warming (2050–2070) (mid), and end-of-century (2090–2100) (bottom) are shown. A negative value indicates a reduction 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”).
