Fig. 7: Maps of the best temporal RFI estimates.
From: Changes in temporal inequality of precipitation extremes over China due to anthropogenic forcings

The best temporal RFI estimates were calculated based on the bootstrapping procedure for a PRCPTOT, c SDII, e R95p, and g RX5day over eight regions in China. b, d, f, h The uncertainty range (5th to 95th percentile) of RFI and the horizontal line in the box represents the best estimate (i.e., median value). The subfigures were done in the software R 4.0.2 (https://cran.r-project.org/bin/windows/) and then the subfigures were merged by using the Microsoft PowerPoint 2013 software (https://www.microsoft.com/).