Fig. 11
From: A dataset of gridded precipitation intensity-duration-frequency curves in Qinghai-Tibet Plateau
The modelling results of normalized PC1 (a) and normalized PC2 (b) by using different variables for the leave-one-out validation. The length of the error bar is equal to the standard deviation of MSE. Note that the number of samples to calculate MSE is 202, which is different from that (i.e., 203) in Fig. 8a,b.
