Fig. 1: Comparison of the spatiotemporal characteristics of SWE before and after applying the CDF-t statistical downscaling technique during the validation period from 1999 to 2014.
From: New insights from the bias-corrected simulations of CMIP6 in Northern Hemisphere’s snow drought
(a) shows the observed and simulated cumulative distribution functions of Northern Hemisphere mean SWE, both prior to and following the application of the CDF-t method. (b) presents the observed and simulated monthly mean NH SWE values, both prior to and following the application of the CDF-t methods. (c) shows the multi-year average spatial distribution of SWE for the GISS-E2-1-G model prior to using the CDF-t technique. (d) shows the multi-year average spatial distribution of SWE for the GISS-E2-1-G model after the application of the CDF-t method.
