Extended Data Fig. 9: The Random Forest snowpack reconstruction methodology exhibits high skill based on a perfect model framework.
From: Evidence of human influence on Northern Hemisphere snow loss
CMIP6 ensemble mean forced (HIST minus HIST-NAT) trends in March SWE from 1981–2020 based on (a) climate model SWE output and (b) SWE estimated using climate model temperature and precipitation and Random Forest model. c, Scatterplot of reconstructed versus original trends, where each dot represents a grid cell. Points are colored by their density. Dashed line denotes perfect agreement between reconstructed and original trends. Spatial correlation is shown in the bottom right corner.
