Extended Data Fig. 1: Projected changes in climate variables over the Tibetan Plateau up to 2100.
From: Climate change threatens terrestrial water storage over the Tibetan Plateau
(a) Annual average temperature, (b) annual precipitation, and (c) annual surface short-wave radiation for the 2002–2100 period were estimated by the ensemble mean of nine CMIP6 models under SSP1-2.6, SSP2-4.5, and SSP5-8.5 scenarios. Both temperature and surface short-wave radiation were bias corrected using the delta approach, and precipitation was corrected using the quantile mapping approach. Shadows represent uncertainty range of ±1 standard deviation among outputs from different models.
