Extended Data Fig. 5: Trends in climate drivers over the Tibetan Plateau during 2002–2017.
From: Climate change threatens terrestrial water storage over the Tibetan Plateau

Precipitation, temperature, and surface short-wave radiation are analyzed during (a–c) annual, (d–f) summer (June–August), and (g–i) winter (December–February) periods. Stippling marks regions that have a significant trend (the Mann-Kendall test at a 5% significance level). Precipitation data were derived from Integrated Multi-satellitE Retrievals for GPM (IMERG) V06, and temperature and radiation data were derived from reanalysis ERA5 data.