Fig. 2: Occurrence frequency and severity of dry snow drought (DSD) and warm snow drought (WSD) from 1979 to 2022.
From: Snow droughts amplify compound climate extremes over the Tibetan Plateau

Spatial distribution of annual mean occurrence frequency (a, c) and severity (b, d) of DSD and WSD, elevation dependency of snow drought occurrence frequency (e), and snow drought frequency under different moisture conditions (f).