Fig. 5: Sensitivity of compound climate extremes to the snow droughts with 1-month lag. | Communications Earth & Environment

Fig. 5: Sensitivity of compound climate extremes to the snow droughts with 1-month lag.

From: Snow droughts amplify compound climate extremes over the Tibetan Plateau

Fig. 5

Spatial distribution of the sensitivity of CDHE to DSD (a) and CPHE to WSD (b), where insets show the proportion of areas with positive and negative sensitivities. Values 66.6% and 69.5% indicate the spatial coverage with non-significant coincidence rates for DSD & CDHE and WSD & CPHE associations, respectively (p ≥ 0.05). Latitudinal gradient of the sensitivity of CDHE to DSD (c) and CPHE to WSD (d).

Back to article page