Fig. 4
From: Spatial variation of the rain–snow temperature threshold across the Northern Hemisphere
Success rates for the different precipitation phase methods ordered by average success rate with the best performing methods at the top. The success rate value is equal to the percentage of precipitation phase observations correctly simulated by the precipitation phase method. Low success rate values (dark red) correspond to a high frequency of misidentified precipitation phase observations. a Success rate plotted by Ts. b Success rate plotted by RH. Details on the different methods and average success rates are available in Supplementary Table 3
