Figure S1: Non-cumulative (gray histogram) and cumulative (black line) frequency distribution of landslide angle


Table S1. Adjusted p-values from multiple pairwise comparisons of slope angles (> threshold angle) using the Dunn's test. The analysis expected three grid cells, where most landslides occurred in areas affected by anthropogenic activities (e.g., slopes surrounding cropland and paddy field). The null hypothesis assumes no significant differences in slope conditions. A p-value higher than a significant level of 5 % leads to accept the null hypothesis. The test was applied after rejecting the null hypothesis of the Kruskal-Wallis static, which indicated significant differences in slope conditions within the extent of the R/A grid cells. 0.8 0.00 1.00 1.00 
1.04 1.00 0.00 0.00 1.00 
1.22 0.00 0.00 0.00 0.00 1.00 4.51 0.00 0.00 0.00 0.00 0.00 1.00 
2.81 0.00 0.00 0.00 0.00 0.00 0.00 1.00 
1.47 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 
1.97 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 
3.75 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 4.87 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 5.91 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 5.45 0.00 0.01 0.08 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 5.68 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 9.77 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 20.91 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 0.00 1.00 25.26 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 35.61 1.00 0.00 0.00 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 105.63 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 
103.88 0.00 0.00 0.00 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 1.00 

Figure S2 : 10 Figure S3 :Figure S5 : 20 Figure S8 :Figure S10 :

 S210S3S520S8S10 Figure S2: Rainfall intensity maxima over multiple timespans (1 -72 h) within the Pstd for the different landslide density grid cells (excluding three grid cells where landslide occurrence was deemed to be affected by anthropogenic activities). Dashed lines correspond to theoretical rainfall totals of 300, 800, and 1000 mm.