Skip to main content

Table 1 The area under the curve and accuracy of models’ responses in sampling ratios for the combination zone including plain and mountain (PM) and for the mountainous only zone (M)

From: The performance of using an autoencoder for prediction and susceptibility assessment of landslides: A case study on landslides triggered by the 2018 Hokkaido Eastern Iburi earthquake in Japan

ZoneModelSampling ratio (Sampling numbers)Area under the curve on test data setAccuracy
Precision & RecallTPR & TNRTPR & FPR
Combination zone including plain and mountain (PM)PM 11:1 (5627:5627)0.9370.9480.8910.892
PM 21:2 (5627:11254)0.9380.9680.9070.911
PM 31:3 (5627:16881)0.9030.9670.9150.920
PM 41:4 (5627:22508)0.8330.9570.9050.916
PM 51:5 (5627:28135)0.8540.9670.9110.932
PM 61:10 (5627:56270)0.7540.9640.9100.943
Mountainous zone (M)M 11:1 (5627:5627)0.9410.9510.8910.892
M 21:2 (5627:11254)0.8970.9520.8860.894
M 31:3 (5627:16881)0.8720.9520.8870.894
M 41:4 (5627:22508)0.8450.9490.8810.910
M 51:5 (5627:28135)0.8000.9490.8830.918
M 61:10 (5627:56270)0.7100.9560.8930.940