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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

Zone

Model

Sampling ratio (Sampling numbers)

Area under the curve on test data set

Accuracy

Precision & Recall

TPR & TNR

TPR & FPR

Combination zone including plain and mountain (PM)

PM 1

1:1 (5627:5627)

0.937

0.948

0.891

0.892

PM 2

1:2 (5627:11254)

0.938

0.968

0.907

0.911

PM 3

1:3 (5627:16881)

0.903

0.967

0.915

0.920

PM 4

1:4 (5627:22508)

0.833

0.957

0.905

0.916

PM 5

1:5 (5627:28135)

0.854

0.967

0.911

0.932

PM 6

1:10 (5627:56270)

0.754

0.964

0.910

0.943

Mountainous zone (M)

M 1

1:1 (5627:5627)

0.941

0.951

0.891

0.892

M 2

1:2 (5627:11254)

0.897

0.952

0.886

0.894

M 3

1:3 (5627:16881)

0.872

0.952

0.887

0.894

M 4

1:4 (5627:22508)

0.845

0.949

0.881

0.910

M 5

1:5 (5627:28135)

0.800

0.949

0.883

0.918

M 6

1:10 (5627:56270)

0.710

0.956

0.893

0.940