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Table 8 Model comparisons between the ETAS model with and without the triggering effect

From: Measuring seismicity diversity and anomalies using point process models: case studies before and after the 2016 Kumamoto earthquakes in Kyushu, Japan

 

μ

K 0

C

Α

P

K M7.3

c M7.3

P M7.3

ΔAIC

S2

ETAS

0.0231

1.440

0.00301

1.353

1.222

− 5.23

S2 

Equation 2

0.0170

2.494

0.0196

1.586

1.301

0.130

0.153

1.391

S3

ETAS

0.00561

5.381

0.0257

4.187

1.573

+ 2.51

S3 

Equation 2

0.00531

5.072

0.0251

3.031

1.244

1.04 × 10−4

0.380

1.520

  1. The MLEs of the reference ETAS model and the ETAS model with triggering effect (Eq. (2)) are listed with the AIC differences between the two models