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Table 1 Tsunamigenic events for the SWIFT TSUNAMI system

From: Near-field tsunami forecast system based on near real-time seismic moment tensor estimation in the regions of Indonesia, the Philippines, and Chile

Event with M w

Date (yyyy-mm-dd)

Origin time (UTC)

Latitude (°N)

Longitude (°E)

Focal depth (km)

Fault planea

Strike (deg)

Dip (deg)

Rake (deg)

Scaling lawb

L (km)

W (km)

D (m)

Tsunami datac

Reference

DART

Tide Gauge

2012 M w 8.6 off Sumatra earthquake

2012-04-11

08:38:34

2.0

94.0

50

FP1

FP2

201

110

54

89

1

144

SC1

SC2

207

352

103

176

10.4

3.6

23227, 23401, 56001, 56003

1, 2, 4, 7

Duputel et al. (2012a)

2007 M w 8.5 Bengkulu earthquake

2007-09-12

11:10:23

−5.0

101.0

15

FP1

FP2

314

112

10

81

112

86

SC1

SC2

184

314

92

157

9.2

3.2

23401

6

Gusman et al. (2010)

2007 M w 7.7 aftershock of Bengkulu earthquake

2007-09-12

23:49:01

−2.7

100.6

30

FP1

FP2

325

126

27

64

107

82

SC1

SC2

73

125

36

62

3.7

1.3

23401

–

Gusman et al. (2010)

2010 M w 7.8 Sumatra earthquake

2010-04-06

22:15:03

2.3

96.5

20

FP1

FP2

306

127

7

83

89

90

SC1

SC2

82

140

41

70

4.1

1.4

23401, 56001

2, 3, 4, 6

–

2010 M w 7.5 Mentawai tsunami earthquake

2010-10-25

14:42:21

−4.0

99.8

10

FP1

FP2

308

97

31

63

117

75

SC1

SC2

58

99

29

49

2.9

1.0

56001

4, 5, 6, 7

Satake et al. (2013)

2012 M w 7.5 Philippine Trench earthquake

2012-08-31

12:47:38

10.8

127.0

40

FP1

FP2

346

206

56

41

65

122

SC1

SC2

58

99

29

49

2.9

1.0

52405, 52404, 52403

8

Heidarzadeh and Satake (2014)

2015 M w 8.4 Illapel earthquake

2015-09-16

22:54:29

−31.2

287.2

5

FP1

FP2

12

169

21

71

112

82

SC1

SC2

164

280

82

140

8.2

2.8

32402, 32401, 32412, 32411

14–31

Heidarzadeh et al. (2016)

2014 M w 8.1 Iquique earthquake

2014-04-01

23:46:49

−20.1

289.2

25

FP1

FP2

352

167

17

73

95

88

SC1

SC2

116

198

58

99

5.8

2.0

32401, 32402, 32412, 32413

9–16, 18, 19, 21

Gusman et al. (2015)

  1. aFP1 and FP2 are two fault planes because of the double couple
  2. b SC1 and SC2 indicate the scaling laws of Utsu (2001) and Murotani et al. (2013), respectively. Length (L), width (W), and slip amount (D) of a finite rectangular fault are given by these scaling laws using the M w
  3. a,b The initial tsunami height conditions of src01, src02, src03, and src04 shown in figures are yielded by the pairs of FP1/SC1, FP1/SC2, FP2/SC1, and FP2/SC2, respectively
  4. c The tsunami data stations are shown in Fig. 2. Selected tide gauge stations are located within a 2-h tsunami arrival time