Title: THE 2004 GIANT SUMATRA EARTHQUAKE AND TSUNAMI
1THE 2004 GIANT SUMATRA EARTHQUAKE AND TSUNAMI
Barbara ROMANOWICZ Univ. of California at Berkeley
2Alaska 1964 M 9.2
3Aleutians 1946 (M7.8) (Hilo)
4Lisbon (1755)
512/26/04 Sumatra eq. Mw 9.0
1300 km rupture zone 15-20m of slip shaking
lasted -8 mn
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10WORLDWIDE EARTHQUAKES PER YEAR
Frequency-magnitude relationship suggests that
magnitude 9 events will occur about once per
decade since 1900, the actual number is once
per 20 years.
11LARGEST EARTHQUAKES, 1900 - 2004
12LARGEST EARTHQUAKES, 1900 - 2004
9.3
USGS
13Mo rigidity x slip x rupture area (N-m)
Harvard CMT group
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15Some recent Tsunami
NOAA
16The Geophysical Context
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22COMPLEX PLATE BOUNDARY ZONE IN SOUTHEAST
ASIA Northward motion of India deforms all of
the region Many small plates (microplates) and
blocks
Molnar Tapponnier, 1977
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24INTERSEISMIC India subducts beneath Burma
microplateat about 5 cm/yr, of which 3 cm/yr is
convergence Fault interface is
locked EARTHQUAKE (COSEISMIC) Fault interface
slips, overriding plate rebounds, releasing
accumulated motion
Stein Wysession, 2003
HOW OFTEN Fault slipped 12 m 1200 cm 1200
cm / 3 cm/yr 400 yr Longer if some slip is
aseismic
25Generic subduction zone cross section
26Earthquake generated tsunamis
27Tsunami wave propagation characteristics
NOAA
28Commonly, the water recedes (a wave trough)
significantly for a few minutes before the first
wave crest arrives. People often go out to
explore the beach at that time.
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30TSUNAMI TRAVEL TIME (HOURS SIMULATION)
NOAA
31TSUNAMI WARNING
- Earthquake waves travel 10 times faster than
tsunami - seismic velocities 6-8 km/s
- tsunami (deep sea) 600 km/h 0.6 km/s
- Seismology rapid earthquake location, size and
mechanism - deep sea buoys verify tsunami and provide alert
32Timeline
Origin Time 12/26/05 0058 UTC
PTWC Alarm
10 min
USGS SP Alarm
Initial USGS Loc (mb6.2) PTWC Bulletin (Mwp8.1)
20 min
USGS Released Auto Loc (mb6.3, n132) USGS Auto
MT (Mw8.2)
30 min
Time since OT
40 min
USGS Reviewed MT (Mw8.2)
50 min
PTWC Bulletin M8.5
60 min
70 min
USGS Reviewed Loc (Ms8.5, n157) Sent 25,000
emails, calls to White House, State Dept.,
Embassies, etc.
80 min
33TSUNAMI WARNING
Because seismic waves travel much faster (km/s)
than tsunamis, rapid analysis of seismograms can
identify earthquakes likely to cause major
tsunamis and predict when waves will arrive
Deep ocean buoys can measure wave heights, verify
tsunami and reduce false alarms
34Historical Seismicityandfuture earthquakes
35COMPARISON WITH PREVIOUS RUPTURES
BILHAM, 2005
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37Stress change after the 12/26/04 Sumatra
earthquake
McCoskey et al.,2005
38Current and future seismological investigations
39Stein Wysession after IRIS
One of the largest earthquakes since seismic
recording The largest since the deployment of
modern broadband instrumentation
40STS-1 seismometers
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42Ni et al., Nature, 2005
43MODELING SEISMOGRAMS shows how slip varied on
fault plane Maximum slip area 400 km
long Maximum slip 20 m
Stein Wysession
44After Park et al, 2005
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47(0.8 to 2.2 mHz)
Sumatra 12/26/04
CAN
1S5
3S2
1S4
UNM
0S12
0S9
0S8
0S7
0S10
0S11
0S0
0S5
1S3 /3S1
0S6
200 hours starting 10 hours before origin time
48Mode 23S5
Bolivia 06/09/94
Ritzwoller et al., 1988
49oS2
oSo
oS3
After Park et al, 2005
(53.9 min) (25.7 min) (20.5
min)
50Sumatra-Andaman earthquake 26 December 2004 CAN
G station (STS1)
20.9 dr0.05mm
25.7
0S2
53.9
0S3
0S0
3S1 2S2 1S3
0S4
44.2
0S5
1S2
0T2
2S1
0T3
0T4
Courtesy of G. Roult, IPGP
510S3
2S1
0T2
0S2
Courtesy of G. Roult
52mode 0S2 5 singlets
Courtesy of G. Roult, IPGP
53mode 0S3 7 singlets
Courtesy of G. Roult, IPGP
540S2
0S3
Preared by A.Cao, BSL
55Mo 1030 dyne-cm Mw 9.3
0S2
Stein and Okal, Nature, 2005
56Stein and Okal, 2005
57ARU
RPN
58ARU Distance 6705 km Azimuth 337o
Dec. 04 event
March05 event
R1
R2
R3
Source Directivity effect
J. Rhie, BSL
59RPN Distance 16360 km Azimuth 137o
Dec.04 event
March05 event
R1
R2
60COULD IT HAVE HAPPENED HERE?TSUNAMIS IN SAN
FRANCISCO BAY
- Local
- Possible tsunamis in 1854, 1856, 1868, 1887
- 1898 Mare Island Earthquake (M 6-6.5)
- 1906 San Francisco Earthquake (M 7.8)
- Tele-tsunamis
- 1960 Chilean (M9.5)
- 1964 Good Friday Alaska (M9.2)
61California Integrated Seismic Network subset o
f Berkeley and Caltech broadband stations
62Courtesy of D.Dreger, UCB
632003 San Simeon earthquake
- Finite-source models show a shallow rupture
extending 25 km SE of the epicenter. - The finite-source parameters were used to update
ShakeMap the day of the earthquake greatly
improving strong shaking estimates in the most
heavily impacted areas.
Dreger, 2004
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65Mode attenuation
mode 0S0
Q 5300
30
10
20
mode 0S2 singlet m2
Q 500
Station CRZF, Crozet, Indian Ocean
Courtesy of G. Roult, IPGP
66Anomalous splitting of core modes
With inner core anisotropy
Durek and Romanowicz, 1999
67Mantle mode
CMB
ICB
Core mode
CMB
ICB
Ritzwoller et al. database
68THE END
69EPS 20 Earthquakes
70Interesting Effects of Earthquake Change in
length of day -2.68?sec Change in oblateness
10E-9 Shift of North Pole 2.5 cm 145E (As
calculated by Chao and Gross of NASA Goddard and
JPL)
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75 mode 0S0, decay of amplitude with time
period
period
CRZF
PAF
f 0.81465203 1/Q 0.1813
f 0.81465942 1/Q 0.1805
76Chen Jis Modeled Surface Displacements
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78Stein and Okal, 2005
79Source ??
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84High frequency
Low frequency
85With inner core anisotropy
Durek and Romanowicz, 1999
8611/03/02 Denali Earthquake Dreger et al, 2003
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89Chile earthquake, 1960 May 22th, recorded at
Paris (IPGP) with an inclinometer
90Kinematic Modeling of the Denali Earthquake
- Regional distance seismic and GPS data were
inverted for kinematic slip parameters (e.g.
Dreger et al., 2004 Oglesby et al., 2005). - Slip is mostly shallow with 4 primary asperities.
- Rupture velocity is fast on average.
- Simulated PGV correlates with the occurrence of
liquefaction features (e.g. Kayen et al., 2004) - Continuing efforts include updating the kinematic
model using the recently released GPS data set,
and examining implications for using finite
source parameters in ShakeMap.
Dreger 2004
91AFFECTED COUNTRIES
BBC
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95Bolivia 06/09/94 Mw8.2 h647 km station BKS
Kuril 10/04/94 Mw8.3 h58 km station BKS
96Most recent large event 7.9 - 2000 Previous
events gtM8 1861- 8.5 1833 - 8.7 1797 -
8.4 Tsunamis 1797 1833 1843 1861 1881 1883
- Krakatau! 1907 1941 2004