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Application of SASHA for Mt. Etna case
Task D: Probabilistic Hazard Assessment
Salvatore D'Amico
Istituto Nazionale di Geofisica e VulcanologiaOsservatorio Etneo, Catania (Italy)
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
Regional and local seismicity at Mt. Etna
• Mt. Etna area is affected by strong regional earthquakes,
• but also by shallow local earthquakes due to volcano-tectonic faults.
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
Features of volcano-tectonic earthquakes Moderate magnitude
ML ≤ 5.0
High values of epicentral intensityI0 ≤ X EMS
Shallow depth sources H < 2 km b.s.l.
Coseismic surface faulting
Strong attenuation of the macroseismic intensity ∆I = 4 in 20 km(~70 km in tectonic areas)
Macroseismic Catalogue of Mt. Etna from 1832 to 2008
Azzaro et al. (2009) http://www.ct.ingv.it/ufs/macro/critical parameter
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
1
2
3
X X
XLo
cal
Reg
ion
al
50 yrs exposure time10% probability
The process to compute PSHA by SASHA
Local seismicity
Short exposure times10, 30 years
The “site approach” performs a Poissonian PSHA using the seismic history at a site, i.e. the dataset of macroseismic intensities available for a given locality
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
Database and Catalogue
• 4432 macroseismic observations– Statistical estimation on site
• 415 localities (Villages, towns, etc.)
• from 1566 to 2008• Imax IX-X EMS
• 140 earthquakes• from 1000 to 2008• Io EMS (VI - XI-X)• M (3.4 - 4.7)
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
Probabilistic Results of Task B
Estimation of probability distributions of
the intensity at a site, given the epicentral
intensity I0 and the site-epicenter
distance, through a binomial-beta model.
I0 = VIIII0 = IX
(Azzaro et al., 2012)
Intensity attenuation at Etna
Point sources
Isotropic model
Linear sources
Anisotropic model15 earthquakesIo > VII
IX 6.1488 0.6076VIII 3.9251 0.5175VII 10.4333 1.1037
IX 1.1844 0.2501VIII 2.1534 0.3654VII 3.0629 0.4248VI 0.9872 0.239
125 earthquakesIo > VI
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
1915 Linera Earthquake: Io IX-X – M 4.7
Isotropic Vs Anisotropic model
Isotropic model Anisotropic model
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
PSHA Map: attenuated dataIsotropic model Anisotropic model
Exp
osu
re t
ime:
30
yrE
xpo
sure
tim
e: 1
0 yr
Difference: Iso-Ani
10% prob.
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
PSHA Map: felt + attenuated dataIsotropic model Anisotropic model
Exp
osu
re t
ime:
30
yrE
xpo
sure
tim
e: 1
0 yr
10% prob.
Difference: Iso-Ani
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
0
Fiandaca
Moscarello
Pernicana
S. Tecla
Tremestieri
0.0 0.5 1.0 1.5 2.0 2.5
4.5
4
3.5
Hazard deaggregation: Zafferana (Iexp: VIII) 37.6920 15.1040 7 ZAFFERANA_ETNEA
3002 1832 11 24 37.6160 15.0260 3.70 7.00 11. 0.01
3004 1850 1 1 37.6170 14.9230 3.90 7.50 18. 0.01
3005 1855 1 26 37.7240 15.1470 3.90 7.50 5. 0.12
3015 1865 7 19 37.7020 15.1530 4.50 9.00 4. 0.54
3056 1875 1 7 37.6260 15.1360 3.70 7.00 8. 0.02
3100 1881 2 12 37.7100 15.1680 3.70 7.00 6. 0.04
3146 1883 3 22 37.6530 15.0650 4.10 8.00 6. 0.50
3151 1883 3 22 37.6020 15.0030 3.70 7.00 13. 0.01
3171 1883 3 26 37.6120 15.0280 3.50 6.50 11. 0.01
3204 1883 4 28 37.6130 15.0280 3.50 6.50 11. 0.01
3225 1883 6 24 37.7050 15.1210 3.70 7.00 2. 0.50
3270 1885 9 25 37.6140 15.0270 3.70 7.00 11. 0.01
3273 1885 10 2 37.6140 15.0260 3.50 6.50 11. 0.01
3614 1901 5 11 37.6170 15.0290 3.70 7.00 11. 0.01
3770 1908 5 9 37.6690 15.1650 3.50 6.50 6. 0.02
3951 1914 5 8 37.6590 15.1490 4.70 9.50 5. 0.50
4010 1918 11 24 37.6860 15.1400 3.50 6.50 3. 0.04
4062 1920 9 26 37.7130 15.1610 3.90 7.50 6. 0.08
4244 1935 6 30 37.6550 15.1570 3.50 6.50 6. 0.02
4254 1942 11 15 37.6140 15.0290 3.50 6.50 11. 0.01
4261 1950 4 8 37.7070 15.1640 3.90 7.50 6. 0.08
4286 1952 3 19 37.6600 15.1470 3.90 7.50 5. 0.50
4408 1971 4 21 37.7140 15.1480 4.10 8.00 5. 0.21
4500 1984 10 19 37.6940 15.1030 3.70 7.00 0. 1.00
4768 2002 10 29 37.8070 15.0720 3.50 6.50 13. 0.01
4769 2002 10 29 37.6490 15.1720 3.50 6.50 8. 0.01
6003 1633 2 22 37.6140 15.0260 3.90 7.50 11. 0.03
6010 1634 12 21 37.6140 15.0810 3.70 7.00 9. 0.02
6019 1669 3 10 37.6150 15.0140 3.70 7.00 12. 0.01
6020 1669 3 10 37.6140 15.0260 3.90 7.50 11. 0.03
6023 1669 3 11 37.6150 15.0140 3.70 7.00 12. 0.01
6080 1805 7 11 37.7180 15.1500 4.30 8.50 5. 0.25
0
Tremestieri
Moscarello
Moscarello
Fiandaca
S. Leonardello
Tremestieri
Tremestieri
Tremestieri
Tremestieri
Tremestieri
Moscarello
S. Tecla
S. Leonardello
Moscarello
Tremestieri
S. Leonardello
S. Tecla
Moscarello
S. Tecla
Pernicana
S. Tecla
Exposure time 30 yrs - 10% prob.
3.5 4.0 4.5
Magnitude
0
2
4
6
8
10
12
14
16
18
20
Dis
tan
ce
(k
m)
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
FaultsID YE MO DA LAT LON M Io DIST PROB
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
3.5 4.0 4.5
Magnitude
0
2
4
6
8
10
12
14
16
18
20
Dis
tan
ce
(k
m)
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Acireale (Iexp VI)
Hazard deaggregation
3.5 4.0 4.5
Magnitude
0
2
4
6
8
10
12
14
16
18
20
Dis
tan
ce
(k
m)
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Zafferana (Iexp VIII)
3.5 4.0 4.5
Magnitude
0
2
4
6
8
10
12
14
16
18
20
Dis
tan
ce
(k
m)
0
1
2
3
4
5
6
7
8
Nicolosi (Iexp VII)
0
Fiandaca
Moscarello
Pernicana
S. Tecla
Tremestieri
0.0 0.5 1.0 1.5 2.0 2.5
4.5
4
3.5
0
Fiandaca
Moscarello
Pernicana
S. Tecla
Tremestieri
0.0 1.0 2.0 3.0 4.0 5.0 6.0
4.5
4
3.5
0
Fiandaca
Moscarello
Pernicana
S. Tecla
Tremestieri
0.0 0.2 0.4 0.6 0.8 1.0
4
3.5
Exposure time 30 yrs - 10% prob.
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
Giardini-Naxos
Acireale
Adrano
Bronte
Catania
Giarre
Linguaglossa
Nicolosi
Randazzo
Tremestieri Etneo
Zafferana Etnea
• Variability of hazard at local scale along the volcano edifice
• High values (XIII - IX) of IEXP
• Main contribute to hazard by STF and MF
• Useful tool for establishing a priority of intervention for retrofit actions of urban areas.
• Identification of earthquakes to be used for scenario in Task F
Conclusions
Giardini-Naxos
Acireale
Adrano
Bronte
Catania
Giarre
Linguaglossa
Nicolosi
Randazzo
Tremestieri Etneo
Zafferana Etnea
Exp. time 30 yrs10% prob.
Exp. time 10 yrs10% prob.
MF
STF
UPStrat-MAFA 3rd General Meeting 23-26 July 2013, Selfoss, Iceland
Task D: Probabilistic Hazard Assessment: Application of SASHA for Mt. Etna case
Open questions and Suggestions
• Dependency of hazard from uncertainties in epicentral intensity
• Extensive use of the anisotropic model for all earthquakes with known seismogenic fault– Use of a "standard" size for linear
source for each Epicentral intensity class
Giardini-Naxos
Acireale
Adrano
Bronte
Catania
Giarre
Linguaglossa
Nicolosi
Randazzo
Tremestieri Etneo
Zafferana Etnea
Giardini-Naxos
Acireale
Adrano
Bronte
Catania
Giarre
Linguaglossa
Nicolosi
Randazzo
Tremestieri Etneo
Zafferana Etnea
Exp. time 30 yrs10% prob.
Exp. time 10 yrs10% prob.