Civil Engineering Reference
In-Depth Information
fractiles of the ground motion parameters at various probability levels can
be easily extracted to construct uniform hazard spectra.
A signifi cant advantage of using Monte Carlo simulation rather than
numerical integration to perform the hazard analysis is that it facilitates the
production of seismic deaggregation results at any probability level (i.e. to
show hazard contributions by magnitude and distance), because all infor-
mation that is needed for seismic deaggregation is kept throughout the
analysis. The process of constructing uniform hazard spectra and deaggrega-
tion results is illustrated in Fig. 1.5.
A further advantage of the simulation-based approach over conventional
numerical integration is transparency of the procedure. The calculation
steps are straightforward and intuitive: simulating earthquake time and
location, generating earthquake magnitude and fault dimensions, and then
estimating ground motion parameters for given earthquake characteristics.
Construction of uniform hazard spectra:
Reorganise the calculated response spectra values on the
annual maximum basis, and sort them in an ascending order
2.0
Uniform hazard spectra for Vancouver
Assign the annual probability of exceedance
Select the target probability level
Annual prob.
of exceedance
:
0.0021060
0.0021058
0.0021056
0.0021054
0.0021052
:
:
:
0.0004048
0.0004046
0.0004044
0.0004042
0.0004040
:
1.0
PGA
( g )
:
0.235
0.236
0.236
0.236
0.236
:
:
:
0.487
0.487
0.488
0.488
0.488
:
SA(0.2)
( g )
:
0.577
0.577
0.577
0.577
0.577
:
:
:
1.244
1.245
1.245
1.245
1.245
:
SA(0.5)
( g )
:
0.342
0.342
0.342
0.342
0.343
:
:
:
0.749
0.749
0.749
0.749
0.749
:
SA(1.0)
( g )
:
0.185
0.185
0.185
0.185
0.185
:
:
:
0.432
0.432
0.432
0.432
0.433
:
SA(2.0)
( g )
:
0.091
0.091
0.091
0.091
0.091
:
:
:
0.227
0.227
0.227
0.227
0.227
:
0.5
10% in
50 years
0.3
0.2
Exceedance probability
0.1
2% in 50 years
2% in
50 years
10% in 50 years
0.05
PGA
0.1
0.2 0.3
0.5
1.0
2.0 3.0
Vibration period for SA (s)
Construction of seismic deaggregation:
Each of the annual maximum response spectra values is associated
with an event in the synthetic earthquake catalogue
Reassemble magnitude and distance information for events with response
values exceeding the target value, and produce a histogram
Seismic deaggregation (PGA) for Vancouver
0.05
0.04
0.03
9.0
0.02
8.0
0.01
0.0
7.0
Moment
magnitude
0
50 100
Distance (km)
6.0
150
200
250 5.0
1.5 Construction of uniform hazard spectra and seismic
deaggregation.
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