Chiou and Youngs PEER-NGA Empirical Ground Motion Model for ...
Chiou and Youngs PEER-NGA Empirical Ground Motion Model for ...
Chiou and Youngs PEER-NGA Empirical Ground Motion Model for ...
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MODEL PARAMETER DEVELOPMENT<br />
The general <strong>for</strong>m of the ground motion model used to assess the model parameters is shown<br />
in Equation (16):<br />
f<br />
Source<br />
f<br />
= c (<br />
Path<br />
f<br />
HW<br />
2<br />
4<br />
9<br />
[ y ]<br />
[ 1+<br />
exp{<br />
c ( c − M ) } ]<br />
3<br />
M n M<br />
= c ln<br />
b<br />
2 2<br />
[ RRUP<br />
+ c5<br />
cosh{<br />
c6<br />
max( M − cHM<br />
, 0 ) } ] + ( c4a<br />
− c4<br />
) × ln[<br />
RRUP<br />
+ cRB<br />
]<br />
= φ ×<br />
[ c + c / cosh{<br />
max( M − c , 0}<br />
]<br />
tan<br />
/ 2 ) ×<br />
⎧ ⎡ VS<br />
30 ⎤ ⎫<br />
= φ1<br />
min⎨ln<br />
⎢<br />
0⎬<br />
+<br />
⎩ ⎣1130⎥<br />
, b<br />
⎦ ⎭<br />
2<br />
γ 1<br />
1130<br />
⎛ c2<br />
− c ⎞<br />
− 6 ) + ⎜<br />
⎟ × ln<br />
⎝ cn<br />
⎠<br />
f<br />
⎧ W cos( δ ) ⎫<br />
⎨ ⎬<br />
⎩2(<br />
ZTOR<br />
+ 1)<br />
⎭ ⎧<br />
× ⎨1−<br />
π / 2 ⎩ R<br />
{ ln[ y ] }<br />
[ exp{<br />
φ ( min( V , 1130 ) − 360)<br />
} − expφ<br />
( 1130 − 360)<br />
]<br />
3<br />
] = c<br />
γ 2<br />
2<br />
= c cos ( δ ) × tanh( R<br />
Site<br />
Site<br />
ln<br />
ln[ y<br />
Surface<br />
RUP<br />
= ln[ y<br />
1<br />
+<br />
f<br />
S 30<br />
1130<br />
Source<br />
] + f<br />
−1<br />
R ⎫<br />
JB<br />
⎬<br />
+ 0.<br />
001⎭<br />
− 4 )<br />
C&Y2006 Page 33<br />
+<br />
Site<br />
f<br />
Path<br />
Site<br />
+<br />
γ 3<br />
+ σ ⋅ z<br />
f<br />
HW<br />
+ c<br />
+ τ ⋅ z<br />
1a<br />
× R<br />
ij<br />
F<br />
RUP<br />
3<br />
RV<br />
+ c<br />
1b<br />
F<br />
NM<br />
RUP<br />
⎡ exp 1130 + φ ⎤ 4<br />
ln⎢<br />
⎥<br />
⎣ φ4<br />
⎦<br />
i<br />
+ c ( Z<br />
The parameter y1130 is the ground motion on the reference site condition (VS30 = 1130 m/sec).<br />
Its level is based on the source scaling function fSource, the path scaling function, fPath, the<br />
hanging wall function fHW, <strong>and</strong> a r<strong>and</strong>om effect τ zi that is modeled as a Gaussian r<strong>and</strong>om<br />
variate with inter-event st<strong>and</strong>ard deviation τ. The log of the ground motion at a site is the<br />
sum of the log of the reference motion <strong>and</strong> a nonlinear amplification, fSite, that is a function of<br />
VS30 <strong>and</strong> the level of the reference motion. The ground motions at the site also include a<br />
r<strong>and</strong>om Gaussian variate with intra-event st<strong>and</strong>ard deviation σ. The inter-event component<br />
of r<strong>and</strong>omness in included when computing the site amplification. Also note that the site<br />
amplification function uses the reference motion <strong>for</strong> the same spectral period. The additional<br />
parameters in Equation (16) are: RRUP , closest distance to the rupture plane (km); RJB ,<br />
Joyner-Boore distance to the rupture plane (km); δ , rupture dip; W , rupture width (km); ZTOR<br />
, depth to top of rupture (km); FRV , reverse faulting factor equal to 1 <strong>for</strong> 30º ≤ λ ≤ 150º, <strong>and</strong> 0<br />
otherwise; FNM , normal faulting factor equal to 1 <strong>for</strong> -120º ≤ λ ≤ -60º, 0 otherwise; λ , slip<br />
rake angle; VS30 , average shear wave velocity <strong>for</strong> top 30 m (m/s). Note, fHW applies to all<br />
faulting styles.<br />
The model parameters were obtained by fitting the model to the selected <strong>PEER</strong>-<strong>NGA</strong> data<br />
using the nonlinear mixed effects method nlme implemented in the statistical packages S-<br />
Plus <strong>and</strong> R. The process used to obtain these parameters is described below.<br />
7<br />
TOR<br />
+<br />
(16)