Geology Reference
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are approximately 1.82/ M apart on the frequency axis. If the true spectral density
varies only slightly over this range of frequencies,
E S gg, n ( f )
S gg ( f ),
(2.361)
and the estimator, on average, gives an unbiased estimate of the true spectral
density.
In the overlapping segment analysis, the final spectral density estimate, S gg ( f ),
is taken as the average of the estimates (2.360) over κ overlapping segments of
length M of a complete record of length T . Thus,
κ
κ
S gg, j ( f )
S gg ( f )
1
κ
1
κ
S gg ( f )
S gg, j ( f )
=
=
+
S gg ( f ).
(2.362)
j = 1
j = 1
The variance of the final spectral density estimate is then
E S gg ( f )
S gg ( f ) 2
var S gg ( f )
=
E S gg, j ( f )
S gg ( f )
κ
κ
S gg ( f ) S gg, k ( f )
1
κ
=
.
(2.363)
j = 1
k = 1
The process generating g( t ) is assumed to be stationary, so that the terms in the
double sum depend only on the unsigned di
ff
erence of the indices j and k . Taking
m as the non-negative value of this di
ff
erence, the double sum can be rearranged
to give
var S gg ( f )
var S gg, n ( f )
1
κ
=
κ 1
m ) cov S gg, n ( f ),
S gg, n + m ( f ) ,
2
κ
+
(2.364)
2
m = 1
where the covariance of S gg, n ( f )and S gg, n + m ( f )is
E S gg, n ( f )
S gg ( f )
cov S gg, n ( f ),
S gg, n + m ( f )
S gg ( f ) S gg, n + m ( f )
=
E S gg, n ( f ) S gg, n + m ( f )
E S gg, n ( f ) 2
=
, (2.365)
recognising that both E S gg, n ( f ) and E S gg, n + m ( f ) are
S gg ( f ).
To evaluate the covariance, we require the expected value of the product of a
spectral estimate based on a window w n ( t ) of the data centred at b n on the time
 
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