Environmental Engineering Reference
In-Depth Information
6.3.4.2 Projection
Owing to the orthogonality of the PC basis ( Equation 6.11 ), one can compute each expan-
sion coefficient as follows:
δ αβ
[
] =
=
(6.24)
E
Y
Ψ
()
X
E
Ψ
()
X
y
Ψ
()
X
=
y
E
Ψ
() ()
X
Ψ
X
y α .
α
α
β
β
β
α
β
M
M
β∈
β∈
Thus, each coefficient y α is nothing but the orthogonal projection of the random response
Y onto the corresponding basis function Ψ α ( X ). The latter may be further elaborated as
[
] =
y
=
E Ψ
Y
()
X
M
() () () .
x xxx
X
Ψ
f
d
(6.25)
α
α
α
D X
The numerical estimation of y α may be carried out with either one of the two expressions,
namely:
• By MCS allowing one to estimate the expectation in Equation 6.25 (Ghiocel and
Ghanem, 2002). This technique however shows low efficiency, as does MCS in general;
• By the numerical integration of the right-hand side of Equation 6.25 using Gaussian
quadrature (Le Maître et al., 2002; Berveiller et al., 2004a; Matthies and Keese, 2005).
The quadrature approach has been extended using sparse grids for a more efficient inte-
gration, especially in large dimensions. The so-called stochastic collocation methods have
also been developed. The reader is referred to the review paper by Xiu (2009) for more
details.
6.3.4.3 Least-square minimization
Instead of devising numerical methods that directly estimate each coefficient from the
expression y α = E[ Y Ψ α ( X )], an alternative approach based on least-square minimization
and originally termed “regression approach” has been proposed in Berveiller et al. (2004b,
2006). The problem is set up as follows. Once a truncation scheme A M is chosen (for
instance, A = A M,p as in Equation 6.18 ), the infinite series is recast as the sum of the trun-
cated series and a residual:
Y
=
M
()
X
=
y
X
αα
Ψε,
()
+
(6.26)
α∈
A
in which ε corresponds to all those PC polynomials whose index α is not in the truncation
set A . The least-square minimization approach consists of finding the set of coefficients
y = { y α , α ∈ A } that minimizes the mean-square error
2
def
E
[]
ε
2
=
E
Y
y
α Ψ X
()
,
(6.27)
α∈
A
 
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