Geoscience Reference
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Fig. 9.2 Flow chart of the
relationship between the
forecast aspect and various
input components of the data
assimilation system
o
Σ
y
R
o
a
C
a )
K
x
e ( x
b
Σ
b
B
x
b
C
parameters. The DAS operator K incorporates both R and B models and from ( 9.4 )
the analysis variation induced by a perturbation in the K operator is expressed as
x a D ı
x b /
ı
K
Œ
y h
.
(9.22)
By replacing ( 9.22 )in( 9.17 ), the first order forecast variation
ıe
is expressed in
terms of
ı
K as
@e
@
x b /
ıe D
x a
K
Œ
y h
.
(9.23)
R n
From ( 9.23 )and( 9.62 ), the forecast sensitivity to the K operator is the rank-one
matrix
@e
@
K D @e
x b /
T
2 R n p
x a Œ
y h
.
(9.24)
@
To obtain the forecast sensitivity to the error covariance specification it is necessary
to analyze how the K operator responds to variations in R and B . Additionally, each
covariance model incorporates a diagonal matrix
whose entries are the values
assigned to the error standard deviation and an error correlation model C ,
˙
R D ˙ o C o ˙ o ;
B D ˙ b C b ˙ b
(9.25)
A flow chart of the functional dependence of the forecast aspect on various DAS
input components is illustrated in Fig. 9.2 and the extension of the adjoint-DAS
applications to parameters in the error covariance specification is discussed next.
9.3.2.1
Forecast R-Sensitivity and Impact Estimation
From ( 9.5 )and( 9.65 ), the first order variation in the K operator induced by a
variation
ı
R in the observation error covariance model R is expressed as
K D BH T
HBH T
1 ı
HBH T
1 D K
HBH T
1 (9.26)
ı
Œ
C R
R
Œ
C R
ı
R
Œ
C R
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