Geoscience Reference
In-Depth Information
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
;ı
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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