Geoscience Reference
In-Depth Information
and (
9.33
) may be evaluated prior to the actual implementation of the model
R
in the
DAS and provide insight on the potential forecast gain at a reduced computational
effort.
9.3.2.2
Forecast B-Sensitivity and Impact Estimation
From (
9.5
)and(
9.65
), the first order variation in the
K
operator associated with a
variation
ı
B
in the background error covariance model
B
is expressed as
BH
T
HBH
T
1
BH
T
HBH
T
1
H
BH
T
HBH
T
1
ı
K
D
ı
Œ
C
R
Œ
C
R
ı
Œ
C
R
BH
T
HBH
T
1
D
Œ
I
KH
ı
Œ
C
R
(9.34)
An explicit relationship between
ıe
and
ı
B
is obtained by replacing (
9.34
)in(
9.23
),
@e
@
BH
T
HBH
T
1
Œ
x
b
/
ıe
D
x
a
;Œ
I
KH
ı
Œ
C
R
y
h
.
R
n
@e
@
T
BH
T
HBH
T
1
Œ
x
b
/
D
Œ
I
KH
x
a
;ı
Œ
C
R
y
h
.
(9.35)
R
n
With the aid of (
9.6
)and(
9.20
), (
9.35
) may be expressed as
@e
@
BH
T
z
ıe
D
x
b
;ı
(9.36)
R
n
From (
9.36
)and(
9.62
), the forecast
B
-sensitivity is the rank-one matrix
H
T
z
T
@e
@
B
D
@e
2
R
n
n
(9.37)
@
x
b
A first order assessment of the forecast performance of a new background error
covariance model
B
, as compared with the model
B
in the DAS, may be obtained
B
D
B
B
in (
9.36
),
by setting
ı
/
Œı
H
T
z
T
@e
@
x
a
.
B
x
a
.
eŒ
/
eŒ
B
B
(9.38)
x
b
Having available the
x
b
-sensitivity vector defined as in (
9.20
), the evaluation
of the first order impact estimate (
9.38
) may be performed prior to the actual
implementation of the model
B
in the DAS at a computational cost roughly
equivalent to the cost of a post-multiplication operation (
9.7
).
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