Geoscience Reference
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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
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
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
(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 .
/
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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