Geoscience Reference
In-Depth Information
Equations ( 9.4 )and( 9.5 ) establish the relationship x a
x a .
x b ;
D
y
;
R
;
B
/
and
x a in ( 9.17 )intermsof
allow the expression of the first order analysis variation
ı
x b ;
variations in the DAS input components y
;
R ,and B .
9.3.1
Sensitivity to Observations and Background
Baker and Daley ( 2000 ) derived the equations of the forecast sensitivity with respect
to observations and background
@e
@
y D K T @e
(9.19)
@
x a
@e
@
@e
@
x a D @e
x a H T @e
I H T K T
x b D Œ
(9.20)
@
@
y
identity matrix. It is noticed that the x b -sensitivity
equation ( 9.20 ) is formally valid only for a linear observation operator, h
n n
where I denotes the
/ D Hx ,
since it neglects the dependence of the linearized observation operator ( 9.3 )on x b .
For the purpose of estimating the forecast sensitivity to background error covariance
parameters we will simply interpret ( 9.20 ) as a vector notation. Second order
derivative information or additional approximations are also necessary to evaluate
the observation sensitivity in a variational DAS with multiple outer loop iterations
( Daescu 2008 ; Tr emolet 2008 ).
The relationship
@e
@
.
x
x a x b
@e
@
x b / H
x a x b /
x b ;
R n D
y ;
y h
.
.
(9.21)
R p
may be established from ( 9.19 ), ( 9.20 ), and the analysis equations ( 9.4 ), ( 9.5 ) and its
significance to the parametric error covariance sensitivity is explained in Sect. 9.3.3 .
The evaluation of the observation sensitivity is currently integrated in the routine
activities at NWP centers to monitor the observing system performance using OBSI
measures such as ( 9.9 )and( 9.10 ). As shown below, the vectors ( 9.19 )and( 9.20 )
are also key ingredients to obtain information on the forecast R -and B -sensitivity,
respectively.
9.3.2
Forecast R -and B -Sensitivity and Impact Estimation
The forecast R -and B -sensitivity and impact estimation identifies those error
covariance parameters of potentially high forecast impact and provides guidance
on the forecast benefit that may be achieved from adjusting the error covariance
Search WWH ::




Custom Search