Geoscience Reference
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the observation error correlation will slightly increase the observation influence and
for
¢ o ¢ b
the observations will not be more influent in the analysis despite R is
not diagonal.
(i) R diagonal and B non-diagonal (
˛ ¤ 0; ˇ D 0
) . Equations ( 4.24 )and( 4.25 )
reduce respectively to
r C 1 ˛ 2
r 2 C 1 ˛ 2 C 2r
S 11 D S 22 D
(4.26)
r 2 C 1 ˛ 2 C 2r
S 12 D S 21 D
(4.27)
It can be seen that if the observations are very close compared to the scale-length
of the background error correlation, i.e.
' 1
(data dense area), then
1
r C 2
S 11 D S 22 D S 12 D S 21 '
(4.28)
Furthermore, if
¢ b
D ¢ o ,thatis
r D 1
, we have three pieces of information
with equal accuracy and S 11 D
S 22 D 1=3
. The background sensitivity at both
locations is
1 S 11 D 1 S 22 D 2=3
. If the observation is much more accurate
than the background (
¢ b >> ¢ o /
,thatis
r 0
, then both observations have
influence S 11 D
S 22 D 1=2
, and the background sensitivities are
1 S 11 D
1 S 22 D 1=2
.
Let's now turn to the dependence on the background-error correlation
'
,forthe
case
¢ b
D ¢ o .
r D 1/
.Itis
S 11 D S 22 D 2 ˛ 2
4 ˛ 2
(4.29)
˛
4 ˛ 2
S 12 D S 21 D
(4.30)
If the locations are far apart, such that
' 0
,thenS 11 D S 22 D 1=2
, the background
sensitivity is also
. It can be concluded that where observa-
tions are sparse, S ii and the background-sensitivity are determined by their relative
accuracies (
1=2
and S 12 D S 21 D 0
) and the off-diagonal terms are small (indicating that surrounding
observations have small influence). Conversely, where observations are dense, S ii
tends to be small, the background-sensitivities tend to be large and the off-diagonal
terms are also large.
It is also convenient to summarize the case
r
¢ b
D ¢ o .r D 1/
by showing the
projected analysis at location
1
.2 ˛ 2 /y 1 C 2x 1 ˛.x 2 y 2 /
1
4 ˛ 2
y 1 D
(4.31)
 
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