Geoscience Reference
In-Depth Information
!
=
X
n i
X
r
r
c j ¼
c iaj
n i
i ¼
1
a ¼
1
i ¼
1
The PseudoF measure of quality of the classi
cation is then given by the ratio
between B/(r
1) and W/(n
r) for B denoting the variance of the conditional
expectation given the classi
cation, W the expectation of the conditional variance, r
the number of classes and n the number of alternatives classi
ed.
Thus,
PseudoF
¼
ð
B
=
ð
r
1
Þ
Þ=
ð
W
=
ð
n
r
Þ
Þ
for
X
n i X
j
r
2
B ¼
c ij c j
;
i ¼ 1
X
X
X
r
2
W
¼
c iaj c ij
;
i ¼
1
j
a
and
X
r
n
¼
n i :
i ¼ 1
Thus,
!
!
r
!
!
X
n i X
j
= X
X
X
a ð c iaj c ij Þ
Þ= X
r
r
r
2
2
PseudoF ¼
ð c ij c j Þ
=
ð
r 1
n i
:
i ¼
1
i ¼
1
j
i ¼
1
Given the decomposition of the variance,
!
!
!
X
X
X
i
X
X
= X
i
X
X
Þ= X
i
2
2
2
PseudoF ¼
ð c iaj c ij Þ
c iaj c ij
c iaj c ij
=
ð
r 1
n i r
j
j
a
j
a
i
This construction does not take into account the possibility of different scales of
measurement of the different criteria. An alternative measure for the case of mea-
sures of importance for the criteria being available would compute the ratios sep-
arately for each criterion and weigh these ratios with weights that take into account
such scales:
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