Geoscience Reference
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!
=
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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