Geoscience Reference
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ne the 2
n
coef
cients cor-
responding to the capacities of the 2
n
subsets of S. Modeling the capacity by means
of its Moebius transform may simplify this task.
For
To compute a capacity
µ
, the modeler needs to de
µ
a capacity on S, the Moebius transform of
µ
is the function
ʽ
: P(S)
R
→
de
ned by
X
ðÞ
A
B
j
j
2
S
v
ð
A
Þ
¼
1
l
ð
B
Þ; 8
A
2
B
A
The Moebius transform determines the capacity by:
X
l
ð
A
Þ
¼
m
ð
B
Þ:
B
A
The determination of the capacity may employ the Penrose-Banzhaf or Shapley
interaction indices (Grabisch and Roubens
1999
) for limited levels of iteration.
Given a capacity
µ
ↆ
on S, the Penrose-Banzhaf joint index for any subset A
Sis
given by (Penrose
1946
; Banzhaf
1965
)
2
#ð
S
n
A
Þ
X
K
S
n
A
X
Þ
#ð
A
L
Þ
l
ð
K
[
L
Þ;
Banzhaf A
ðÞ
¼
ð
1
L
A
for # the cardinality function, i.e., the function that associates to each set the number
of elements in it.
Analogously the Shapley joint index is de
ned by
X
X
ð
1
Þ
#A
n
L
ð
Þ
Sl
ð
A
Þ
¼
½
ð
#
ð
S
n
A
n
K
ÞÞ!ð
#
ð
K
ÞÞ!=ð
#
ð
S
n
A
Þþ
1
Þ!
l
ð
K
[
L
Þ
ð
K
S
n
A
Þ
L
A
For an isolated criterion i, Sµ({i})
µ
({i}) is called the Shapley value (Shapley
1953
).
The capacity
µ
is said to be k-additive, for a positive integer k, if its Moebius
transform
ʽ
satis
es (Grabisch
1997
):
2
S
; m
(1)
8
T
2
ðÞ
¼
T
0if
#
ðÞ
[
T
k
;
2
S
such that
(2)
9
B
2
#
ðÞ
¼
B
k and
m
ðÞ6
¼
B
0
:
By assuming 2-additivity, the complexity of the problem of determining the
capacity is reduced. The capacity can then be determined employing only the
coef
cients
µ
({i}) and
µ
({i, j}) for i and j
∈
S.
Necessary and suf
cient conditions for 2-additivity are:
(1)
P
i
; fg
S
Þ
P
i
2
S
l
fi;
l
fi;
i
;
j
gÞ ð
m
2
i
gÞ
¼
1
ð
normality
Þ;
(2)
l
fi;
ðÞ
i
0
; 8
i
2
S nonnegativity
ð
Þ
and
8
A
S with
# ðÞ
2
; 8
k
2
A
;
P
i
2
A
n fg
l
fi;
i
;
k
g
(3)
ð
ð
Þ
l
fi;
i
ðÞ
Þ # ðÞ
2
ð
Þ
l
fi;
k
ðÞ
ð
monotonicity
Þ:
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