Geoscience Reference
In-Depth Information
d !
In our proofs we use the concept of level sets. For a function f W
R
R
the
d W f.x/ g (the
level set for a value 2
R
is given by L .f;/ WD f x 2
R
d W f.x/< g ) and the level curve for a value
strict level set is L < .f;/ WDf x 2
R
d W f.x/ D g : For a function f i . / we use
2
R
is given by L D .f;/ WDf x 2
R
the notation
.f i / WD arg min
x2 R
f i .x/:
X
d
For two points x and y we denote the segment defined by x and y as xy .
In this chapter we focus on some fundamental results in the continuous,
network and discrete cases. We will describe in some detail a complete geometric
characterization for the planar 1-facility case, an optimal time algorithm for the
1-facility network problem as well as the computation of the entire set of Pareto-
optimal solutions of the discrete multicriteria p-median problem. Although we are
concentrating on the median case we will give some outlook to extensions.
9.2
1
-Facility Planar/Continuous Location Problems
In this section we study Problem ( 9.1 )wheref 1 . /;:::;f Q . / are convex, inf-
compact functions, defined in
2 , which represent different criteria or scenarios.
Recall that a real function f. / is said to be inf-compact if its lower level sets
f x 2
R
d W f.x/ g are compact for any 2
. The next result states a
useful characterization of the different solution sets defined in the previous section
using level sets and level curves which will be used later.
R
R
Theorem 9.1 The following characterizations hold :
Q
\
X wPar f 1 ;:::;f Q ,
L < .f q ;f q .x// D;
x 2
(9.2)
qD1
Q
Q
\
\
X Par f 1 ;:::;f Q ,
L .f q ;f q .x// D
L D .f q ;f q .x//
x 2
qD1
qD1
(9.3)
Q
\
X sPar f 1 ;:::;f Q ,
L .f q ;f q .x// Df x g :
x 2
(9.4)
qD1
Search WWH ::




Custom Search