An optimisation algorithm applied to the one-dimensional stratification problem
Section 3. The one-dimensional stratification problem
Consider the
population vector
corresponding to the stratification variable
Without
loss of generality, we assume that the population elements in
are
ordered by the stratification variable such that
The
stratum boundaries are used to define the
strata
according to the rule:
1)
2)
for
3)
The stratification
problem corresponds to determining the cut-off points, i.e., the stratum
boundaries
such
that the variance (or equivalently the CV) of the estimator of total
is
minimised. In this section, we consider that the total number of strata
is
defined before applying the optimal stratification methods considered.
In practice, the
values of the survey variable
are not
available and hence the variance in expression (2.3) is not computable. A
common approach is to minimise instead the variance (or CV) of the estimator
for the total of the stratification variable
Several
authors have developed methods that focus on this optimization problem, which
from now on we call the one-dimensional “stratification problem”. We adopted
the same approach here.
Finding the
boundary points that minimize the variance (2.6) or the CV (2.7) corresponds to
a hard problem both from analytic and computational points of view. This is so
because the integer population and sample sizes
and
respectively) depend in a
nonlinear way on the stratum boundaries. According to de Moura Brito, Ochi, Montenegro and Maculan (2010a), depending
on
and the
number of distinct population
values,
the number of possible choices for the boundary points can be very large.
In view of this
difficulty, over the past decades, various methods were developed to search for
the optimum stratum boundaries, aiming to provide at least solutions which
correspond to local minima of good quality.
Dalenius (1951)
tackled the problem for the case
by
approximating the variance in (2.6) by ignoring the finite population
correction, which is equivalent to assuming that the sampling within strata
would have been simple random sampling with replacement. The approximate
variance to be minimised is then given by:
Under the Neyman
allocation (Cochran, 1977) using the
variable, and replacing the sample sizes
in (3.1)
by their theoretical values
leads to the expression used by
Dalenius (1951):
Dalenius and
Hodges (1959) considered the case when
and
offered an analytic solution which relied on approximating the distribution of
the
variable
by its histogram with a moderate number of classes. Still considering the
approximate variance and assuming Neyman’s allocation, Ekman (1959) provided a
solution using a geometric approach to find the stratum boundaries. Hedlin
(2000) further extended Ekman’s solution while retaining the original variance
(2.6) as the function to be minimised, which he labelled the extended Ekman
rule.
Hidiroglou (1986) proposed an approach which
pre-specifies the required precision (CV) for the estimator of total, and which
divides the population into two strata
such
that the total sample size
is
minimised. In this paper, the second stratum corresponds to a “take-all” or “certainty”
stratum, where all elements are included in the sample with probability one
Lavallée
and Hidiroglou (1988) generalized the approach to
strata,
while retaining the idea that the stratum containing the largest population
units is to be sampled completely. Their approach relied on adopting a special
type of allocation called Power Allocation (Bankier, 1988). More recently, Rivest (2002) further generalised the
approach of Lavallée and Hidiroglou (1988) while considering that the
target is minimising the variance for the estimator of a total of a model-based
prediction of the survey variable
instead
of the stratification variable
Gunning and Horgan (2004) proposed the
so-called Geometric method for defining the stratum boundaries. This method
assumes that the CVs of the stratification variable
are
approximately constant, and that the distribution of the stratification
variable is approximately uniform within each stratum. Under these assumptions,
the optimum stratum boundaries would form a Geometric progression, thus leading
to a very simple analytic solution.
Keskintürk and Er (2007) proposed an approach
based on a global optimisation technique called Genetic Algorithms. Following a
similar idea, de Moura Brito et al. (2017b) applied another global optimisation technique called
GRASP to the stratification problem. Here we followed a route like Keskintürk and
Er (2007), but have adopted an efficient choice of Genetic Algorithm, namely
the Biased Random Key Genetic Algorithm (BRKGA), described in Section 4.
Kozak (2004) proposed a method called random
search, followed later by Kozak and Verma (2006), where this approach was
compared to the Geometric method of Gunning and Horgan (2004). Khan, Nand and Ahmad (2008) used ideas of dynamic programming to develop an
algorithm that determines the stratum boundaries considering that the
stratification variable has either a Triangular or Normal distribution, and
that sampling within strata is with replacement. De Moura Brito,
Maculan, Lila and Montenegro (2010b) proposed an
exact algorithm based on graph theory, where proportional allocation to the
strata is assumed.
Er (2011) compared the efficiency of several
methods available in the literature, taking the Geometric approach of Gunning and
Horgan (2004) as the initial solution. Kozak (2014) compared his random search
with the Genetic Algorithm proposed by Keskintürk and Er (2007). Rao, Khan and Reddy
(2014) developed a method that tackles the stratum boundary determination and
stratum allocation problems simultaneously. Their algorithm relies on the
assumption that the stratification variable follows a Pareto distribution. Our
approach is more general and does not assume that the size variable follows a
particular distribution.
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