DISPERSION OF THE ERRORS IS NON-CONSTANT AND NOT RELATED TO THE MEAN
DISPERSION OF THE ERRORS IS NON-CONSTANT AND NOT RELATED TO THE MEAN (TIME SERIES DATA)
- Consider a regression : Y(t) = v0*X(t) + e(t)
where e has variance W(t)**2 * VAR and a mean of zero
and where W is a vector of weights t in length.
This is referred to in the statistical literature as weighted regression .
It is standard practice for the weights to be known before-hand
rather than boot-strapped from estimated errors (residuals).
The residuals from a model may not have constant variance and
consequently estimated parameters may be deficient. One form of
non-constant variance is treated by the Box-Cox or lambda
transformations. However the best set of weights may not be a function
of anything and just simply a vector of values.
There are cases in which the user
has an "a priori" knowledge of the weights.
For example consider, the
actuarial economist who has data where each reading
is based upon "n" samples. Thus a reading with a large
"n" is more credible than one with small "n".
A far more common occurrence is when there is no prior knowledge existing and an empirical
approach is required.
Consider
the case where an upward trending series has a residual variance of say
10 for the first half and a variance of the residuals of 20 for the
second half. It would be totally incorrect to either ignore the change
in variance or to use the power transform procedures of Box-Cox. The
suggested procedure is to simply identify a model and compute a vector
of residuals.
By breaking the residuals into consecutive but
non-overlapping sections one can perform the standard F test for
variance change. The time period with the greatest F value is then a
potential point of variance change. This is referred to as a
structural change in the variance .
The vector of weights would then be the inverse of the estimated
local variances.
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