DECOMPOSITION INCLUDING AN AR COMPONENT 179
12.3 Decomposition Including a Stationary AR Component
In this section, we consider an extension of the standard seasonal adjust-
ment method (Kitagawa and Gersch (1984)). In the standard seasonal
adjustment method, the time series is decomposed into three compo-
nents, i.e., the trend component, the seasonal component and the ob-
servation no ise. These components are assumed to follow the models
given in (12.15) and (12.16), and the observation noise is assumed to
be a white noise. Therefore, if a significant deviation from that assump-
tion is present, th e n the decomposition obtained by the standard seasonal
adjustment method might become inappropriate. Figure 12.3 shows the
decomp osition of the BLSALLFOOD data of Figure 1.1(d) that was ob-
tained by the seasonal adjustment method for the model with k = 2, ℓ = 1
and p = 12. In this case, different f rom th e case shown in the previous
section, the estimated trend shows a wiggle, par ticularly in the latter par t
of the data.
Let us consider the problems when the above-men tioned wiggly
trend is obtaine d. Similarly to the Figure 12.2, Figure 12.4 shows the
increasing hor iz on prediction for the latter two years (24 observations)
of the BLSALLFOOD data based on the fo rmer 132 observations. In
this case, apparently the predicted mean y
132+ j|132
provides a reason able
prediction of the actual time series y
132+ j
. However, it is evident that
prediction by this model is not reliable , because an explosive increase in
the size of the confidence interval is observed.
Figure 12.5 shows the overlay o f 13 increa sin g h orizon predictions
that are obtaine d by assuming the starting point to be n = 126,...,138,
respectively. The increasing hor iz on predictions starting at and before
n = 130 have significan t downward bias. On the other hand, the increas-
ing horizon predictions starting at and after n = 135 have significant up-
ward bias. This is the reason that the explosive increase in the width of
the confide nce interval of the increasing horizon p redictions has occurred
as the lead time has increased. The stochastic trend component model
in the seasonal adjustment model can flexibly express a complex trend
component. But in the incre asing horizon prediction with this model, th e
predicted mean t
n+ j|n
can simply be obtained b y using the difference
equation
∆
k
t
n+ j|n
= 0. (12.21)
Therefore, whether the predicted values may go up or down is de-
cided by the starting point o f the trend. From these results, we see that
if the estimated trend is wiggly, it is not appropriate to use the standard