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30 Chapter 1 Introduction<br />

If the operator ∇ is applied to a linear trend function mt c0 +c1t, then we obtain the<br />

constant function ∇mt mt − mt−1 c0 + c1t − (c0 + c1(t − 1)) c1. In the same<br />

way any polynomial trend of degree k can be reduced to a constant by application of<br />

the operator ∇ k (Problem 1.10). For example, if Xt mt +Yt, where mt k<br />

j0<br />

and Yt is stationary with mean zero, application of ∇ k gives<br />

∇ k Xt k!ck +∇ k Yt,<br />

a stationary process with mean k!ck. These considerations suggest the possibility,<br />

given any sequence {xt} of data, of applying the operator ∇ repeatedly until we find<br />

a sequence ∇k <br />

xt that can plausibly be modeled as a realization of a stationary<br />

process. It is often found in practice that the order k of differencing required is quite<br />

small, frequently one or two. (This relies on the fact that many functions can be<br />

well approximated, on an interval of finite length, by a polynomial of reasonably low<br />

degree.)<br />

Example 1.5.3 Applying the operator ∇ to the population values {xt,t 1,...,20} of Figure 1.5, we<br />

find that two differencing operations are sufficient to produce a series with no apparent<br />

trend. (To carry out the differencing using ITSM, select Transform>Difference,<br />

enter the value 1 for the differencing lag, and click OK.) This replaces the original<br />

series {xt} by the once-differenced series {xt − xt−1}. Repetition of these steps gives<br />

the twice-differenced series ∇ 2 xt xt − 2xt−1 + xt−2, plotted in Figure 1.23. Notice<br />

that the magnitude of the fluctuations in ∇ 2 xt increases with the value of xt. This effect<br />

can be suppressed by first taking natural logarithms, yt ln xt, and then applying the<br />

operator ∇ 2 to the series {yt}. (See also Figures 1.1 and 1.17.)<br />

Figure 1-23<br />

The twice-differenced series<br />

derived from the population<br />

data of Figure 1.5.<br />

(millions)<br />

-80 -60 -40 -20 0 20 40 60 80 100<br />

1820 1840 1860 1880 1900 1920 1940 1960 1980<br />

cjt j

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