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186 Chapter 6 Nonstationary and Seasonal Time Series Models<br />

ACF<br />

-1.0 -0.5 0.0 0.5 1.0<br />

Figure 6-8<br />

The sample ACF of the<br />

data in Figure 6.7. Lag<br />

0 10 20 30 40<br />

The autocorrelation function of the model (6.1.6) can be derived by noting that<br />

1 − 2r −1 cos ω B + r −2 B 2 1 − r −1 e iω B 1 − r −1 e −iω B <br />

(6.1.7)<br />

and using (3.2.12). This gives<br />

where<br />

ρ(h) r<br />

−h sin(hω + ψ)<br />

, h ≥ 0, (6.1.8)<br />

sin ψ<br />

tan ψ r2 + 1<br />

r2 tan ω.<br />

− 1<br />

It is clear from these equations that<br />

(6.1.9)<br />

ρ(h) → cos(hω) as r ↓ 1. (6.1.10)<br />

With r 1.005 and ω π/3 as in the model generating Figure 6.7, the model<br />

ACF (6.1.8) is a damped sine wave with damping ratio 1/1.005 and period 6. These<br />

properties are reflected in the sample ACF shown in Figure 6.8. For values of r closer<br />

to 1, the damping will be even slower as the model ACF approaches its limiting form<br />

(6.1.10).<br />

If we were simply given the data shown in Figure 6.7, with no indication of<br />

the model from which it was generated, the slowly damped sinusoidal sample ACF<br />

with period 6 would suggest trying to make the sample ACF decay more rapidly<br />

by applying the operator (6.1.7) with r 1 and ω π/3, i.e., 1 − B + B 2 .Ifit<br />

happens, as in this case, that the period 2π/ω is close to some integer s (in this case<br />

6), then the operator 1 − B s can also be applied to produce a series with more rapidly

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