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Applications of state space models in finance

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5.1 Autoregressive conditional heteroskedasticity 61<br />

(1986) refer to the class <strong>of</strong> <strong>models</strong> with γ1+δ1 = 1 as <strong>in</strong>tegrated GARCH (IGARCH). For<br />

IGARCH <strong>models</strong> the f<strong>in</strong>ite unconditional variance is not def<strong>in</strong>ed. Although the IGARCH<br />

model is not covariance-stationary, it can be shown that it is strictly stationary. Standard<br />

<strong>in</strong>ference procedures rema<strong>in</strong> asymptotically valid given that the sample size is large; cf.<br />

Bollerslev et al. (1992) where further references can be found.<br />

To understand why the GARCH(1,1) process is qualified to model the stylized facts<br />

<strong>of</strong> a small first-order autocorrelation and a slow decay simultaneously, we have a look<br />

at the autocorrelations <strong>of</strong> ɛ 2 t :<br />

γ<br />

ρ1 = γ1 +<br />

2 1δ1<br />

1 − 2γ1δ1 − δ2 1<br />

, (5.9)<br />

ρτ = (γ1 + δ1) τ−1 ρ1, for τ = 2, 3, . . . . (5.10)<br />

With the decay factor <strong>of</strong> the exponentially decl<strong>in</strong><strong>in</strong>g autocorrelations be<strong>in</strong>g equal to<br />

γ1 + δ1, the autocorrelations will decrease the more gradually the closer this sum is to<br />

unity (cf. Franses and van Dijk 2000, ¢ 4.1.1).<br />

5.1.1.2 Forecast<strong>in</strong>g<br />

With respect to forecasts <strong>of</strong> the conditional variance, it follows from (5.5) that the<br />

optimal l-step ahead forecast can be calculated directly from ht+1, which is part <strong>of</strong> the<br />

<strong>in</strong>formation set Ωt:<br />

ˆh t+l|t = ω + γ1ˆɛ 2 t+l−1|t + δ1 ˆ h 2 t+l−1|t . (5.11)<br />

For a covariance-stationary GARCH(1,1) process, it can be shown that this is equivalent<br />

to<br />

ˆh t+l|t = σ 2 + (γ1 + δ1) l−1 � ht+1 − σ 2� , (5.12)<br />

where the forecast reverts to σ 2 at an exponential rate (cf. Andersen et al. 2005).<br />

5.1.2 Nonl<strong>in</strong>ear extensions<br />

The basic GARCH model is based on the assumption that positive and negative past<br />

shocks have the same effect on the conditional variance. However, many f<strong>in</strong>ancial time<br />

series are asymmetric: negative shocks tend to have a bigger <strong>in</strong>fluence on future volatility<br />

than equally sized positive shocks. Asymmetric effects are <strong>of</strong>ten observed for aggregate<br />

equity <strong>in</strong>dices (cf. Andersen et al. 2005), which will be <strong>in</strong> the focus <strong>of</strong> this thesis. This<br />

asymmetry, first observed by Black (1976), is commonly referred to as leverage effect.<br />

Accord<strong>in</strong>g to its def<strong>in</strong>ition, the fall <strong>of</strong> the value <strong>of</strong> equity amounts <strong>in</strong> an <strong>in</strong>creased debtto-equity<br />

ratio, the leverage. This implies an <strong>in</strong>creased level <strong>of</strong> risk<strong>in</strong>ess, which results <strong>in</strong><br />

<strong>in</strong>creased future volatility. 12 In the standard GARCH model, the conditional variance<br />

does not depend on the sign <strong>of</strong> the shocks such that asymmetries cannot be accommodated.<br />

Over the last fifteen years various nonl<strong>in</strong>ear extensions <strong>of</strong> the GARCH model<br />

12 The volatility-feedback hypothesis by Campbell and Hentschel (1992) represents an alternative<br />

but less regarded explanation for volatility asymmetries, accord<strong>in</strong>g to which positive<br />

volatility shocks lead to lower future returns.

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