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direct multi-step estimation and forecasting - OFCE - Sciences Po

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Direct <strong>multi</strong>-<strong>step</strong> <strong>estimation</strong> <strong>and</strong> <strong>forecasting</strong><br />

9.2 A general forecast-error taxonomy<br />

We now borrow from Clements <strong>and</strong> Hendry who suggest in Clements <strong>and</strong> Hendry (1998b) <strong>and</strong><br />

Hendry (2000) a general forecast error taxonomy which helps us in assessing the advantages of<br />

<strong>multi</strong>-<strong>step</strong> <strong>estimation</strong>. We use the framework presented above but for ease of exposition modify it<br />

slightly. Notice that in (20), f x (·), if it represents the true DGP, provides the—potentially time<br />

dependent—joint density of x t at time t, conditional on X t−p<br />

t−1 = (x t−1, ..., x t−p ), <strong>and</strong> z t . Assume,<br />

without loss of generality, that {z t } contains only deterministic factors—such as intercepts, trends<br />

<strong>and</strong> indicators—<strong>and</strong> that all stochastic variables are included in {x t }. As previously, it is desired to<br />

forecast x T +h , or perhaps of function thereof (e.g. if z t originally contained stochastic variables),<br />

over horizons h = 1, ..., H, from a forecast origin at T . Now, the dynamic model does not coincide<br />

with the data generating process <strong>and</strong> it specifies the distribution of x t conditional on X t−r<br />

t−1 , with lag<br />

length r, deterministic components d t <strong>and</strong> implicit stochastic specification defined by its parameters<br />

ψ t . This model is fitted over the sample t = 0, ..., T, so that parameter estimates are a function of<br />

the observations, represented by:<br />

̂ψ T = Ψ T<br />

(<br />

˜X0 T , D 0 T<br />

)<br />

, (23)<br />

where ˜X denotes the measured data <strong>and</strong>, as before D 0 t = (d t , ..., d 0 ). A sequence of forecasts<br />

{̂x T +h|T } is produced as a result. The subscript on ̂ψ in (23) denotes the influence of the sample<br />

size. Let ψ e T = E T<br />

[̂ψT<br />

], where it exists. Because the underlying densities may be changing over<br />

time, all expectation operators must be time dated. Future values of the stochastic variables are<br />

unknown, but those of deterministic variables are known; there, therefore, exists a function g h (·)<br />

such that<br />

̂x T +h|T = g h<br />

(<br />

˜XT<br />

−r+1<br />

T<br />

, D T +1<br />

T +h , ̂ψ T<br />

)<br />

. (24)<br />

The corresponding h–<strong>step</strong> ahead expected forecast error is, thus, the expected value of e T +h|T =<br />

x T +h − ̂x T +h|T , <strong>and</strong> is given by<br />

]<br />

E T +h<br />

[x T +h − ̂x T +h|T | X 0 T , {Z ∗ } 0 T +h<br />

,<br />

where the actual values of the deterministic factors over the forecast period (including any deterministic<br />

shifts) are denoted by {Z ∗ } T +1<br />

T +h <strong>and</strong> {Z∗ } 0 T +h = {Z ∗ } T +1<br />

T +h , Z0 T ; <strong>and</strong> the<br />

[<br />

]<br />

expectation<br />

36

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