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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 />

Discussion<br />

Although Stoica <strong>and</strong> Nehorai do not make explicit the difference between the model parameters<br />

<strong>and</strong> their powered-up <strong>multi</strong>-<strong>step</strong> counterparts, they show the importance of the hypothesis of<br />

model misspecification as a justification for the use of DMS. Here, it is the same model which is<br />

used at all forecast horizons, but the <strong>estimation</strong> method matches the desired outcome. In their<br />

simulations, the authors find that an ARMA(2, 2) estimated by an AR(1) model can lead to more<br />

accurate forecasts when using DMS. Their conclusion relating to under-parameterization mirrors<br />

that of Bhansali (1999); it is surprising that the very specific form of DGP they use should not<br />

strike them: it exhibits a root close to unity. It is thus possible that non-stationarity may appear<br />

as a feature benefitting DMS.<br />

5 Efficiency in matching criteria for <strong>estimation</strong> <strong>and</strong> forecast<br />

evaluation.<br />

Analyzing the ARIMA time series reported in Madrikakis (1982), Weiss <strong>and</strong> Andersen (1984) compare<br />

the <strong>forecasting</strong> properties of various <strong>estimation</strong> methods when the forecast accuracy criterion<br />

varies. In particular, they compare the one-<strong>step</strong> <strong>and</strong> <strong>multi</strong>-<strong>step</strong> ahead forecasts. They find that<br />

when a one-<strong>step</strong> ahead forecast accuracy loss function is used, it is preferable to use one-<strong>step</strong><br />

ahead <strong>estimation</strong> (<strong>and</strong> then OLS, Least-Absolute Deviation seem similar for either MSFE or Mean<br />

Absolute Error (MAE) criteria). Similarly, when the forecast accuracy is measured by the absolute<br />

percentage trace of a matrix of the forecast errors at several horizons, the best amongst the four<br />

<strong>estimation</strong> methods which they use (the <strong>multi</strong>-<strong>step</strong> trace, one-<strong>step</strong> ahead OLS, one-<strong>step</strong> MAE <strong>and</strong><br />

one-<strong>step</strong> Mean Absolute Percentage Error) is the <strong>multi</strong>-<strong>step</strong> trace. They, thus, find some significant<br />

improvement from matching <strong>estimation</strong> <strong>and</strong> <strong>forecasting</strong> horizons.<br />

Weiss (1991) builds upon the earlier work on <strong>multi</strong>-<strong>step</strong> <strong>estimation</strong> for <strong>forecasting</strong> <strong>and</strong> derives<br />

conditions under which this technique is asymptotically ‘optimal’, in a sense that he defines. He<br />

builds on the work by Johnston, where, in model (6), he allows for more lags of the endogenous<br />

14

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