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226 J. M. Rodríguez-Poo et al.<br />

version <strong>of</strong> the ACD. Grammig and Mauer (2000) use a Burr distribution <strong>in</strong> the<br />

ACD model. Zhang et al. (2001) <strong>in</strong>troduce a threshold ACD (TACD). Fernandes<br />

and Grammig (2001) <strong>in</strong>troduce the augmented ACD model, a very general model<br />

that covers almost all the exist<strong>in</strong>g ones. Drost and Werker (2004) provide a method<br />

for obta<strong>in</strong><strong>in</strong>g efficient estimators <strong>of</strong> the ACD model with no need to specify the<br />

distribution. Meitz and Terasvirta (2005) <strong>in</strong>troduce smooth transition ACD models<br />

and test<strong>in</strong>g evaluation procedures.Alternative models are the stochastic conditional<br />

duration (SCD) model <strong>of</strong> Bauwens and Veredas (2004) and the stochastic volatility<br />

duration (SVD) model <strong>of</strong> Ghysels et al. (2004), both based on latent variables.<br />

In the application <strong>of</strong> most <strong>of</strong> the above studies, durations show a strong<br />

<strong>in</strong>tradaily seasonality, i.e., an <strong>in</strong>verted U shape pattern along the day, as it is shown<br />

<strong>in</strong> Figs. 2 and 3 for price and volume durations <strong>of</strong> two stocks traded at the NYSE.<br />

The study <strong>of</strong> seasonality for regularly spaced variables, i.e., observed at equidistant<br />

periods <strong>of</strong> time, is well known. It has focused ma<strong>in</strong>ly on the <strong>in</strong>tradaily behavior<br />

<strong>of</strong> volatility either on stock markets or on foreign exchange markets—see, among<br />

others, Baillie and Bollerslev (1990), Bollerslev and Domowitz (1993), Andersen<br />

and Bollerslev (1997 and 1998) and Beltratti and Morana (1999). All these articles<br />

used data sampled at different frequencies: hourly, half-hourly, every 15 m<strong>in</strong> or<br />

every 5 m<strong>in</strong>.<br />

Durations do not fit <strong>in</strong>to this category as they are themselves the ma<strong>in</strong> characteristic<br />

<strong>of</strong> irregularly spaced data. For tick-by-tick data, Engle and Russell<br />

(1998) <strong>in</strong>troduce a method for deal<strong>in</strong>g with <strong>in</strong>tradaily seasonality. It consists <strong>of</strong><br />

decompos<strong>in</strong>g the expected duration <strong>in</strong>to a determ<strong>in</strong>istic part, that depends on the<br />

time-<strong>of</strong>-the-day at which the duration starts, and a stochastic part. The determ<strong>in</strong>istic<br />

component accounts for the seasonal effect whereas the stochastic component<br />

models the dynamics. If both components are assumed to belong to a parametric<br />

family <strong>of</strong> functions, the two sets <strong>of</strong> parameters can be jo<strong>in</strong>tly estimated by maximum<br />

likelihood (ML) techniques. And, under standard regularity conditions, ML<br />

estimators <strong>of</strong> the parameters <strong>of</strong> <strong>in</strong>terest are consistent and asymptotically normal<br />

(see Engle and Russell, 1998; corollary, p. 1135).<br />

In many situations the researcher does not have enough <strong>in</strong>formation to fully<br />

specify the seasonality functions or seasonality itself is not the ma<strong>in</strong> subject<br />

<strong>of</strong> analysis but it has to be taken <strong>in</strong>to account. In these cases, the choice <strong>of</strong> a<br />

particular parametric function can be delicate. An alternative is to approximate<br />

the seasonal component through nonparametric functions (ma<strong>in</strong>ly Fourier series,<br />

spl<strong>in</strong>e functions, or other types <strong>of</strong> smoothers) and then estimate the parameters<br />

<strong>of</strong> the dynamic component us<strong>in</strong>g maximum likelihood techniques. Unfortunately,<br />

standard maximum likelihood for f<strong>in</strong>ite dimensional parameters, <strong>in</strong> the presence <strong>of</strong><br />

<strong>in</strong>f<strong>in</strong>ite “<strong>in</strong>cidental” parameters, may yield <strong>in</strong>consistency and slow rates <strong>of</strong> convergence<br />

(see, for examples <strong>of</strong> <strong>in</strong>consistency: Kiefer and Wolfowitz (1956); Grenander<br />

(1981); and Shen and Wong (1994) and for examples <strong>of</strong> slow rates <strong>of</strong> convergence<br />

Birgé and Massart (1994)). In order to solve this problem many alternative solutions<br />

have been proposed. If the seasonal component is estimated through spl<strong>in</strong>es,<br />

Fourier series, neural networks, or wavelets, then the method <strong>of</strong> sieve extremum<br />

estimation can be used to make <strong>in</strong>ference on the seasonal term. Chen and Shen<br />

(1998) give sufficient conditions for spl<strong>in</strong>es and Fourier series under regularly<br />

spaced dependent data. If, <strong>in</strong>stead, other methods such as kernels or local polynomials<br />

are used, then the sieve method is no longer valid and other nonsieve ML<br />

estimation methods are needed. Among others, the so-called generalized pr<strong>of</strong>ile

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