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228 J. M. Rodríguez-Poo et al.<br />

this event are observed. We gather these characteristics <strong>in</strong> a k-dimensional vector<br />

yi. Thus, the follow<strong>in</strong>g set <strong>of</strong> observations is available<br />

{(di,yi)}i=1,...,n.<br />

One possible way to obta<strong>in</strong> <strong>in</strong>formation about the whole process is to assume that<br />

the ith duration has a prespecified conditional parametric density di|Ii−1 ∼ p<br />

� di| ¯di−1, ¯yi−1; δ � , where ( ¯di−1, ¯yi−1) is the past <strong>in</strong>formation and δ is a set <strong>of</strong><br />

f<strong>in</strong>ite-dimensional parameters. Under these conditions it is possible to estimate<br />

the parameter vector δ through maximum likelihood techniques. But sometimes<br />

assumptions about the knowledge <strong>of</strong> the whole conditional density are too strong<br />

and the researcher prefers to make assumptions about some <strong>of</strong> its conditional<br />

moments. Let<br />

E[di| ¯di−1, ¯yi−1]=ψ(¯di−1, ¯yi−1; ϑ1) (1)<br />

be the expectation <strong>of</strong> the ith duration conditional on the past filtration. The ACD<br />

class <strong>of</strong> models consists <strong>of</strong> parameterizations <strong>of</strong> (1) and the assumption that<br />

di = ψ(¯di−1, ¯yi−1; ϑ1)εi,<br />

where εi is an i.i.d. random variable with density function p(εi; ξ)depend<strong>in</strong>g on a<br />

set <strong>of</strong> parameters ξ and mean equal to one. The vector ϑ1 conta<strong>in</strong>s the parameters<br />

that measure the dynamics <strong>of</strong> the scale and ξ conta<strong>in</strong>s the shape parameters. The<br />

conditional log-likelihood function can be written as<br />

Ln (d; ϑ1,ξ) =<br />

n�<br />

log p � di| ¯di−1, ¯yi−1; ϑ1,ξ � . (2)<br />

i=1<br />

If the conditional density is correctly specified and ϑ1 and ξ are f<strong>in</strong>ite-dimensional<br />

parameters, then, under some standard regularity conditions, the maximum likelihood<br />

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

normal (for conditions see Engle and Russell (1998)).<br />

The specification described above is sometimes too simple and/or rigid s<strong>in</strong>ce the<br />

expected duration can vary systematically over time and can be subject to many<br />

different time effects. One way to extend the above model is to decompose the<br />

conditional mean <strong>in</strong>to different effects. In standard time series literature a stochastic<br />

process can be decomposed <strong>in</strong>to a comb<strong>in</strong>ation <strong>of</strong> cycle and trend, seasonality and<br />

noise. This decomposition, with a long tradition <strong>in</strong> time series analysis, has already<br />

been used <strong>in</strong> volatility (see, among others, Andersen and Bollerslev (1998)) and<br />

duration analysis (e.g. Engle and Russell (1998)). Instead <strong>of</strong> (1), the follow<strong>in</strong>g<br />

nonl<strong>in</strong>ear decomposition is proposed:<br />

E[di| ¯di−1, ¯yi−1]=ϕ � ψ(¯di−1, ¯yi−1; ϑ1), φ( ¯di−1, ¯yi−1; ϑ2) � . (3)<br />

Durations are modeled as a possibly nonl<strong>in</strong>ear function <strong>of</strong> two components,<br />

ψ(·; ϑ1) and φ(·; ϑ2), that represent dynamic and seasonal behavior, respectively.<br />

The function ϕ(u, v) nests a great variety <strong>of</strong> models. ϕ(u, v) = (u × v) forms an

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