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Semiparametric estimation for f<strong>in</strong>ancial durations 243<br />

knots are chosen ad hoc). For UniNW and UniSp we show the seasonal curve ˆφϑ1,ξ(t ′ 0 )<br />

at a different scale than the other seasonal estimators. It is not possible to present them<br />

at the same scale s<strong>in</strong>ce it is a logarithmic function, see Eq. (13), and the argument <strong>of</strong> the<br />

function is not the observed duration but the duration adjusted by the dynamics.<br />

3.4 Predictibility<br />

So far estimation results dovetail with the theory. We now check how well they predict the<br />

probability distribution. S<strong>in</strong>ce density forecast is strongly dependent on the distributional<br />

assumption, we only show results for ML (the exponential density does it worse than<br />

the generalized gamma). Another reason for stick<strong>in</strong>g to ML is because we want to study<br />

the predictive capabilities <strong>of</strong> the model for different estimators <strong>of</strong> seasonality. S<strong>in</strong>ce the<br />

density and the parametric component are the same, differences <strong>in</strong> density forecast may<br />

exclusively come from the different specification <strong>of</strong> the seasonal component.<br />

If εj ∼ GG � �<br />

1, ˆγn, ˆνn then<br />

� � � � �<br />

dj ∼ GG ϕ ψ ¯dj−1, ¯yj−1; ˆϑ1n , ˆφ ˆϑ1n,ˆξn<br />

t ′ �� �<br />

−1<br />

j−1 , ˆγn, ˆνn ,<br />

for UniNW and UniSp. For the two-step methods, s<strong>in</strong>ce ˜dj = dj ˆφ<br />

�<br />

t ′ �−1 j−1 , the seasonal<br />

curve is outside the function ϕ(·), that is<br />

or<br />

˜dj =<br />

ˆφ<br />

dj<br />

�<br />

t ′ j−1<br />

� � � �� �<br />

−1<br />

� ∼ GG ϕ ψ ¯dj−1, ¯yj−1; ˆϑ1n , ˆγn, ˆνn<br />

� � � ��−1 �<br />

dj ∼ GG ϕ ψ ¯dj−1, ¯yj−1; ˆϑ1n ˆφ t ′ � �<br />

−1<br />

j−1 , ˆγn, ˆνn .<br />

Figures 7 and 8 show the density forecast results. The histograms for UniNW are<br />

significantly better than for any other estimator. Although formal tests can be performed<br />

to assess the accuracy <strong>of</strong> this statement, visual <strong>in</strong>spection <strong>of</strong> the figures reveals that<br />

estimation <strong>in</strong> two steps (BiSp and BiNW) results <strong>in</strong> misspecification <strong>in</strong> the conditional<br />

distribution <strong>of</strong> the durations—<strong>in</strong> l<strong>in</strong>e with Bauwens et al. (2004). Moreover, estimation <strong>in</strong><br />

one step with spl<strong>in</strong>es, UniSp, leads to similar results as the two step estimators. This fits<br />

with the conclusions on estimation results that found similar estimates under BiSp and<br />

UniSp. Second, for volume durations none <strong>of</strong> the specifications correctly captures the<br />

dynamic component. This is expected as the dynamics are modeled <strong>in</strong> the same way for<br />

all specifications and Bauwens et al. (2004) already show that a simple Log-ACD(1,1)<br />

is unable to fit the dynamics.<br />

The better performance <strong>of</strong> UniNW is a result <strong>of</strong> its flexibility, as already mentioned.<br />

UniNW adapts to changes <strong>in</strong> the seasonal pattern. We can <strong>in</strong>terpret the seasonal estimator<br />

UniNW as a time-vary<strong>in</strong>g <strong>in</strong>tercept that adapts the conditional expectation <strong>of</strong> the durations<br />

to changes <strong>in</strong> seasonality. This is because UniNW is a pure nonparametric estimator<br />

and follows the pr<strong>in</strong>ciple <strong>of</strong> let the data speak. This is not the case <strong>of</strong> the polynomial<br />

spl<strong>in</strong>e (22). In fact, Eq. (22) not only depends implicitly on ˆϑ1n and ˆξn but also depends<br />

on ˆθn and ˆδn. And these parameters are estimated us<strong>in</strong>g the <strong>in</strong>-sample to fit the <strong>in</strong>-sample

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