Pj. Brockwell et O. Stramer, ON THE APPROXIMATION OF CONTINUOUS-TIME THRESHOLD ARMA PROCESSES, Annals of the Institute of Statistical Mathematics, 47(1), 1995, pp. 1-20
Citations number
21
Categorie Soggetti
Statistic & Probability",Mathematics,"Statistic & Probability
Threshold autoregressive (AR) and autoregressive moving average (ARMA)
processes with continuous time parameter have been discussed in sever
al recent papers by Brockwell ef al. (1991, Statist. Sinica, 1, 401-41
0), Tong and Yeung (1991, Statist. Sinica, 1, 411-430), Brockwell and
Hyndman (1992, International Journal Forecasting, 8, 157-173) and Broc
kwell (1994, J. Statist. Plann. Inference, 39, 291-304). A threshold A
RMA process with boundary width. 2 delta > 0 is easy to define in term
s of the unique strong solution of a stochastic differential equation
whose coefficients are piecewise linear and Lipsckitz. The positive bo
undary-width is a convenient mathematical device to smooth out the coe
fficient changes at the boundary and hence to ensure the existence and
uniqueness of the strong solution of the stochastic differential equa
tion from which the process is derived. In this paper we give a direct
definition of a threshold ARMA processes with delta = 0 in the import
ant case when only the autoregressive coefficients change with the lev
el pf the process. (This of course includes all threshold AR processes
with constant scale parameter.) The idea is to express the distributi
ons of the process in terms of the weak solution of a certain stochast
ic differential equation. It is shown that the joint distributions of
this solution with delta = 0 are the weak limits as 6 1 0 of the distr
ibutions of the solution with delta > 0. The sense in which the approx
imating sequence of processes used by Brockwell and Hyndman (1992, Int
ernational Journal Forecasting, 8, 157-173) converges to this weak sol
ution is also investigated. Some numerical examples illustrate the val
ue of the latter approximation in comparison with the more direct repr
esentation of the process obtained from the Cameron-Martin-Girsanov fo
rmula. It is used in particular to fit continuous-time threshold model
s to the sunspot and Canadian lynx series.