Meddahi (2002) ARMA Representation of Two-Factor Models

garchstochastic-volatilitydiffusion-processtemporal-aggregation

Summary

Derives closed-form expressions for the moving-average roots of a two-factor ARMA model — the analytically hard part of characterising the ARMA(p,p) structure of a variable defined as the sum of p AR(1) processes. Applies the result to characterise the weak GARCH(2,2) representation (Drost-Nijman 1993) of squared returns for two-factor continuous-time stochastic volatility models (affine, GARCH diffusion, constant-elasticity-of-variance (CEV), Ornstein-Uhlenbeck, eigenfunction, square-root stochastic autoregressive volatility (SR-SARV)) at any observation frequency hh, linking continuous-time parameters directly to discrete-time GARCH coefficients.

Key Claims

Concepts Introduced or Extended

Entities Mentioned

Quotes

"Many financial time series models are specified through a structural representation. Nonetheless, knowing their reduced ARMA form may be useful for impulse response analysis, filtering, forecasting, and for purposes of statistical inference."

"While the model is a (weak) GARCH(2,2) for all frequencies, it appears as a (weak) GARCH(1,1) for the weekly frequency and lower ones. The main reason is that the very volatile but non persistent factor has no impact on volatility clustering. This explains the empirical relevance of the GARCH(1,1) with respect to other ARCH-type models."

My Take

The paper fills a clean gap: Granger-Morris (1976) told us the ARMA order of a sum of AR(1) processes but could not analytically characterise the MA roots for orders > 1. The closed-form in Proposition 2.1 is the main new result, and the SV application in Section 3 is its payoff. The temporal-aggregation result (GARCH(2,2) \to GARCH(1,1) at lower frequencies) provides a satisfying theoretical explanation for a long-standing empirical regularity. The identification difficulty at high frequencies (AR \approx MA roots) is an important caveat for microstructure-heavy intra-daily estimation.