After stripping out systematic risk via the factor-residual decomposition, the accumulated idiosyncratic residual should be stationary and mean-reverting. But stationarity alone does not give a tradeable signal — the trading rules (entry level, sizing, expected time to convergence, stop-loss horizon) all require a parametric model of how fast the residual reverts and how wide its fluctuations are.
The Ornstein-Uhlenbeck (OU) process is the canonical mean-reverting diffusion: it is the continuous-time analogue of the discrete AR(1) model, with a well-defined equilibrium variance and a mean-reversion speed that can be estimated by OLS from the time series of accumulated residuals. Its parameters — the speed of reversion , the long-run mean , and the instantaneous volatility — connect directly to trading design: entry band width, expected half-life of a position, and stop-loss horizon.
Learning objectives. By the end of this note you should be able to:
- state the OU SDE and identify its three parameters (, , );
- solve the OU SDE and derive its equilibrium mean and variance;
- discretise the OU SDE to an AR(1) model and identify the AR(1) parameters with the OU parameters;
- estimate OU parameters by OLS from the accumulated residual series;
- compute the half-life and equilibrium standard deviation and use them to set band widths and stop-loss horizons.
In this lesson
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- The Ornstein-Uhlenbeck SDE
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- The solution and equilibrium distribution
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- AR(1) discretisation and OLS calibration
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- Half-life and trading horizon
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- Connection to band design
Before you start
- PCA Eigenportfolios as Statistical Risk Factors
- Stationarity, Non-Stationarity, and the Tradability of Spreads
The full lesson, with worked examples and exercise solutions, is for members.
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