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Two series that each have a unit root, I(1), are cointegrated if some linear combination of them, such as y_t − βx_t, is stationary, I(0). Cointegration means the series share a common stochastic trend and do not drift apart in the long run, so a regression of one on the other is meaningful rather than spurious. The Engle-Granger method estimates β by OLS and then tests the residuals for a unit root using special critical values. When series are cointegrated, an error correction model links short-run changes to the previous period's deviation from the long-run relationship.
Simulate two random walks that share a common trend and two that are independent, and plot each pair along with the residual from regressing one on the other. Students see the residual wander without bound in the spurious case and revert in the cointegrated case. Then estimate an error correction model on the cointegrated pair and interpret the adjustment coefficient as the fraction of last period's gap closed each period.
From your work on unit roots you know that regressing one I(1) series on another can produce a spurious regression: high R² and significant t-statistics even when the series are unrelated. The usual fix is to difference the data. But some pairs of trending series really are tied together. Consumption and income both grow, but consumption does not drift arbitrarily far from income. Short- and long-term interest rates move a lot, but the spread between them tends to return toward a typical level. Cointegration describes this case.
Two I(1) series x_t and y_t are cointegrated if there is a number β such that y_t − βx_t is stationary. Each series wanders, but they wander together, because they share a common stochastic trend. The combination y_t − βx_t measures the distance from long-run equilibrium, and that distance keeps returning toward its mean. Clive Granger introduced the idea, and his 1987 paper with Robert Engle set out how to represent, estimate, and test it. Granger's work on cointegration was cited when the two shared the 2003 Nobel Memorial Prize in Economic Sciences.
The Engle-Granger two-step method tests for it. First, regress y_t on x_t in levels by OLS and save the residuals. Second, run a Dickey-Fuller-type regression on those residuals. If you reject a unit root, the series are cointegrated. The critical values differ from the usual Dickey-Fuller table. Because OLS chose β to make the residuals as small as possible, they look more stationary than an arbitrary series would, so the test requires stronger evidence. With cointegration, the OLS estimate of β converges to the true value unusually fast, a property called superconsistency.
Once cointegration is established, the error correction model describes the short run:
Δy_t = α + γΔx_t + δ(y_{t−1} − βx_{t−1}) + u_t.
Every term in this equation is stationary, so the usual regression tools can be used for γ and δ. The coefficient γ captures the immediate response to a change in x. The coefficient δ, expected to be negative, governs adjustment: if y was above its long-run level last period, y tends to fall now. With δ = −0.25, about a quarter of any gap closes each period. Granger's representation theorem shows that cointegration and an error correction form go together.
For more than two series there can be several cointegrating relationships. Johansen's method tests for their number within a vector autoregression, producing a vector error correction model.
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