Tutorials › Econometrics (Graduate) › Superconsistency Of Cointegrating Regression

Unit Roots and Cointegration · Tutorial 401 of 952

Superconsistency Of Cointegrating Regression

Learn why a persistent integrated regressor makes the OLS cointegrating slope superconsistent, even when its innovations are correlated with the stationary regression error.

Advanced 11 min read

What You'll Learn

  • State the cointegrating regression assumptions that yield superconsistency.
  • Compare the orders of the OLS numerator and denominator.
  • Derive the rate-\(n\) convergence of the slope estimate.
  • Explain why correlated regressor innovations and regression errors need not cause inconsistency.
  • Distinguish superconsistency from ordinary square-root-rate estimation and from valid inference.

Why Cointegrating Regressions Behave Differently

In a regression with stationary variables, estimation typically learns about a slope by accumulating information at the square-root-of-sample-size rate. A cointegrating regression has a different structure: its regressor is integrated, so its level wanders over a range that grows with the sample. The resulting variation in the regressor can dominate a stationary regression error and make the slope estimate converge faster.

This result is called superconsistency. It is a statement about the rate at which the estimated long-run coefficient approaches its population value, not a claim that every finite-sample estimate is accurate. It also does not require the regressor and regression error to be independent. Endogeneity can affect the limiting distribution and finite-sample behavior, even though the coefficient remains consistent under the conditions below.

Model and Assumptions

Consider the cointegrating regression

$$ y_t=\alpha+\beta x_t+u_t,\qquad t=1,\ldots,n. $$

Here \(y_t\) and \(x_t\) are integrated of order one, while \(u_t\) is stationary. Thus, the linear combination \(y_t-\alpha-\beta x_t=u_t\) is stationary even though the two series being related are not. This is the defining feature of a cointegrating relation. For the rate derivation, use the following regularity conditions:

  • \(x_t\) has no deterministic drift and can be written as \(x_t=x_{t-1}+v_t\), where \(v_t\) is a stationary, short-memory process with positive long-run variance.
  • \(u_t\) is stationary, has finite moments, and is sufficiently weakly dependent for its partial sums to grow at order \(\sqrt n\).
  • The joint partial sums of \(v_t\) and \(u_t\) obey a functional central limit theorem. They may be correlated, including contemporaneously.
  • The regression includes an intercept, and the integrated component of \(x_t\) is nondegenerate.

“Short-memory” here rules out additional unit-root behavior and ensures that partial sums have the usual square-root scale. The joint limit condition allows dependence between \(v_t\) and \(u_t\); independence is not required. The OLS slope with an intercept is

$$ \hat{\beta} = \frac{\sum_{t=1}^n (x_t-\bar{x})(y_t-\bar{y})} {\sum_{t=1}^n (x_t-\bar{x})^2}. $$
Definition: The OLS slope is superconsistent at rate \(n\) if \(n(\hat{\beta}-\beta)=O_p(1)\). Equivalently, its estimation error is \(O_p(1/n)\), which is faster than the usual \(O_p(1/\sqrt n)\) rate. Under regularity conditions, \(n(\hat{\beta}-\beta)\) often has a nondegenerate, generally nonstandard limiting distribution; the rate statement alone does not specify that distribution.

Why the Denominator Grows Like \(n^2\)

The increments of an integrated regressor have stationary-scale variation, but its levels accumulate those increments. For a zero-drift random walk, a typical \(x_t\) is of order \(\sqrt n\) when \(t\) is near \(n\). Consequently, the squared deviations in the OLS denominator are typically of order \(n\) each, and summing \(n\) such terms gives order \(n^2\).

The functional central limit theorem makes that argument precise. Let \(W(r)\) denote the Brownian-motion limit of the scaled partial sums of \(v_t\), and let \(\sigma_v^2>0\) be the long-run variance of \(v_t\). With an intercept, centering the regressor corresponds in the limit to centering the Brownian path by its average. Under the stated conditions,

$$ \frac{1}{n^2}\sum_{t=1}^n (x_t-\bar{x})^2 \ \Rightarrow\ \sigma_v^2\int_0^1 \left(W(r)-\int_0^1 W(s)\,ds\right)^2\,dr. $$

The random integral is positive with probability one: a Brownian path is not constant over the interval. Thus the denominator, divided by \(n^2\), converges to a finite positive random quantity. In particular, the denominator is of order \(n^2\), not \(n\).

Why the Numerator Grows Like \(n\)

Substitute the regression model into the OLS formula. Since \(y_t-\bar{y}=\beta(x_t-\bar{x})+(u_t-\bar{u})\), the intercept disappears after centering, leaving the exact decomposition

$$ \hat{\beta}-\beta = \frac{\sum_{t=1}^n (x_t-\bar{x})(u_t-\bar{u})} {\sum_{t=1}^n (x_t-\bar{x})^2}. $$

The numerator is of order \(n\) under the joint weak-dependence conditions. One way to see the scale is to write \(U_t=\sum_{j=1}^t(u_j-E[u_j])\). Stationarity and the partial-sum limit imply that \(U_t\) is typically of order \(\sqrt n\) when \(t\) is of order \(n\); the integrated regressor is also of order \(\sqrt n\). Summing their increments against the regressor therefore produces terms on the \(n\) scale. A joint functional limit justifies this order even when increments and errors are correlated. Centering by sample means does not increase the order.

This argument is an order argument, not a claim that the numerator has a particular expectation or equals a fixed constant times \(n\). Its scaled limit can depend on the joint dependence between \(v_t\) and \(u_t\). Combining an \(O_p(n)\) numerator with an \(O_p(n^2)\) denominator yields the result.

Theorem: Under the stated cointegrating-regression conditions, the OLS slope satisfies \(\hat{\beta}-\beta=O_p(1/n)\), or equivalently \(n(\hat{\beta}-\beta)=O_p(1)\). Hence \(\hat{\beta}\) converges in probability to \(\beta\) at a faster rate than a usual square-root-rate estimator.

Worked Examples

Worked Example: Computing a Cointegrating OLS Slope

Suppose a hypothetical four-period data set follows \(y_t=2+2x_t+u_t\), with \(x_t=(0,1,2,3)\) and \(u_t=(0,0.2,-0.2,0.1)\). These values illustrate the OLS calculation; four observations cannot establish an asymptotic rate.

The corresponding \(y_t\) values are \(2,4.2,5.8,8.1\). The sample means are \(\bar{x}=1.5\) and \(\bar{y}=5.025\). The centered regressor values are \((-1.5,-0.5,0.5,1.5)\), and the centered outcome values are \((-3.025,-0.825,0.775,3.075)\). Therefore,

$$ \hat{\beta} = \frac{(-1.5)(-3.025)+(-0.5)(-0.825)+(0.5)(0.775)+(1.5)(3.075)} {(-1.5)^2+(-0.5)^2+(0.5)^2+(1.5)^2} = \frac{9.95}{5} = 1.990. $$

The fitted intercept is \(\hat{\alpha}=\bar{y}-\hat{\beta}\bar{x}=5.025-(1.990)(1.5)=2.040\). The estimated slope is \(0.010\) below the data-generating slope of \(2\). That finite-sample discrepancy is not evidence for or against superconsistency: the rate describes how estimation error behaves as the sample size grows under the model conditions.

Worked Example: Comparing the Rate at Two Sample Sizes

Consider a stylized order calculation, not observed data. Suppose at sample size \(n=400\), the denominator is \(0.8n^2\) and the numerator is \(0.6n\). The implied slope error is

$$ \hat{\beta}-\beta \approx \frac{0.6(400)}{0.8(400^2)} = \frac{240}{128000} = 0.001875. $$

If the sample size doubles to \(n=800\) and the same illustrative order constants apply, the numerator becomes \(0.6(800)=480\), while the denominator becomes \(0.8(800^2)=512000\). The corresponding error is

$$ \hat{\beta}-\beta \approx \frac{480}{512000} = 0.0009375. $$

The illustrative error halves when the sample size doubles, as an \(n^{-1}\) rate suggests. Actual numerator and denominator values are random, so this arithmetic illustrates the rate relationship rather than predicting a particular sample’s error.

Worked Example: Endogeneity and a Small Slope Error

Suppose, hypothetically, that the stationary regressor increment \(v_t\) has standard deviation \(1\), the stationary regression error \(u_t\) has standard deviation \(0.5\), and their contemporaneous correlation is \(0.8\). Their covariance is

$$ \operatorname{Cov}(v_t,u_t) = (0.8)(1)(0.5) = 0.4. $$

Thus the regressor innovation and the regression error are endogenous in the sense that they are correlated. Now use illustrative order constants at \(n=500\): suppose the realized OLS numerator is \(0.4n=200\) and the denominator is \(0.7n^2=175000\). The slope error is then

$$ \hat{\beta}-\beta = \frac{200}{175000} \approx 0.001143. $$

This calculation does not assert that the covariance determines either order constant or the realized numerator. It shows how a nonzero innovation-error covariance can coexist with a small slope error when the denominator has the larger \(n^2\) scale. In the asymptotic argument, endogeneity may alter the distribution of the scaled numerator and thus the limit of \(n(\hat{\beta}-\beta)\); it need not prevent \(\hat{\beta}\) from converging to \(\beta\).

Why Superconsistency Matters—and What It Does Not Say

The contrast with a stationary regression is useful. With a stationary regressor, the centered sum of squares is ordinarily order \(n\). If the stationary error is weakly dependent, the cross-product with the regressor is typically order \(\sqrt n\), giving a slope error of order \(1/\sqrt n\). In the cointegrating regression, the integrated regressor instead gives a denominator of order \(n^2\) and a cross-product of order \(n\). This difference is the source of the faster rate.

Superconsistency helps explain why a long-run coefficient can be estimated consistently despite endogeneity between the regressor’s innovations and the stationary error. It does not mean that endogeneity is irrelevant. It can affect the limiting distribution, and it does not justify using ordinary stationary-regression standard errors or reference distributions without further analysis. Nor does consistency alone show that \(x_t\) and \(y_t\) are cointegrated: the stationary-error assumption is part of the model, not a consequence of obtaining a high \(R^2\) or a plausible-looking slope.

Common Pitfall

A common mistake is to reason that correlation between \(v_t\) and \(u_t\) must make OLS inconsistent, just as endogeneity can cause inconsistency in a stationary regression. That conclusion ignores the different orders in the cointegrating regression. Under the conditions given here, the dependence can change the order-\(n\) numerator’s limiting behavior, but the denominator remains order \(n^2\). Their ratio still converges to zero. This correction is conditional: if the regression error is not stationary, or if the integrated regressor is degenerate or the regularity conditions fail, this argument does not establish superconsistency.

Key takeaway: In a correctly specified cointegrating regression with an integrated regressor and a stationary error, OLS has an order-\(n\) denominator and an order-\(n\) numerator. Their ratio gives an order-\(1/n\) slope error. Endogeneity can affect the limiting distribution without preventing consistency.

Check Your Understanding

Use the model and rate argument in this tutorial to answer the following questions.

  1. What stationarity property distinguishes a cointegrating regression from a regression between two unrelated integrated series?
  2. Why is the centered sum of squares of a zero-drift integrated regressor of order \(n^2\), rather than \(n\)?
  3. Using the OLS slope decomposition, identify the numerator and denominator orders that imply the rate-\(n\) result.
  4. How can correlation between \(v_t\) and \(u_t\) affect the asymptotic behavior without preventing consistency?
  5. Does superconsistency by itself establish cointegration or validate ordinary stationary-regression inference? Explain.
Clinical Biostats