Hendry's classic econometric warning
Can rainfall explain inflation?
A convincing regression can still describe the wrong economic relationship.
Theoretical introductionSpurious regression → co-integration
Fig. 1 The photograph gives context; it is not econometric evidence.
An unexpected relationship
The model looked strong—then Hendry revealed the variable
Fig. 2 British prices and British rainfall provide the historical setting.
01UK prices and a variable C showed a close nonlinear relationship.
02A quadratic regression gave a good fit and significant coefficients.
03With an AR(1) error model, the fit became “spectacular.”
04C was cumulative rainfall in the United Kingdom.
This case warns about misleading econometric relationships. It is not automatic evidence of co-integration.
Why ordinary inference can fail
Persistence can turn accidental movement into false confidence
1 · REMEMBERSPersistent levels
Earlier shocks remain inside later observations.
2 · ALIGNSApparent co-movement
Two unrelated paths can move together for many periods.
3 · INFLATESMisleading tests
Conventional t-tests use the wrong reference behavior.
4 · MISSTATESFalse economic story
A high R² becomes an explanation the data do not justify.
Fig. 3 The formula can be familiar while its time-series assumptions fail.
Controlled demonstration · synthetic data
Independent random walks still produce a significant OLS slope
Fig. 4 Independent innovations generate β̂ = 0.455, R² = 0.372, and conventional p < 0.001; the residual is not stationary.
Why stationarity matters
Three paths can rise, but they require different treatments
I(0): stable level
Mean and variance stay broadly stable. Shocks fade.
Trend-stationary
A predictable trend changes the mean. Remove the trend.
I(1): stochastic trend
Each shock shifts the future path. Difference once.
Fig. 5 A visible upward path alone does not identify the type of trend.
Random walk → first difference
Differencing removes the accumulated path
Fig. 6 If ΔXt is I(0), then Xt is I(1).
Differencing prevents a naive level regression, but it may remove a genuine long-run relation.
From spurious regression to co-integration
Co-integration asks whether the gap stays stable
Fig. 7 The levels drift, but their estimated long-run gap stays bounded.
ut = Yt − α − βXtX and Y may each be I(1). They are co-integrated when this linear combination is I(0).
Boundary: statistical stability does not prove causation.
The diagnostic difference
The residual reveals whether co-movement is stable
Fig. 8 A spurious residual wanders; a co-integrating residual returns toward a stable mean.
Long-run equilibrium and short-run correction
Yesterday's gap creates today's adjustment
Last period
Y is 10 units above equilibrium.
+10
×
Adjustment speed
λ = −0.30
−0.30
=
This period
Correction contribution
−3
Fig. 9 The error correction model combines a long-run gap with short-run changes.
How to test the relationship
The tests form a sequence, not a checklist
1 · CLASSIFYADF
Is each series I(0) or I(1)?
H₀: unit root
2 · TEST GAPEngle–Granger
Is one estimated residual stationary?
H₀: no co-integration
3 · TEST RANKJohansen
How many long-run relations exist?
H₀: rank ≤ r
4 · MODELECM / VECM
How does the system correct and forecast?
Estimate after rank choice
Fig. 10 Integration order and co-integration evidence come before equilibrium correction.
Choose the method to match the design
Both tests ask whether a long-run combination is stable
Engle–Granger
- Estimate one long-run equation.
- Test its estimated residual.
- Use residual-based critical values.
- Simple for one relation.
Johansen
- Model all variables jointly.
- Use trace and max-eigen tests.
- Allow several long-run relations.
- Choose lags and deterministic terms first.
Fig. 11 A strong level regression is not enough; the long-run combination must be statistically stable.
Time-series econometrics
Spurious regression
or co-integration?
Shared movement is not enough. The residual must stay stable for the long-run relationship to be credible.
DPIC96 × PCECC96FRED data10–15 minutes
Fig. 1 Co-movement in levels does not prove a stable equilibrium.
The research route
Five questions move from illusion to forecasting
01
Spurious regression
Why can unrelated trends look significant?
02
Co-integration
When is a level relationship meaningful?
03
Equilibrium correction
How do short-run gaps close?
04
Statistical tests
What do ADF, Engle–Granger, and Johansen test?
05
Forecasting
Does the equilibrium improve predictions?
The logic is sequential: test persistence before trusting levels, then test equilibrium before using a VECM.
THEORY → TESTS → EVIDENCE → FORECASTS
Question 1 · Spurious regression
Persistence creates false confidence
Fig. 2 The regression formula looks ordinary; its sampling logic is not.
Yt = α + βXt + εt
01Observations are strongly dependent across time.
02OLS mistakes shared drift for repeated evidence.
03The usual t-test no longer has its usual meaning.
A small p-value can describe a statistical artifact, not an economic relationship.