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Stationarity and Unit Roots

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Probability AxiomsRandom Variables+4 moreSerial Correlation (Autocorrelation) in Regression
stationarity unit-root ADF-test I(1) random-walk

Core Idea

A time series is (weakly) stationary if its mean, variance, and autocovariances do not depend on time. Many economic series — GDP levels, price indices, exchange rates — are non-stationary: they have stochastic trends, drifting means, and growing variance. A random walk y_t = y_{t−1} + ε_t has a 'unit root' and is integrated of order 1 (I(1)); its first difference Δy_t = ε_t is stationary. The Augmented Dickey-Fuller (ADF) test formally tests for unit roots. Regressing one I(1) series on another without cointegration produces spurious results; the standard remedy is to work in differences.

How It's Best Learned

Apply the ADF test to GDP levels and then to GDP growth rates — levels typically fail the test (unit root not rejected) while growth rates pass. Simulate a random walk and AR(1) with ρ<1 to see the difference visually.

Common Misconceptions

Explainer

Your time series background gives you the tools to model how economic variables evolve over time. The next essential question is whether a series behaves consistently over time — whether its statistical properties are stable or drifting. A series is weakly stationary if its mean, variance, and autocovariances are all constant over time. Think of coin flip outcomes: no matter when you start recording, the mean hovers at 0.5 and the variance stays fixed. A stationary series has a stable "center of gravity" it keeps returning to after shocks. Many standard results in time series econometrics — the law of large numbers, the central limit theorem — require stationarity to hold. When stationarity fails, those results break down, and so do many standard regression techniques.

The contrast is a random walk: y_t = y_{t−1} + ε_t, where ε_t is white noise. Each period, the series moves by a random shock — and here is the key: the shock is permanent. There is no mean to return to. After a positive shock today, the series simply starts from a higher level and wanders from there. The variance of a random walk grows without bound as time passes (it equals σ²t after t periods), which violates the stationarity requirement of constant variance. This is what it means to be integrated of order 1, or I(1): one differencing operation is needed to produce a stationary series. The first difference Δy_t = y_t − y_{t−1} = ε_t is simply white noise — stationary. GDP levels, stock prices, exchange rates, and many price indices behave like random walks (or near-random walks). GDP growth rates, stock returns, and inflation rates tend to be stationary.

The practical danger of non-stationarity is spurious regression. If you regress one I(1) series on another unrelated I(1) series — say, U.S. GDP on the population of Iceland — you will typically find a high R² and a statistically significant slope coefficient, even though no true relationship exists. Both series are simply trending over time, and OLS interprets their shared trend as a relationship. Your probability theory and random variables background helps here: you know that the sampling distributions of OLS estimates change fundamentally when variables are I(1), invalidating the usual t- and F-test critical values. This is why checking for stationarity before running regressions is not optional.

The Augmented Dickey-Fuller (ADF) test formalizes this check. The null hypothesis is that the series has a unit root (is non-stationary); rejection of the null means stationarity. The ADF regression tests whether the autoregressive coefficient is equal to one by running the transformed regression Δy_t = α + ρ*y_{t−1} + lagged differences + ε_t and testing whether ρ = 0. Note the counterintuitive direction of the test: you need evidence *against* the null (unit root) to conclude stationarity, and failing to reject does not prove the series is non-stationary — it may just mean you have insufficient power. If a series is I(1), the standard remedy is to work in differences: first-differencing removes the stochastic trend, produces a stationary series, and restores the validity of standard inference. The tradeoff is that differencing also removes all long-run level information — the cointegration framework, covered next, recovers long-run relationships without discarding them.

Practice Questions 5 questions

Prerequisite Chain

Understanding ZeroThe Number ZeroCounting to FiveCounting to 10Counting to 20Counting a Set of Objects Up to 20Cardinality: The Last Number CountedMatching Numerals to QuantitiesSubitizing Small QuantitiesAddition Within 10Number Bonds to 10Addition Within 20Doubles and Near DoublesDoubles Facts Within 10Near Doubles Facts Within 20Mental Math Strategies for AdditionMental Math: Adding and Subtracting TensAddition Within 100Repeated Addition as MultiplicationMultiplication as Equal GroupsMultiplication: ArraysBasic Multiplication Facts (0s, 1s, 2s, 5s, 10s)Multiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Multiplication and Division Fact FamiliesRelationship Between Multiplication and DivisionDivision Facts as Inverse of MultiplicationRemainders and Quotients in DivisionDivision Word ProblemsMulti-Step Word ProblemsSolving Multi-Step Word ProblemsMultiplication Word ProblemsDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueIntegers and the Number LineComparing and Ordering IntegersAbsolute ValueAdding IntegersSubtracting IntegersMultiplying IntegersDividing IntegersUnit RatesProportionsPercent ConceptConverting Between Fractions, Decimals, and PercentsOperations with Rational NumbersTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionSine, Cosine, and Tangent RatiosTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIndefinite IntegralsBasic Integration RulesRiemann SumsDefinite Integral DefinitionDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsCenter of MassConservation of Linear MomentumElastic CollisionsInelastic CollisionsCoefficient of RestitutionCollision Analysis and Real-World ApplicationsTwo-Body Collisions in the Center-of-Mass FrameReduced Mass and Two-Body ProblemsKinematics in Two DimensionsProjectile MotionCircular Motion: KinematicsSimple Harmonic MotionIntroduction to Differential EquationsSolow Growth ModelCapital Accumulation and the Golden RuleInvestment Demand and Capital FormationAggregate DemandThe AS-AD ModelBusiness CyclesTime Series Data: Structure and ConceptsStationarity and Unit Roots

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