The Ornstein-Uhlenbeck Process

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ornstein-uhlenbeck mean-reversion stationary-process gaussian-process

Core Idea

The Ornstein-Uhlenbeck (OU) process solves dX = -θX dt + σ dW, where θ > 0 controls the rate of mean reversion. Its explicit solution X(t) = X(0)e^{-θt} + σ∫₀ᵗ e^{-θ(t-s)} dW(s) is Gaussian with mean X(0)e^{-θt} and variance (σ²/2θ)(1 - e^{-2θt}). As t → ∞, the process converges to a stationary Gaussian distribution N(0, σ²/2θ). The OU process is the prototypical mean-reverting diffusion and the only stationary Gaussian Markov process.

Explainer

The Ornstein-Uhlenbeck process is the simplest non-trivial SDE with an explicit solution and a non-degenerate stationary distribution. It satisfies dX = -θX dt + σ dW, where the drift -θX acts as a restoring force pulling the process toward zero. When X is positive, the drift is negative (pushing down); when X is negative, the drift is positive (pushing up). This is mean reversion — the continuous-time analogue of a discrete-time AR(1) process with coefficient e^{-θ}.

The solution technique uses an integrating factor, paralleling the method for linear ODEs. Define Y(t) = X(t)e^{θt}. By Itô's formula, dY = e^{θt}(dX + θX dt) = e^{θt}σ dW. This is a pure Itô integral with no drift, so Y(t) = X(0) + σ∫₀ᵗ e^{θs} dW(s). Multiplying by e^{-θt} gives the explicit solution: X(t) = X(0)e^{-θt} + σ∫₀ᵗ e^{-θ(t-s)} dW(s). Since this is a deterministic function of Gaussian random variables (the Itô integral of a deterministic function is Gaussian), X(t) is Gaussian with mean E[X(t)] = X(0)e^{-θt} and variance Var(X(t)) = σ²∫₀ᵗ e^{-2θ(t-s)} ds = (σ²/2θ)(1 - e^{-2θt}).

As t → ∞, the mean decays to zero and the variance converges to σ²/(2θ). The process forgets its initial condition exponentially fast (at rate θ) and settles into a stationary Gaussian distribution N(0, σ²/(2θ)). The autocorrelation of the stationary process is R(τ) = (σ²/2θ)e^{-θ|τ|} — exponentially decaying with correlation time 1/θ. This is a fundamental model in physics (velocity of a Brownian particle under friction, by Uhlenbeck and Ornstein's original 1930 paper), finance (the Vasicek interest rate model), and biology (fluctuations around a homeostatic set point).

The OU process occupies a special place in the taxonomy of stochastic processes: it is the unique continuous-time process that is simultaneously Gaussian, Markov, and stationary. Brownian motion is Gaussian and Markov but not stationary (variance grows). A stationary Gaussian process with a non-exponential covariance function loses the Markov property. The exponential covariance is the only one compatible with all three properties, and this pins down the OU process uniquely (up to location and scale parameters). This characterization theorem explains why the OU process appears as the natural building block in so many contexts.

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Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication 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 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-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 IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble 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: KinematicsRotational KinematicsTorqueMoment of InertiaRotational Kinetic EnergyThe Work-Energy TheoremConservation of Mechanical EnergyFirst Law of ThermodynamicsThermodynamic Processes and the PV DiagramIsobaric and Isochoric ProcessesHeat EnginesThermal Efficiency of Heat EnginesRefrigerators and Heat PumpsSecond Law of ThermodynamicsEntropyMicrostates and MacrostatesEnsemble Theory FundamentalsCanonical Ensemble (NVT)Partition Function: Definition and PropertiesThe Canonical Partition Function and Thermodynamic DerivationMaxwell-Boltzmann Distribution and Classical LimitBrownian MotionProperties of Brownian MotionThe Itô IntegralItô's Formula (Itô's Lemma)Stochastic Differential EquationsThe Ornstein-Uhlenbeck Process

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