Fokker-Planck Equation

Author

John Robin Inston

Published

August 22, 2026

These lecture notes were written from studying the material provided by Sungsoo Ahn on their personal website. To read this source material please click here.

1 Fokker-Planck Equation

1.1 Definition & Intuition

Consider a \(d\)-dimensional stochastic process \((X_t)_{t\in[0,T]}\) where \(X_t\in\mathbb{R}^d\) with dynamics given by the SDE

\[ \begin{cases} dX_t = f(X_t, t)dt + g(t) dW_t \\ X_0 \sim p_0 \end{cases} \]

where:

  • \(f:\mathbb{R}^d\times [0,T]\to \mathbb{R}^d\) is the drift term.
  • \(g:[0,T]\to \mathbb{R}\) is the diffusion term.
  • \(W_t\) is a \(d\)-dimensional Wiener process.
  • \(p_0\) is the initial distribution of \(X_0\).

The Fokker-Planck Equation (FPE) is the PDE for the marginal density \(p_t(x)\) of \(X_t\) at time \(t\). Intuitively, the SDE describes the evolution of a single particle and the FPE describes the probability of finding the particle at position \(x\) at time \(t\).

The Fokker-Planck Equation (FPE) is a PDE that describes the time evolution of \(p_t(x)\)

\[ \frac{\partial p_t(x)}{\partial t} = \underbrace{-\nabla \cdot (f(x,t)p_t(x))}_{\text{drift advection}} + \underbrace{\frac{g^2(t)}{2}\Delta_x p_t(x)}_{\text{diffusion spread}}, \]

where \(\nabla_x\) is the gradient (divergence) operator and \(\Delta_x = \sum_{i=1}^D \frac{\partial^2}{\partial x_i^2}\) is the Laplacian operator with respect to \(x\).

1.2 Drift Advection

The quantity \(fp_t\) is the probability flux, that is the evolution of the probability density due to the drift term. The negative Divergence of the probability flux measures \(-\nabla\cdot (fp_t)\) measures the net inflow of probability to a small region around \(x\).

For \(d=1\) this becomes the finite difference approximation

\[ \partial_t p \approx -\frac{(f\cdot p)(x+\Delta x)- (f\cdot p)(x)}{\Delta x}. \]

1.3 Diffusion Spread

At each instant, the SDE’s noise perturbs the particle by a symmetric random displacement \(gdW\). The aggregate effect is Gaussian blurring: peaks erode and valleys fill in.

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