Laplace's Equation

Let the heat equation run forever and the temperature stops changing: u_t \to 0. What remains is the steady state, governed by setting the time derivative to zero in u_t = \alpha(u_{xx} + u_{yy}):

\nabla^2 u = u_{xx} + u_{yy} = 0.

This is Laplace's equation, and \nabla^2 (the Laplacian) is the most important operator in physics — it governs steady temperatures, electrostatic potentials, gravitational fields, incompressible flow, and more. Its solutions are called harmonic functions.

The mean-value property

The Laplacian measures how a value compares with the average of its surroundings. Setting it to zero forces every point to equal the average of its neighbours. Made precise, this is the mean-value property: the value of a harmonic function at the centre of any circle equals the average of its values around that circle.

Two consequences follow at once. A harmonic function can have no interior bumps or dips — no local maxima or minima inside the region (that is the maximum principle). And it is completely determined by its values on the boundary: fix the edge, and the smooth "membrane" stretched across the inside is forced. A simple harmonic function is u = x^2 - y^2, since u_{xx} + u_{yy} = 2 - 2 = 0.

A harmonic saddle

A heatmap of u = x^2 - y^2: warm where u > 0, cool where u < 0, pale near zero. It rises along the x-axis and falls along the y-axis — a saddle. Notice there is no isolated hottest or coldest spot in the interior; the extremes all sit on the edge, the hallmark of a harmonic function.