For , compute :
- elliptic (Laplace)
- parabolic (heat)
- hyperbolic (wave)
Why this is asked: B² − 4AC decides the type pointwise; the sign can change with the point (Tricomi). Reduce to canonical form by solving the characteristic ODE dy/dx = (B ± √(B²−4AC))/2A.
For the sign of decides the type, the type decides the behaviour, and the type can change from point to point.
Because it is a one-line computation that determines everything else about an equation, and because the coefficients may depend on and — so "what type is this" is often really "where is it each type", which options rarely make explicit.
For the second-order equation with principal part :
The names come from conic sections, and the analogy is exact: the characteristic equation has no real roots, one, or two, giving zero, one or two families of real characteristic curves.
Elliptic — Laplace, . No real characteristics. Solutions are as smooth as possible: harmonic functions are analytic, satisfy the mean value property and the maximum principle, and are determined by boundary values on a closed curve. Boundary value problems, not initial value problems.
Parabolic — heat, . One characteristic family, constant. Smooths immediately and irreversibly: discontinuous initial data becomes analytic for any , and information propagates at infinite speed. Well posed forwards in time only — the backward heat equation is the standard ill-posed problem.
Hyperbolic — wave, . Two families, . Preserves kinks: a corner in the initial data travels along a characteristic and stays a corner. Finite propagation speed, and the domain of dependence is a triangle. Reversible in time.
has . Elliptic for , parabolic on the axis, hyperbolic for — the Tricomi equation, and the standard example that "type" is a local property. When a question gives variable coefficients, the answer is a region.
Change variables to along the characteristics:
The recipe: solve for , integrate to get the characteristic curves, and use them as the new coordinates. In the parabolic case there is only one family, so the second coordinate is chosen freely — any function independent of the first.
d'Alembert is the hyperbolic canonical form paying off: becomes in , , so
and with initial data , ,
"The type is a property of the equation." It is a property of the equation at a point. is all three types in different regions.
"The heat equation can be solved backwards." It is ill-posed backwards: arbitrarily small changes in the final data produce arbitrarily large changes earlier. The wave equation is reversible; the heat equation is not.
"Discontinuities propagate in all three." Only hyperbolic. Parabolic and elliptic equations smooth data immediately, which is why the heat kernel is analytic for every .
"The wave equation has infinite propagation speed." Finite, . The heat equation has infinite speed — a bump anywhere makes everywhere at once, which is physically odd and mathematically true.
"An initial value problem is well posed for Laplace." It is not — Hadamard's example shows small Cauchy data producing unbounded solutions. Elliptic equations take boundary conditions.
"The classification needs constant coefficients." Only the coefficients of the second-order terms matter, and they may vary. Lower-order terms never affect the type.
See it move
The trap here
“A PDE has a single type throughout its domain” — false
The Tricomi equation
Elliptic in the upper half-plane, hyperbolic in the lower, parabolic on the axis.
Check yourself
The partial differential equation xy ᵧ is
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