Math 2.0

Partial differential equations Definition

Camassa–Holm equation

Builds on Water waves

Definition

Let κ∈ℝ\kappa \in \R be a constant. The Camassa–Holm equation for a real function u(x,t)u(x, t) of x∈ℝx \in \R and t∈ℝt \in \R is ut+2κux−uxxt+3uux=2uxuxx+uuxxx.u_t + 2\kappa u_x - u_{xxt} + 3uu_x = 2u_xu_{xx} + uu_{xxx}. With m=u−uxxm = u - u_{xx}, called the momentum, it takes the equivalent form mt+umx+2mux+2κux=0.m_t + um_x + 2mu_x + 2\kappa u_x = 0.

Remarks

Example: for κ=0\kappa = 0 and c>0c > 0, the peakon u(x,t)=c e−∣x−ct∣u(x, t) = c\,e^{-\abs{x - ct}} is a weak solution. It is not differentiable at the crest, so it solves the equation in the weak sense, written as ut+uux+∂xG∗(u2+12ux2)=0u_t + uu_x + \partial_x G * \left(u^2 + \tfrac{1}{2}u_x^2\right) = 0, with G(x)=12e−∣x∣G(x) = \tfrac{1}{2}e^{-\abs{x}} the kernel of (1−∂x2)−1(1 - \partial_x^2)^{-1}. For the peakon, m=2c δ(x−ct)m = 2c\,\delta(x - ct) is a point mass, since (1−∂x2)e−∣x∣=2δ(1 - \partial_x^2)e^{-\abs{x}} = 2\delta. Non-example: the equation ut+2κux−uxxt+3uux=0u_t + 2\kappa u_x - u_{xxt} + 3uu_x = 0, without the right-hand side, is an equation of Benjamin–Bona–Mahony type; it misses the terms 2uxuxx+uuxxx2u_xu_{xx} + uu_{xxx}, so it is not the Camassa–Holm equation. The two forms agree because mt=ut−uxxtm_t = u_t - u_{xxt} and umx+2mux=3uux−uuxxx−2uxuxxum_x + 2mu_x = 3uu_x - uu_{xxx} - 2u_xu_{xx}.

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Further reading

  1. Web https://en.wikipedia.org/wiki/Camassa%E2%80%93Holm_equation
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DefinesCamassa–Holm equation
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Changed3 November 2026

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