Dubrovin's universality conjecture for Hamiltonian perturbations

Let u0=u0(x,t)u_0=u_0(x,t) be a smooth solution to the unperturbed equation

ut+a(u)ux=0,u_t+a(u)u_x=0,

defined for all xRx\in\mathbb R and 0t<t00\leq t<t_0, and monotone in xx for any tt. Consider a Hamiltonian perturbation

ut+a(u)ux+ϵ[b1(u)uxx+b2(u)ux2]+ϵ2[b3(u)uxxx+b4(u)uxuxx+b5(u)ux3]+=0,u_t+a(u)u_x+\epsilon\left[b_1(u)u_{xx}+b_2(u)u_x^2\right]+\epsilon^2\left[b_3(u)u_{xxx}+b_4(u)u_xu_{xx}+b_5(u)u_x^3\right]+\cdots=0,

where the bjb_j are smooth functions. A gradient catastrophe occurs at a point (x0,t0)(x_0,t_0) of the unperturbed solution.

Dubrovin's universality conjecture. There exists a solution u=u(x,t;ϵ)u=u(x,t;\epsilon) to the perturbed equation on the same domain with

u(x,t;ϵ)=u0(x,t)+ϵ2u1(x,t)+ϵ4u2(x,t)+o(ϵ4),u(x,t;\epsilon)=u_0(x,t)+\epsilon^2u_1(x,t)+\epsilon^4u_2(x,t)+o(\epsilon^4),

where u1u_1 and u2u_2 can be written down explicitly. The equation PI2P_I^2 has a unique solution y=y(x,T)y=y(x,T) smooth for all real xx and all values of TT. The generic solution can be extended up to t=t0+δt=t_0+\delta for sufficiently small positive δ=δ(ϵ)\delta=\delta(\epsilon) and, near (x0,t0)(x_0,t_0), satisfies

u(x,t;ϵ)=u0(x,t)+aϵ2/7y(bϵ6/7(xc(tt0)x0),dϵ4/7(tt0))+O(ϵ4/7),u(x,t;\epsilon)=u_0(x,t)+a\epsilon^{2/7}y\left(b\epsilon^{-6/7}(x-c(t-t_0)-x_0),d\epsilon^{-4/7}(t-t_0)\right)+O(\epsilon^{4/7}),

for constants a,b,c,da,b,c,d depending on the hyperbolic equation, the solution uu, and the perturbation. Here yy is the unique smooth solution specified above.

This conjecture predicts universal behavior near gradient catastrophe for generic Hamiltonian perturbations and connects the small-dispersion limit with the special pole-free solution of the fourth-order analogue of the Painlevé I equation. The source attributes the conjecture to Dubrovin; its resolution status is not specified here.

Sources & referencesView supporting material

Primary source

T. Claeys and M. Vanlessen, “The existence of a real pole-free solution of the fourth order analogue of the Painleve I equation”, arXiv:math-ph/0604046 (2006).

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