Sheffield's extremal Brownian Gibbs line ensemble conjecture

Let Θ={θssR}\Theta=\{\theta_s\mid s\in\mathbb{R}\} be the horizontal shift group of N×R\mathbb{N}\times\mathbb{R}-indexed line ensembles, acting by

θsLi(x)=Li(x+s)for all iN, xR.\theta_s\mathcal{L}_i(x)=\mathcal{L}_i(x+s)\qquad\text{for all }i\in\mathbb{N},\ x\in\mathbb{R}.

A line ensemble is horizontal shift-invariant if θsL\theta_s\mathcal{L} has the same distribution as L\mathcal{L} for every sRs\in\mathbb{R}. Let GΘ\mathscr{G}_{\Theta} be the set of Brownian Gibbs line ensemble measures L\mathcal{L} such that 21/2Li(x)+x22^{1/2}\mathcal{L}_i(x)+x^2 is horizontal shift-invariant. Let A\mathcal{A} be the Airy line ensemble and define

Lic(x)=12(Ai(x)x2)+c.\mathcal{L}^c_i(x)=\frac{1}{\sqrt{2}}\bigl(\mathcal{A}_i(x)-x^2\bigr)+c.

Sheffield's extremal Brownian Gibbs line ensemble conjecture. As a convex set, the extremal points of GΘ\mathscr{G}_{\Theta} are exactly {LccR}\{\mathcal{L}^c\mid c\in\mathbb{R}\}.

This conjecture would classify stationary Brownian Gibbs line ensembles after the parabolic shift and could provide an invariance principle for convergence to the Airy line ensemble, with applications to KPZ universality. The cited work proves that the displayed Lc\mathcal{L}^c are extremal, reducing the conjecture to uniqueness at each prescribed mean height; the full characterization remains open in the supplied text.

Sources & referencesView supporting material

Primary source

Ivan Corwin and Xin Sun, “Ergodicity of the Airy line ensemble”, arXiv:1405.0464 (2014).

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