The directed-landscape geodesic upper-tail rate conjecture

Let pipi be the LL-geodesic from (0,0)(0,0) to (0,1)(0,1). For ti(0,1/2]t i (0,1/2], define

ι(t)=(2t)5/2(9b+4)+6t2(25b+13)2(2t)3/2(26b+19)482t+243(38t)3(1t)2t2,\iota(t)=\frac{-(2t)^{5/2} (9 b+4)+6 t^2 (25 b+13)-2(2 t)^{3/2} (26 b+19)-48 \sqrt{2t}+24}{3 \left(3-\sqrt{8t}\right)^3 (1-t)^2 t^2},

where

b=72t2+6(2t)3/2143t122t+72(98t)t.b=\frac{\sqrt{72 t^2+6 (2t)^{3/2}-143 t-12 \sqrt{2t}+72}}{(9-8 t) \sqrt{t}}.

The directed-landscape geodesic upper-tail rate conjecture. For t(0,1/2]t\in (0,1/2], as aa\to\infty,

P(π(t)a)=eι(t)a3+o(a3).P(\pi(t)\ge a)=e^{-\iota(t) a^3+o(a^3)}.

In particular, as t0t\to 0,

ι(t)=827/t2+o(1/t2).\iota(t)=\frac8{27}/t^{2}+o(1/t^2).

This conjecture gives the proposed large-deviation rate for a geodesic forced to lie high at time tt; the paper notes that the corresponding heuristic path is not generally piecewise linear when t1/2t\ne1/2, but instead involves two linear pieces and a parabola. The optimization leading to the formula is beyond the scope of the paper, and no resolution is supplied.

Sources & referencesView supporting material

Primary source

Sayan Das, Duncan Dauvergne and Bálint Virág, “Upper tail large deviations of the directed landscape”, arXiv:2405.14924 (2024).

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