Published online by Cambridge University Press: 29 May 2025
We explain how the claims of KPZ scaling theory are confirmed by a recent proof of Borodin and Corwin on the asymptotics of the semidiscrete directed polymer.
1. Introduction
The Kardar–Parisi–Zhang (KPZ) equation [1986] is a stochastic partial differential equation modeling surface growth and, more generally, the motion of an interface bordering a stable against a metastable phase. Scaling theory is an educated guess on the nonuniversal coefficients in the asymptotics for models in the KPZ universality class. Scaling theory has been developed in a landmark contribution by Krug, Meakin and Halpin-Healy [Krug et al. 1992]. The purpose of our article is to explain how to apply scaling theory to the semidiscrete directed polymer. This model has been discussed in depth at the 2010 random matrix workshop at MSRI and, so-to-speak as a spin-off, Borodin and Corwin [2014] developed the beautiful theory of Macdonald processes, which provides the tools for an asymptotic analysis of the semidiscrete directed polymer. As we will establish, scaling theory is consistent with the results of Borodin and Corwin, thereby providing a highly nonobvious control check.
To place the issue in focus, let me start with a simple example. Assume as given the stationary sequence Xj , j ∈ ℤ, of mean zero random variables and let us consider the partial sums
As well studied, it is fairly common that Sn/√n converges to a Gaussian as n→∞, i.e.,
where FG is the distribution function of a unit Gaussian random variable. Here FG is the universal object, while the coefficient D > 0 depends on the law ℙ and
is in this sense model dependent, resp. nonuniversal. However, using stationarity, D is readily guessed as
The KPZ class deals with strongly dependent random variables, for which partial sums are of size n⅓ rather than n½. FG is to be substituted by the GUE Tracy–Widom distribution function, FGUE, which first appeared in the context of the largest eigenvalue of a FGUE random matrix [Forrester 1993; Tracy and Widom 1994].
To save this book to your Kindle, first ensure no-reply@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
Find out more about the Kindle Personal Document Service.
To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.
To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.