Large deviations of surface height in the $1+1$-dimensional Kardar-Parisi-Zhang equation: exact long-time results for $\lambda H<0$
Pavel Sasorov, Baruch Meerson, Sylvain Prolhac

TL;DR
This paper derives exact large deviation functions for rare height fluctuations in the 1+1D KPZ equation at long times, revealing a crossover between Tracy-Widom and different tail behaviors, supported by numerical analysis.
Contribution
It provides the first exact long-time large deviation function for height fluctuations in the KPZ equation for $ ext{sign}( ext{nonlinearity})<0$, revealing a crossover in tail behavior.
Findings
Identified a crossover from Tracy-Widom to a different tail at large deviations.
Derived exact large deviation functions for $ ext{sign}( ext{nonlinearity})<0$.
Supported analytical results with numerical evaluations.
Abstract
We study atypically large fluctuations of height in the 1+1-dimensional Kardar-Parisi-Zhang (KPZ) equation at long times , when starting from a "droplet" initial condition. We derive exact large deviation function of height for , where is the nonlinearity coefficient of the KPZ equation. This large deviation function describes a crossover from the Tracy-Widom distribution tail at small , which scales as , to a different tail at large , which scales as . The latter tail exists at all times . It was previously obtained in the framework of the optimal fluctuation method. It was also obtained at short times from exact representation of the complete height statistics. The crossover between the two tails, at long times, occurs at as previously conjectured. Our analytical findings are supported by…
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Large deviations of surface height in the -dimensional Kardar-Parisi-Zhang equation: exact long-time results for
Pavel Sasorov
Keldysh Institute of Applied Mathematics, Moscow, 125047, Russia
Baruch Meerson
Racah Institute of Physics, Hebrew University of Jerusalem, Jerusalem 91904, Israel
Sylvain Prolhac
Laboratoire de Physique Théorique; Université de Toulouse, UPS, CNRS, Toulouse, France
Abstract
We study atypically large fluctuations of height in the 1+1-dimensional Kardar-Parisi-Zhang (KPZ) equation at long times , when starting from a “droplet” initial condition. We derive exact large deviation function of height for , where is the nonlinearity coefficient of the KPZ equation. This large deviation function describes a crossover from the Tracy-Widom distribution tail at small , which scales as , to a different tail at large , which scales as . The latter tail exists at all times . It was previously obtained in the framework of the optimal fluctuation method. It was also obtained at short times from exact representation of the complete height statistics. The crossover between the two tails, at long times, occurs at as previously conjectured. Our analytical findings are supported by numerical evaluations using exact representation of the complete height statistics.
Contents
- I Introduction
- II Governing equations
- III Solution
- IV Tale of two tails
- V Numerical evaluation
- VI Discussion
I Introduction
The celebrated Kardar-Parisi-Zhang (KPZ) equation KPZ defines an important universality class of non-equilibrium surface growth HHZ ; Krug ; Corwin ; QS ; S2016 . In dimension this equation,
[TABLE]
describes the evolution of the interface height driven by a Gaussian white noise with zero mean and covariance
[TABLE]
The diffusion term describes relaxation of the interface, whereas the nonlinear term breaks the symmetry in an essential way. At long times the interface width, governed by Eq. (1), grows as , whereas the horizontal correlation length grows as . These power laws – the hallmarks of the KPZ universality class – were confirmed in experiments experiment1 . In the recent years the focus of interest in the KPZ equation shifted toward a more detailed characterization of the fluctuating interface, such as the complete one-point probability distribution of height at a specified time at a specified point in space Corwin ; QS ; S2016 . For the KPZ equation in dimension several groups derived exact representations for a generating function of at any . These remarkable results have been obtained for three classes of initial conditions (and for some combinations of them): flat interface CLD , “droplet” SS ; CDR ; Dotsenko ; ACQ ; Corwin , and Brownian, stationary interface IS ; Borodinetal . In the long-time limit, and for typical fluctuations, converges to the Tracy-Widom (TW) distribution for the Gaussian orthogonal ensemble (GOE) TWGOE for the flat interface, to the TW distribution for the Gaussian unitary ensemble (GUE) TW for the droplet, and to the Baik-Rains distribution BR for the stationary interface. A series of ingenious experiments with liquid-crystal turbulent fronts fully confirmed these long-time results for typical fluctuations experiment2 .
Less is known about large deviations, that is atypically large fluctuations of the surface height, which are described by the far tails of . Extracting these tails from the exact representations requires considerable effort. As of present, there have been only two attempts in this direction, made by Le Doussal et al. for the droplet initial condition: for long DMS and short DMRS times. We will comment on their results as we proceed.
Given the difficulties in extracting the tails from the exact representations, one can look for alternatives that would directly probe the far tails of . One such alternative has existed long before the exact representations for the height distribution of the 1+1 dimensional KPZ equation were found. It appears in different areas of physics under different names: the optimal fluctuation method (OFM), the instanton method, the weak noise theory, the macroscopic fluctuation theory, etc. In the context of the KPZ equation the OFM was employed in Refs. Fogedby1998 ; Fogedby1999 ; Fogedby2009 ; KK2007 ; KK2008 ; KK2009 ; MKV ; KMS ; JKM . The crux of the method is a saddle-point evaluation of the path integral for the KPZ equation conditioned on a specified large deviation. Correspondingly, it requires a small parameter (hence the term “the weak noise theory”). In dimension this small parameter turns out to be proportional to KK2007 ; KK2008 ; KK2009 ; MKV ; KMS ; JKM . As a result, at short times, the OFM correctly describes the complete large-deviation function (LDF) of the interface height. For a whole class of initial conditions, including the three initial conditions described above, the tails of this short-time LDF, determined with the OFM, scale as (for ) and (for ). For the droplet initial condition these tails agree with the corresponding short-time tails obtained by Le Doussal et al. DMRS .
When is the OFM applicable at long times? A necessary condition is that the LDF of height, predicted by the OFM (it is equal to the action of the classical field theory emerging in the OFM) is much larger than unity KK2007 ; KK2008 ; MKV ; KMS ; JKM . At arbitrarily long but finite times this condition is always satisfied sufficiently far in the tails of . It is possible, however, that a dominant contribution to comes from non-saddle-point histories . This is indeed what happens at long times in the part of for the KPZ equation. At small the GOE TW tail, the GUE TW tail and the Baik-Rains tail all scale as , and this is much smaller than predicted by the OFM. The situation is reversed at large . Therefore, it was conjectured in Refs. MKV ; KMS ; JKM that, at , each of the tails of the GOE TW, GUE TW and the Baik-Rains distributions crosses over to the corresponding tail that predicts a higher probability at large .
In this work we employ the exact representations for the droplet initial condition SS ; CDR ; Dotsenko ; ACQ ; Corwin to derive exact LDF of height of the -dimensional KPZ equation at long times. As we show, this LDF describes a smooth crossover between the tail and the tail, in support of the above conjecture.
Here is how the remainder of this paper is structured. In Sec. 2 we present the governing equations and the mathematical formulation of the problem. The problem is solved in Sec. 3. In Sec. 4 we discuss the properties of the LDF of height at . Section 5 presents results of a numerical evaluation of the LDF. Section 6 includes a brief summary and discussion.
II Governing equations
Let us assume that , so that the is the left tail of signlambda . Following Ref. DMS , we will use in this paper the units of distance , time and height . In these units Eq. (1) has and with the noise covariance (2). We consider the “droplet” initial condition, conveniently represented by the limit of parabolic interface KMS :
[TABLE]
We will study the probability distribution of the shifted height at the origin at time ,
[TABLE]
The term is universal, whereas the term is not: the coefficient depends on the exact way of introducing a finite spatial correlation length (an ultraviolet cutoff) of the Gaussian noise Hairer .
The exact representation for is the following SS ; CDR ; Dotsenko ; ACQ . Introduce the generating function
[TABLE]
where the averaging is over the distribution . This generating function is given by a Fredholm determinant:
[TABLE]
where the kernel, corresponding to the operator , is
[TABLE]
is the projector on the interval , and is the Airy function. Using this representation for typical fluctuations, , one obtains at long times , where is given by the GUE TW distribution SS ; CDR ; Dotsenko ; ACQ ; Corwin . For the far right tail of one obtains DMS :
[TABLE]
This leading-order asymptote coincides with the positive tail of the GUE TW distribution. It was derived from Eqs. (5)-(7) in Ref. DMS . It was also obtained in Ref. KMS by applying the OFM to the KPZ equation with the parabolic initial condition (3) for arbitrary , including the limits of and different .
The left tail of the GUE TW probability density, conjectured in TW and proved in DIK2008 , is equal to
[TABLE]
where is the Riemann zeta function, and . As we will see, the far left tail of is quite different from the TW left tail (9). To determine the far left tail of , , we will use an alternative exact representation, established in Ref. ACQ . The logarithm of the generating function can be expressed as
[TABLE]
where
[TABLE]
The function of three arguments and satisfies a nonlinear integro-differential equation,
[TABLE]
subject to the boundary condition
[TABLE]
As this boundary condition is specified at plus infinity, we will need to know the behavior of in its right tail, . This behavior, at , has been recently established in Ref. DMS . Omitting pre-exponential factors,
[TABLE]
Our calculation of the LDF of height for the left tail, , relies on an asymptotically exact solution of the problem (12) and (13), and asymptotic evaluation of the integrals (10) and (11), at .
III Solution
We are interested in the regime of and (and, therefore, ). Let us introduce the new variables
[TABLE]
and make the ansatz
[TABLE]
where . As it turns out, the function is independent of . We will not use this property in our calculations until later, but will suppress the subscript in the function and in the related functions , and which we will introduce shortly. In the new variables Eq. (12) takes the form
[TABLE]
where . The boundary condition (13) becomes
[TABLE]
where we have used the asymptotic of the Airy function for a large positive argument DLMF . In its turn, Eq. (11) can be rewritten as
[TABLE]
For given (a monotonic function) and , Eq. (17) is the Schrödinger equation for the wave function of a quantum particle with mass and energy moving in the potential . The factor in front of the square brackets plays the role of . Employing the small parameter , we will solve Eq. (17) in the WKB approximation. As we will see, under some condition that we will specify, the WKB approximation holds for all except in a small vicinity of the (unique) “classical turning point” of the “particle” . The turning point is defined by the equality . Let us introduce the classical momentum of the “particle”,
[TABLE]
It is a (positive) real function of in the classically allowed region and a purely imaginary function in the classically forbidden region . The wave function oscillates in the classically allowed region, and decays exponentially in the classically forbidden region. The general form of the WKB solution is well known LL ; Bender :
[TABLE]
To determine the function , we use the boundary condition (18). This yields
[TABLE]
which can be rewritten as
[TABLE]
The second integral in the right hand side of Eq. (24) converges at because rapidly goes to zero as [see Eq. (14)] and therefore rapidly goes to zero as . Now we should plug the asymptotic solutions (21) and (22) into Eq. (19) and solve the resulting equation for . Continuing to use the large parameter , we make the following simplifications:
- •
We neglect in Eq. (24) an exponentially small contribution of to the integral in the region of and obtain
[TABLE]
- •
We neglect small contributions to the integral in Eq. (19) which come from (i) the classically forbidden region and (ii) the small non-WKB region around the classical turning point .
- •
For , the dominant contribution to the integral (11) comes from the region of . Correspondingly, the dominant contribution to the integral (19) comes from the region of . Therefore, we can approximate at and neglect an exponentially small contribution from the region .
- •
We replace the rapidly oscillating factor in Eq. (19), coming from Eq. (21), by .
As a result, Eq. (19) takes the form of a formidable-looking nonlinear integral equation for :
[TABLE]
Its solution, however, is amazingly simple and, as we announced earlier, independent of :
[TABLE]
Miraculously, this not only “kills” the -dependent exponent in Eq. (26),
[TABLE]
but also solves the remaining equation
[TABLE]
For the WKB approximation to be valid, we must demand that the characteristic WKB action be large LL ; Bender :
[TABLE]
Using Eq. (28), we can rewrite this condition as
[TABLE]
Further, for the WKB solution to give a dominant contribution to the integral over in Eq. (11), the strong inequality (30) must hold for , the upper integration bound in Eq. (29). For we obtain , and the applicability condition is , or . For the applicability condition is simply .
Going back to Eq. (16), we see that is a self-similar function of its arguments:
[TABLE]
Now we are in a position to evaluate from Eq. (10). As , we can write
[TABLE]
where
[TABLE]
This leads to the exact LDF we are after:
[TABLE]
IV Tale of two tails
The leading-order asymptote yields the height distribution
[TABLE]
Although the WKB approximation demands , the leading-order result (35) actually holds under a weaker condition , because it coincides with the left tail of the Tracy-Widom distribution that describes typical fluctuations of height at long times. The asymptote (35) was obtained in Ref. DMS . Furthermore, the authors of Ref. DMS arrived at a conclusion that this asymptote holds at . This conclusion is in contradiction with our exact large-deviation function (33) and (34) wrongscaling .
The leading-order asymptote of is . Correspondingly, the asymptote of the height distribution is the following:
[TABLE]
This asymptote was obtained in Ref. KMS by using the OFM, and in Ref. DMRS in the short-time limit . As it is clear now, the tail (36) is present at all times . This tail is independent of the diffusion coefficient KMS . Indeed, in the physical variables one obtains
[TABLE]
Therefore, we will call this far-tail asymptote ‘diffusion-free’. For comparison, the tail (35) in the physical variables is
[TABLE]
Here too the KPZ nonlinearity dominates over the diffusion, but the tail still depends on .
The exact LDF (34) describes a smooth crossover between the Tracy-Widom tail (35) and the far tail (36) in the region of . For reference purposes, we present more accurate small- and large- asymptotics:
[TABLE]
V Numerical evaluation
The probability distribution of can be extracted from the exact generating function (5) and (6) CDR . It is equal to
[TABLE]
where is given by the difference of two Fredholm determinants,
[TABLE]
The operators and have respective kernels and
[TABLE]
The central part of , corresponding to typical fluctuations, was computed numerically in Ref. PS2011 using the method introduced by Bornemann in B2010 for accurate evaluations of Fredholm determinants. Here we push the computations further in order to reach the left tail of .
Bornemann’s method consists in approximating a Fredholm determinant by evaluating the multiple integrals in the Fredholm expansion by Gauss-Legendre quadrature with points, which is exact for integrands of degree at most , and converges exponentially fast with quite generally. The approximate Fredholm expansion with discretized integrals can then be resummed as a single determinant, and one has
[TABLE]
For Gauss-Legendre quadrature the points are the zeroes of the -th Legendre polynomial
[TABLE]
and the corresponding weights are given by
[TABLE]
An additional step is needed if the kernel has infinite support, since Gauss-Legendre quadrature requires integrals on a finite segment. This can be remedied by a change of variables in the kernel.
An additional difficulty in the application of Bornemann’s method to Eq. (40) is that the kernel is itself given by an integral (42). We also evaluate this integral by Gauss-Legendre quadrature, after a change of variables which maps the interval to a finite segment. We used for the Gauss-Legendre quadrature of both the Fredholm determinants and the kernel .
The computation of the left tail of is much more demanding than the computation of the central part of the distribution PS2011 , where it was sufficient to use and double-precision numbers. In order to go deeper into the left tail, we had to evaluate for larger negative values of , for which the approximation (43) of the Fredholm determinants in (41) converges more slowly as increases. Besides, the oscillations of for lead to cancelations in the integration over in Eq. (40), and require higher floating-point precision. Both issues of course increase the computation time. We found that and floating-point numbers with digits was a good compromise between how far to the tail we could go and how long the computation would take. With these parameters, each value of took about hours with ‘Mathematica’ Wolfram on a single core of a personal computer. The integral over in (40) is then evaluated by simple rectangular quadrature between and with step .
With the numerical scheme described above, we evaluated the left tail of for and . The results are plotted in Figs. 1 and 2 alongside with the exact LDF from Eq. (33) and the Tracy-Widom asymptotic. The agreement between the numerical results and the exact LDF is rather good. As one can see from Fig. 1, a deviation from the Tracy-Widom asymptotic appears already at quite small , and this deviation is well described by the exact .
VI Discussion
We derived exact LDF of height of the 1+1 KPZ equation with the droplet initial condition at long times for . This LDF, see Eqs. (33) and (34), describes a smooth crossover from the Tracy-Widom distribution tail at small , which scales as , to a diffusion-free tail at large , which scales as . The diffusion-free tail exists at all times , but it is “pushed” to larger and larger as time grows.
Le Doussal et al. DMS argued that, at long times, models in the KPZ universality class exhibit a third-order phase transition from a strong-coupling to a weak-coupling phase. Their argument was based on Eq. (35). Here we have shown that the asymptotic (35) is not valid at . Still, their interpretation of the large deviations of height in terms of a third-order phase transition holds. Indeed, sufficiently close to the “critical point” one still has
[TABLE]
In the light of our results, at , the strong-coupling phase becomes diffusion-free. Here the height fluctuations are dominated by a large-scale optimal noise history KMS .
The diffusion-free tails at very large negative have been also obtained with the OFM for the KPZ equation in dimensions with other types of initial conditions KK2007 ; KK2009 ; MKV ; KMS ; JKM , including the flat and stationary initial conditions. It would be interesting to reproduce them from exact representations of the height distribution at long times.
Finally, the KPZ universality class is defined in terms of typical fluctuations at long times. It should not come as a surprise, therefore, that statistics of large deviations are in general different among different models belonging to the KPZ universality class.
ACKNOWLEDGMENTS
B.M. acknowledges financial support from the Israel Science Foundation (grant No. 807/16).
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