The Competition of Roughness and Curvature in Area-Constrained Polymer Models
Riddhipratim Basu, Shirshendu Ganguly, and Alan Hammond

TL;DR
This paper investigates how local interface fluctuations and global curvature constraints interact in KPZ universality class models, revealing a new exponent triple for constrained paths in directed last passage percolation.
Contribution
It introduces a novel analysis of area-constrained paths in KPZ models, showing a different set of fluctuation exponents than classical Brownian-based models.
Findings
The local interface fluctuation exponent is 2/3.
Facet lengths follow an exponent of 3/4.
Inward deviation has an exponent of 1/2.
Abstract
The competition between local Brownian roughness and global parabolic curvature experienced in many random interface models reflects an important aspect of the KPZ universality class. It may be summarised by an exponent triple representing local interface fluctuation, local roughness (or inward deviation) and convex hull facet length. The three effects arise, for example, in droplets in planar Ising models (Alexander, '01, Hammond, '11,'12). In this article, we offer a new perspective on this phenomenon. We consider directed last passage percolation model in the plane, a paradigmatic example in the KPZ universality class, and constrain the maximizing path under the additional requirement of enclosing an atypically large area. The interface suffers a constraint of parabolic curvature as before, but now its local structure is the KPZ fixed point polymer's rather than…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
The competition of roughness and curvature in area-constrained polymer models
Riddhipratim Basu
Riddhipratim Basu, Department of Mathematics, Stanford University, Stanford, CA, USA
,
Shirshendu Ganguly
Shirshendu Ganguly, Department of Statistics, UC Berkeley, Berkeley, CA, USA
and
Alan Hammond
Alan Hammond, Departments of Mathematics and Statistics, UC Berkeley, Berkeley, CA, USA
Abstract.
The competition between local Brownian roughness and global parabolic curvature experienced in many random interface models reflects an important aspect of the KPZ universality class. It may be summarised by an exponent triple representing local interface fluctuation, local roughness (or inward deviation) and convex hull facet length. The three effects arise, for example, in droplets in planar Ising models [20, 21, 19, 2]. In this article, we offer a new perspective on this phenomenon. We consider directed last passage percolation model in the plane, a paradigmatic example in the KPZ universality class, and constrain the maximizing path under the additional requirement of enclosing an atypically large area. The interface suffers a constraint of parabolic curvature as before, but now its local structure is the KPZ fixed point polymer’s rather than Brownian. The local interface fluctuation exponent is thus two-thirds rather than one-half. We prove that the facet lengths of the constrained path’s convex hull are governed by an exponent of , and inward deviation by an exponent of . That is, the exponent triple is now in place of . This phenomenon appears to be shared among various isoperimetrically extremal circuits in local randomness. Indeed, we formulate a conjecture to this effect concerning such circuits in supercritical percolation, whose Wulff-like first-order behaviour was recently established by Biskup, Louidor, Procaccia and Rosenthal in [9].
Contents
- 1 Introduction and main results
- 2 Important probability estimates
- 3 A Variational Approach to the Constrained Geodesic
- 4 Law of large numbers
- 5 Lower Bound for Scaling Exponents
- 6 Upper Bound for Scaling Exponents
- 7 Proofs of some of the earlier statements
1. Introduction and main results
The geometric properties of random interfaces are a vast arena of study in rigorous statistical mechanics. Two important classes of interface models are phase separation models that idealize the boundary between a droplet of one substance suspended in another, and last passage percolation models, where a directed path in independent local randomness maximizes a random weight determined by the environment.
One of the best known mathematical examples of phase separation is the two dimensional supercritical Ising model in a large box with negative boundary condition. Conditioned to have an atypically high number of positive spins in the box, the vertices in the plus phase tend to form a droplet surrounded by a sea of negative spins. The random phase boundary of such a droplet has been the object of intense study. Wulff proposed that the profile of such constrained circuits would macroscopically resemble a dilation of an isoperimetrically optimal curve. This was established rigorously in [15] and [23]. Via the FK representation of the Ising model, one observes a similar situation in the setting of subcritical two dimensional percolation, where the analogous object is the boundary of the cluster containing the origin after this cluster is conditioned to be atypically large. The Wulff shape captures the macroscopic profile of the circuit in such models, but what of fluctuations? Several definitions may be considered that seek to capture fluctuation behaviour on the part of the circuit, including the deviation in the Hausdorff metric of the convex hull of the circuit from an appropriately scaled Wulff shape. Alternative definitions, more local in nature, serve better to capture the transition in circuit geometry from local Brownian randomness to a smoother profile dictated by the constraints of global curvature. In fact, a pair of definitions is natural, one to capture the longitudinal distance at which the transition takes place, and the second to treat the orthogonal inward deviation of the interface at this transition scale. To specify the characteristic longitudinal distance, we may note that the convex hull of the circuit is a polygonal path that is composed of planar line segments or facets; we may treat the typical or maximum facet length as a barometer of the transition from the shorter scale of local randomness to the longer scale of curvature. Latitudinally, we may note that any point in the circuit has a local roughness, given by its distance from the convex hull boundary. The typical or maximum local roughness along the circuit is a latitudinal counterpart to facet length. Alexander [2], and Hammond [20, 21, 19] analysed such conditioned circuit models and determined that when the area contained in the circuit is of order , so that the circuit has diameter of order , facet length and local roughness scale as and . A similar situation is witnessed when a parabola is subtracted from a two-sided Brownian motion . When is large, facets of the motion’s convex hull have length and inward deviation . This phenomenon is expected to be universal when the local structure of the interface is Brownian and other examples include a Brownian bridge pinned at and and conditioned to remain above the semi-circle of radius centred at the origin which was analysed by Ferrari and Spohn [17].
The second class of random geometric paths we have mentioned are last passage percolation models. These models form part of a huge, Kardar-Parisi-Zhang, class of statistical mechanical models in which a path through randomness is selected to be extremal for a natural weight determined by that randomness. The maximizing paths are often called polymers. The fluctuation behaviour of a length polymer with given endpoints may be gauged either in terms of the scale of deviation of its weight from the mean value, or by the scale of deviation of say the polymer’s midpoint from the planar line segment that interpolates the polymer’s endpoints. The two deviations are given by scales and . These were first proved for planar Poissonian directed last passage percolation, in the seminal work of Baik, Deift and Johansson [4]. Since then, this and other integrable models in the same KPZ universality class have been extensively analysed and detailed information about this model, both geometric and algebraic, has been obtained [24, 26, 27].
It is of much interest to study models that combine phase separation and path minimization (or maximization) in random environment. Consider an environment with local independent randomness, and the circuit through that randomness whose weight determined by that randomness is extremal among those circuits that trap a given area. Studying the random geometry of such a circuit is a problem of extremal isoperimetry. Taking the randomness to be supercritical percolation, Itai Benjamini conjectured the first-order, Wulff-like behaviour of the boundary of the set in the supercritical percolation cluster attaining the so called anchored expansion constant. This was proved by [9] by showing that the curve in the limit solves a natural isoperimetric variational problem; this has recently been extended to higher dimensions by Gold [18]. Given the role of facet length and local roughness in capturing the local random to global curvature transition in circuit geometry, the natural next problem is to understand the scaling exponents of such objects, which is the pursuit we undertake in this paper. Our choice of model preserves the qualitative features of the problem of interface fluctuation in an isoperimetrically extremal droplet in supercritical percolation and at the same time ensures that key algebraic aspects of KPZ theory can be harnessed to yield sharp fluctuation estimates.
The particular setting we consider in this paper is planar Poissonian directed last passage percolation. To impose the required properties, we study this model under a quadratic curvature constraint: that is, we force the best path to move away from the straight line and have a quadratic curvature on the average. This is done naturally by considering the longest upright path in a Poissonian environment joining and which has the additional area trap property that the area under the curve is at least for some . Note that from the discussion above it follows that the unconstrained longest path stays close to the diagonal and hence encloses area . Postponing precise statements until later (see Section 1.2), our main results quantify the competition between the global parabolic nature and local behaviour guided by KPZ relations of the contour. They show that the maximum facet length of the contour’s least concave majorant scales as , while the inward deviation from the concave majorant (local roughness) scales as .
We also establish a law of large numbers for the length of the optimal path. The proof proceeds by setting up a variational problem, as is natural in such contexts (see [12], [9]). Perhaps surprisingly, however, the problem turns out to have a very explicit solution. The geometric information about the limit shape of the constrained polymer is also used as input in some of the arguments about fluctuations. The question of fluctuation in the context of isoperimetrically extremal circuits in supercritical percolation can be formulated as a first passage percolation analogue of our setting of last passage percolation. Although the first passage percolation model is not exactly solvable, it, too, is believed to be in the KPZ universality class, and the geodesics there are believed to have the same scaling of transversal fluctuation as in our case (see [3] and the references therein). Thus our results suggest that a certain universality is being witnessed and, according to this belief, we formulate a conjecture concerning percolation. We elaborate on this and a number of other interesting questions in Section 1.4.
Finally, we discuss briefly the key inputs used in our paper and how it contrasts with the other examples of fluctuation results already mentioned. The results in [20, 21, 19] crucially used the refined understanding and geometric estimates for percolation clusters while a study of area trapping planar Brownian loop [22] used well known estimates for Brownian motion. Exact expressions involving Brownian motion conditioned to stay over a parabola was also the key ingredient in the proofs in [17]. However, in our setting, even though the unconstrained model has integrable properties, the lack of general geometric understanding as one deviates slightly from integrable models causes a big challenge for us. Nonetheless, using certain known facts about the unconstrained model and their robust variants established recently in [8] as blackbox estimates, we rigorously establish local roughness exponents for our model which we henceforth call the Area Trapping Polymer model (see next section for precise definitions). Thus, this work is an example where one can use inputs from the integrable literature to make geometric conclusions about settings which are beyond the exactly solvable world (see also [8]). We believe a general program of developing such geometric arguments would lead to more robust proofs which could work for settings that are non-integrable but are variants of solvable models.
1.1. Model Definitions
We now recall the planar Poissonian directed last passage percolation model.
Let be a homogeneous rate one Poisson Point Process (PPP) on the plane. A partial order on is given by if and . For , a directed path from to is a piecewise linear path that joins points where each for (throughout the article we will adopt the standard notation ) is a point of . Define the length of , denoted , to be the number of -points on .
Definition 1.1**.**
Define the last passage time from to , denoted by , to be the maximum of as varies over all directed paths from to . There may be several maximizing paths between and , and throughout the paper we will refer to the top most path (it is easy to see that the top most path is well defined here) among those, as the geodesic between and and denote it by .
We will often call as the polymer between and and as the polymer length/weight respectively. Next we introduce a constraint in this classical model.
1.1.1. Area Trapped by a path
Consider a path between the origin and a point in the positive quadrant. The area trapped by the path , denoted by , is defined to be the area of the closed polygon determined by the -axis, the vertical line segment joining to together with the line segments of the path . Let denote the geodesic between and . Well-known facts about Poissonian LPP readily imply that asymptotically almost surely. We constrain the model and consider maximizing paths subject to trapping a much larger area. To this end fix , and let
[TABLE]
It is easily seen that, among the paths that attain this maximum, there is almost surely exactly one that traps the least area. This path will be called . We will write provided that the context clarifies the value of in question. We shall call the constrained (or -constrained) geodesic. In analogy with the phase separation example in percolation mentioned the introduction, it might seem more natural to consider the family of down right paths joining and since all of these curves enclose the origin. However because of the obvious underlying symmetry, and to take advantage of standard notational conventions, throughout the sequel we will consider the contour joining the origin to the point .
Our main objects of interest are two quantities that measure local regularity of the constrained geodesic . The following definitions are illustrated by Figure 2.
Definition 1.2**.**
Let denote the convex hull of the polygon determined by the path and the coordinate axes. Let denote the closure of the polygonal part of the boundary of between and above the -axis. Thus is the least concave majorant of and is an union of finitely many line segments. These segments will be called facets. Define maximum facet length of , denoted to be the maximum Euclidean length of the facets. For , let denote the distance from to . This is a natural notion of the local roughness at . Define the maximum local roughness of , denoted by
[TABLE]
In the following subsections we present our main results. We first state our results regarding the fluctuation exponents of .
1.2. Scaling exponents for geodesic geometry
The sense in which we capture the exponents is stronger and easier to state for the lower bounds, and so we begin with them.
Theorem 1.3**.**
Fix and . Then there exists such that for all large enough
[TABLE]
As we have mentioned, the scaling exponent for transversal fluctuation of point-to-point geodesic in unconstrained Poissonian last passage percolation is known to be This fact, put together with the above theorem yields the following lower bound on maximum local roughness.
Theorem 1.4**.**
Fix and . Then there exists such that for all large enough
[TABLE]
Regarding the matching upper bound, we prove that, with high probability, there exists a dense set of for which the maximum length of the facets away from the boundary is bounded above by . To make this precise, fix , and consider a facet in with endpoints and recorded in clockwise order. Setting , let denote the acute angle that makes with the -axis and , the acute angle that makes with the -axis; see Figure 2.
Definition 1.5**.**
The facet is called -interior if .
Note that the union of the -interior facets forms a polygonal path. (The union could be empty, but we will infer later from Theorem 1.10 that this event has an exponentially small probability.) 111Note that at this point, it is not a priori clear if the set of interior facets is non-empty. However, this will be a consequence of Theorem 1.10, stated later, which implies for any , the length of all the facets will be less than with exponentially small failure probability. Let and denote the extremities of this union path, and let denote the subpath of between and . Define the maximum -interior facet length of , denoted by , to be the maximum length of the -interior facets. Define the -interior maximum local roughness, denoted by by altering Definition 1.2 so that now the supremum is taken over all .
Definition 1.6**.**
Fix . We say is -good if .
Here is our upper bound concerning the maximum length of facets.
Theorem 1.7**.**
Fix , and an interval . Let denote the set of -good . Then there exists such that the probability that is at least for all large enough
Our final principal result concerning exponents asserts that, for , it is highly likely that . Thus we obtain, with high probability, an upper bound for interior maximum local roughness for a dense, though possibly -dependent and random, set of .
Theorem 1.8**.**
In the setting of Theorem 1.7, there exists , such that the event that there exists such that occurs with probability at most for all large enough .
We now state our results about law of large numbers for and the constrained geodesic. Although the route taken here of setting up an appropriate variational problem is by now classical [12], we point out that it was not at all obvious that the solution can be explicitly described. Moreover some of the consequences of the results in the following section are used as geometric inputs for the fluctuation results stated before.
1.3. Law of Large Numbers
For the unconstrained model, a straightforward subadditivity argument yields that converges to a limit. The evaluation of the limiting constant is classical: [29, 25] showed that the limit equals by using Young tableaux combinatorics and the RSK correspondence (see also [1]). However, for the constrained model, the subadditive structure is lost and it is not clear a priori that a law of large numbers for exists. Our first result here is to establish the law of large numbers for the area trapping polymer model; we are also able to evaluate the limiting constant implicitly as a function of .
Given , let be given implicitly by the following equation:
[TABLE]
One can see that the function is strictly increasing 222 and . in , and converges to and at [math] and respectively. Let .
Theorem 1.9**.**
For any
[TABLE]
as .
Notice that as ; hence the above theorem is consistent with the result in the classical unconstrained case. In the unconstrained model, one also has a law of large numbers for the geodesic, i.e., it is known that the geodesic is concentrated around the straight line joining and . More precisely, under the rescaling that takes the square to a unit square, the geodesic converges almost surely in Hausdorff distance to the diagonal of the unit square [12] (as mentioned before, the precise order of the transversal fluctuations are known to be as a consequence of integrability). Even though we do not have any exactly solvable structure in the constrained model, we can establish a similar law of large numbers here too asserting that the constrained geodesic concentrates around a deterministic curve. Moreover, we can identify the limiting curve in a fairly explicit manner.
Let be defined as where is as above. Also let be the blow up of i.e. . We denote by the Hausdorff distance. The following theorem is our law of large numbers for the constrained geodesic.
Theorem 1.10**.**
For any and , there exists such that, for all large enough , it is with probability at least that
[TABLE]
In particular, this theorem states that to first order, the constrained geodesics behave like a given smooth curve. This result will be useful to us while studying the scaling exponents for local roughness of the constrained geodesic, in particular, when we see to rule out long and flat facets (see Theorem 2.2).
1.4. Open questions and future directions
Below we list below several interesting questions for future research:
- (1)
The upper bound Theorem 1.7 is weaker than the lower bound Theorem 1.3. Strengthening the former is a natural open problem. 2. (2)
By definition, . The typical order of remains unknown. 3. (3)
For , what is the typical deviation of from the curve ? What is the order of fluctuations of ? 4. (4)
In a phase separation problem, [20, 21, 19] determines the polylogarithmic corrections to both elements of the (facet length,local roughness) exponent pair. The powers of the logarithm are . Finding such corrections for the Area Trapping Polymer model would refine the identification of the exponent pair made in this article and suggested by the first point. The first two points will be discussed further in Section 6.2.
Supercritical Percolation: We end this section with a conjecture regarding fluctuation exponents in the context of supercritical percolation on the nearest neighbor graph on . As already mentioned before, [9] settles a conjecture of Benjamini regarding the limit shape of isoperimetrically extremal sets. Formally, for supercritical percolation, with the origin conditioned to be in the infinite cluster , the authors in [9] consider the ‘anchored isoperimetric profile’, i.e. for any they look at the set which solves the following isoperimetric problem:
[TABLE]
where denotes the edge boundary of restricted to (for more details see [9]). The main result in [9] shows the convergence of the set as after suitable renormalization, to a deterministic Wulff crystal, in the Hausdorff sense. To go beyond first order behaviour one has to understand local geometric properties of the boundary of . The extremal circuit broadly has to satisfy the:
- (1)
Volume condition 2. (2)
Extremal isoperimetry condition
The heuristic now is that the former is a global constraint while the latter is only local. Namely, each local part of the boundary does not feel the volume constraint and thereby just tries to move through the ‘open’ edges while trying to minimize the number of open edges that it cuts across, since these are precisely the edges that contribute to . This brings us within the realm of first passage percolation predicted to be in the KPZ universality class as well(see [3] for more on first passage percolation). Thus Theorems, 1.3, 1.4, 1.7 and 1.8 can be thought of as rigorous counterparts to the above discussion in the integrable last passage percolation setting and combined with the above discussion allows us to leads us to conjecture fluctuation exponents for the above model. Below we formulate a precise statement in a slightly simpler setting:
Recall the standard definition of the dual graph of the nearest neighbor lattice on . Given a supercritical bond percolation environment on the edge set of with density , for every positive integer consider the set of dual circuits (simple loop consisting of dual edges) enclosing a connected subset of of size and containing the origin such that the number of primal open edges in the percolation environment that the circuit cuts through is minimized. Note that such a circuit is not necessarily unique due to the discrete nature of the problem. Thus the above model is an exact analogue of the model considered in this paper, in the context of first passage percolation in a bond percolation environment. We now state precisely our conjecture:
Conjecture: Consider bond percolation on the nearest neighbor lattice on with any supercritical parameter value . The random variables
[TABLE]
converge to zero in probability as grows to infinity where for any , the maximum facet length and maximum local roughness are defined in the same way as in this paper by considering the convex hull of the points in .
We end with the remark that the problem considered in [9] corresponds to a similar first passage percolation problem where the environment has bounded dependence range and hence should have the same fluctuation behaviour as the simpler model just described.
1.5. Organization of the rest of the article
In Section 2 we collect some preliminary probabilistic results: some for the constrained model and a few from the unconstrained model. The results for the unconstrained model follow from the sharp moderate deviation estimates in [26, 27] and the consequences established in [8]. In Section 3, we set up and solve the variational problem for the law of large numbers and the following Section 4 is devoted to the proofs of Theorem 1.9 and Theorem 1.10: the law of large numbers for the length of constrained geodesic and the path itself. We next turn to the proofs of the results on the scaling exponents. In Section 5 we provide proofs of Theorems 1.3 and Theorem 1.4. The proofs of Theorem 1.7 and Theorem 1.8 are completed in Section 6. Proofs of some of the auxiliary results stated and used throughout the article are postponed to Section 7.
Acknowledgments
The authors thank Marek Biskup, Craig Evans and Ofer Zeitouni for useful discussions. S.G.’s research is supported by a Miller Research Fellowship at UC Berkeley. A.H. is supported by NSF grant DMS-1512908.
2. Important probability estimates
In this section we gather the probabilistic inputs needed for our proof. First we shall record a few useful facts about the length and geometry of the constrained geodesics that will be used repeatedly later. The bulk of this section will then recall results about the unconstrained model. These results are all consequences of the exactly solvable nature of the Poissonian LPP model and can be derived starting with the basic integrable ingredients of the exactly solvable model obtained by Lowe, Merkl and Rolles [26, 27]. Some of these consequences were established and used recently in [8] and we quote the relevant results here.
We start with some basic facts about the constrained model.
2.1. Some Basic Results for the Area Trapping Polymer Model
We first start with concentration for . In absence of integrability we use the standard Poincáre inequality techniques and obtain a concentration at scale.
Theorem 2.1**.**
Fix any . Then there exists a constant such that for all
[TABLE]
The proof is standard and is postponed until the end of the paper in Section 7.
Our next result rules out flat facets. This is a consequence of Theorem 1.10, which asserts that it is extremely unlikely that any interior facets (which are those in the bulk) have very shallow or steep gradient.
Theorem 2.2**.**
For any small enough there exists such that, with probability , all interior facets make an angle with the axis which lies in the interval .
Proof.
We start by recalling a simple fact: for two facets of with starting points and ending points respectively where by convexity of , the angle made with the axis by the facet is larger than the angle made by .
Consider any interior facet and let . Also let be the straight lines joining the origin to and to respectively. Let and be the points of intersection of and with . Theorem 1.10 implies that, for any , with probability at least the bound
[TABLE]
holds for all -interior facets, simultaneously. Now, by the convexity of , the gradient of the facet is between the gradient of the lines joining to and to . Choosing to be much smaller than we see that the gradient of the facet plus an error of lies between the gradients of the lines joining the origin and and and respectively. Thus we are done by choosing to be small enough and using the strict convexity of ; (see Figure 2(a) for illustration). ∎
We will later need Theorem 4.6, a strengthening of the above result, which is uniform in . We next state useful results that concern the unconstrained, exactly solvable, model. All of these are corollaries of the following moderate deviation estimates.
2.2. Moderate deviation estimates
Recall the polymer length from Definition 1.1. Let be such that ; i.e., is the area of the rectangle whose opposite corners are and . Notice that, by scale invariance of the Poisson point process, the distribution of is a function merely of .
Theorem 2.3** ([26, 27]).**
Fix . Let , as above be points such that the straight line joining and has gradient , where . There exist positive constants , , and depending only on such that, for all and ,
[TABLE]
Observe that the above theorem implies that ; and hence similar tail bounds are true for the quantity . When we make use of Theorem 2.3, it will often be in order to obtain tail bounds for the quantities . Also the results of [4] establish that converges weakly to the GUE Tracy-Widom distribution (which is defined for example in [4]). This law has negative mean, leading to the next bound.
[TABLE]
for some .
2.3. Transversal fluctuations of point-to-point geodesics
Let . Let denote the equation of the line segment joining and . For any path from to , define the maximum transversal fluctuation of the path by
[TABLE]
For points and , we call the -coordinate distance between and and similarly define the -coordinate distance.
Transversal fluctuations for paths between and were shown to be with high probability in [24]. The following more precise estimate was established in [8].
Theorem 2.4** (Tails for Transversal Fluctuations, [8]).**
Fix . Let be points such that the -coordinate distance between and is and the gradient of the line joining and is , where . Then, for the geodesic from to ,
[TABLE]
for -dependent constants , and sufficiently large.
The proof of Theorem 2.4 from [8] in fact shows something more. Any path that has transversal fluctuations much bigger than is not only unlikely to be a geodesic; it is typically much shorter than a geodesic. In particular, the proof of Theorem 11.1 in [8] implies the next result (which can also be derived more straightforwardly).
Theorem 2.5** (Paths with off-scale are uncompetitive).**
Fix and . Let be points such that the -coordinate distance between and is and the gradient of the straight line joining and is where . Let denote the event that there exists a path from to with and (we suppress the dependence of in for brevity). Then there exists such that
[TABLE]
for sufficiently large.
The stretched exponential nature of these estimates allow us to prove uniform properties of the noise space which will be convenient for some of the arguments later. This point is a theme in this article: points to which we seek apply the above results may be special, so that estimates that are uniform over all points will be needed. For the next result, recall that our noise space is nothing other than a rate one Poisson point process in the box . For , let denote the line joining and . Now, for any , the pair is called -steep if the gradient of lies in the interval . Lastly, for ,
[TABLE]
Corollary 2.6**.**
Fix , , and sufficiently small. Then there exists such that
[TABLE]
Proof.
This follows by using Theorem 2.3 and a standard coarse graining argument. Since we are not attempting to prove optimal bounds, we simply partition the box into squares of area one. Thus the corner points are the lattice points, i.e., elements of the set . The proof now follows by first proving the desired statement for lattice points . This just follows by Theorem 2.3 and a union bound over all pairs of lattice points (of which there are ). The proof is then completed by showing that, since any box of area one is unlikely (with stretched exponentially small failure probability) to contain more than points, for any and , one can approximate by , where are the nearest lattice points. ∎
We now specify a modification of the event from Theorem 2.5. Let denote the event where the permitted error term is instead taken to be the quantity defined a few moments ago. The next corollary is proved along the same lines as Theorem 2.5, in combination with the arguments in the proof of Corollary 2.6, and we omit the proof.
Corollary 2.7**.**
Fix , , and small enough. Then there exists such that
[TABLE]
2.4. Paths between points in an on scale parallelogram
Next we control the deviation of lengths between pairs of points within certain parallelograms. We first need some definitions. Let denote a parallelogram with the properties that:
- (a)
One pair of parallel sides are vertical. 2. (b)
The other pair of parallel sides have gradient . 3. (c)
The (horizontal) distance between the vertical sides is . 4. (d)
The height of the vertical sides is .
Note that this defines a unique parallelogram up to translation. This will be enough for our purposes because the underlying noise field is translation invariant.
Theorem 2.8** ([8]).**
Let and for some . Then there exist -dependent constants , such that, for all sufficiently large and ,
[TABLE]
and
[TABLE]
where and respectively denote the right third and the left third of .
The next theorem states that, even if the paths are restricted to stay inside the parallelogram, the fluctuation remains on scale. Let denote the length of the longest path from to that does not exit .
Theorem 2.9** ([8]).**
Under the assumptions of Theorem 2.8, there exist -dependent constants such that, for all sufficiently large and ,
[TABLE]
where and respectively denote the right third and the left third of .
2.5. Paths constrained in a thin parallelogram
The next set of results shows that, if a path is constrained to have much smaller than typical transversal fluctuation, then it must have much smaller length than a typical geodesic’s.
Theorem 2.10** (Paths with small are uncompetitive).**
Fix . Consider the parallelogram , where and . Let and denote the midpoints of the vertical sides and of . Then, for some ,
[TABLE]
for sufficiently large.
The proof of Theorem 2.10 follows a strategy, by now well known, that has been used to show Gaussian fluctuation of paths constrained to stay in a thin rectangle in [11] in the context of first passage percolation. In the context of LPP, the Gaussian fluctuation has recently been shown in [14], and tail bounds are proved in a more general context in the preprint [7]. We now provide a sketch of Theorem 2.10’s proof.
Sketch of Proof.
Without loss of generality let us assume . Also, we can replace the parallelogram by the rectangle one of whose pairs of sides is parallel to the line segment , with the other pair having midpoints and and length . Divide the rectangle into equal parts (each of width ) by parallel line segments perpendicular to . Let denote the left side of the -th rectangle and let be its midpoint. Now let be the best path (i.e. with maximal value of ) between and that stays within . It follows from Theorem 2.8 that it is extremely likely that . It follows that up to an error of order much smaller than we can approximate by . Now observe that are independent and identically distributed with mean (here we use (3)) and standard deviation of the order of . By standard concentration inequalities, one then shows that concentrates around at scale . By choosing properly one gets the result. ∎
In the same vein, we have the following corollary.
Corollary 2.11**.**
Fix , , and small enough. Then there exists such that, with probability at least ,
[TABLE]
2.6. Estimates for One-Sided Geodesics
We end this section by considering geodesics in a different constrained model. Baik and Rains [5, 6] considered increasing paths from to that lie above the diagonal line joining the points. Recall that denotes the length of the longest increasing path between points . Let denote the length of the longest path between and restricted to lie above the line joining and and, similarly to Definition 1.1, let denote the corresponding uppermost one-sided geodesic between and . Moreover, let denote in the special case that and . Baik and Rains [5, 6] proved that and that the fluctuations are again of order (although in this case the scaling limit is different; it is the GSE Tracy Widom distribution instead of the GUE Tracy Widom distribution). We shall need the corresponding moderate deviation estimates, consequences of Theorem 2.9.
Theorem 2.12**.**
Let be as in the hypothesis of Theorem 2.3. There exist positive constants and such that, for all and ,
[TABLE]
Proof.
The upper tail result follows from Theorem 2.3 due to . For the lower tail, we use Theorem 2.9 with the straight line joining and being the bottom side of the parallelogram and use the fact that . ∎
We need a uniform version of this result. Recall from (4).
Corollary 2.13**.**
Fix , , and small enough. Then there exists such that, with probability at least ,
[TABLE]
Proofs of Corollaries 2.7 2.11, 2.13 follow from the corresponding theorems for fixed points, in the same way as Corollary 2.6 follows from Theorem 2.3. We omit the details.
3. A Variational Approach to the Constrained Geodesic
We now move towards proving Theorem 1.9 and Theorem 1.10. Deuschel and Zeitouni [13, 12] studied in detail the hydrodynamic limit of the unconstrained geodesic for inhomogeneous point processes. We follow their strategy broadly and study the limit of the constrained curve by means of appropriate variational problems. We first explain the idea. Fix for the rest of this section. First let us assume that a limiting continuous curve of the constrained geodesics exists after scaling. This curve will be continuous, non-decreasing and surjective. By the area constraint, . Now heuristically, since in practice there is always a little bit of area excess, one can approximate by a piecewise affine function at a scale local enough that each piece is exempt from the area constraint; and we can then use the law of large numbers for the unconstrained geodesic (see Theorem 2.3) at every local scale and sum over them. This argument suggests that the approximating path will have length where
[TABLE]
It thus seems that we should maximize among all curves satisfying the area constraint, and the maximum will be the constant appearing in the required law of large numbers. We now proceed to make this precise. Let be the collection of all right-continuous non-decreasing functions from to . Thus is in bijection with the set of all sub-probability measures on . Now, for any by the Lebesgue decomposition theorem we can write
[TABLE]
in a unique way as a sum of a pair of sub-probability measures, with being the absolutely continuous part and the singular part (with respect to Lebesgue measure). Note that this implies has a derivative almost everywhere 333Throughout the article, for any function on which is differentiable almost everywhere, we will denote its derivative by . Recall, that this does not necessarily imply for all . such that, for any , we have
[TABLE]
while is almost surely flat and hence has derivative [math] almost surely. Thus almost surely. Also define
[TABLE]
Let
[TABLE]
We shall often omit the subscript . Finally let
[TABLE]
The first step is to show existence and uniqueness of the solution.
Proposition 3.1**.**
There exists a unique element that attains the supremum in (8).
Note that the function in Proposition 3.1 will be the same in the statement of Theorem 1.10. The existence and uniqueness parts of Proposition 3.1 have separate proofs. We first state the existence result.
Lemma 3.2**.**
There exists that achieves the supremum in (8).
The proof of Lemma 3.2 is technical: it uses a compactness argument on the space of probability measures following a similar argument from [12]. We postpone the proof until Section 7.
In the next part we show uniqueness.
Lemma 3.3**.**
Suppose and are in and satisfy for . Then .
The proof of Lemma 3.3 is rather straightforward once we establish the following technical lemma that rules out the possibility that any of the optimizing functions have a nontrivial singular part.
Lemma 3.4**.**
Let be such that . Then corresponds to a probability measure which is absolutely continuous with respect to Lebesgue measure.
Here is the basic idea of the proof of this lemma. From the results of [12] it follows that without the area constraint the optimizing curve is the diagonal line, i.e., the preferred gradient for the graph of the function is one. If the singular part is non-trivial, then the graph of the function may be expected to have a flat piece. Because the gradient of the graph has to be one on average due to boundary conditions, it follows that there must be a piece of the graph having gradient away from one. We shall show that one can modify the flat and the steep parts of the curve locally by pieces with more moderate gradient in a way that increases not only the value of the functional ; and thereby optimality will be contradicted. Also, clearly in the case that does not have total mass one, one can add to it another function to make it (or, more precisely of course, to bring it into correspondence with) a probability measure, while also increasing the value of and thus contradict maximality in this case also. Thus is also a probability measure. The details of the proof are postponed to Section 7.
We can now prove the uniqueness result using Lemma 3.4.
Proof of Lemma 3.3.
We use the fact that the square-root function is strictly concave. Given any and as in the statement of the lemma, we consider . Clearly, satisfies the area constraint and . Thus using Jensen’s inequality is necessarily larger than unless almost surely. Since by the previous result the absolutely continuous parts contain mass one, . Hence for all
[TABLE]
Thus we are done. ∎
It still remains to identify the optimizer in (8); in particular we need to show this is the same as defined in Theorem 1.10. To this end, we shall now record some properties of the unique optimizer that will be useful later. We show that the derivative is almost surely positive and decreasing. The proofs are easy and will be postponed until Section 7.
Lemma 3.5**.**
Let denote the unique optimizer in Proposition 3.1. Then
- (i)
The derivative is almost surely decreasing i.e. there is a set of full measure on which it is decreasing. 2. (ii)
* is almost surely positive.*
3.1. Identifying the curve
In this subsection we determine the curve and show that it is the same as the curve in Theorem 1.10. We first start with the following proposition.
Proposition 3.6**.**
Given there exists such that .
Proof.
The proof proceeds by showing that, given any ,
[TABLE]
for some constants and . Fix and let be a polynomial such that
[TABLE]
Define on by defining it to be [math] outside . Let . Now since is monotonically decreasing and positive almost surely (see Lemma 3.5), is bounded above and below by constants on and hence for all (with sufficiently small absolute value depending on , we will need to take both positive and negative values in the argument later), we conclude is strictly positive. Moreover by (9), . We now verify the area constraint. It is easy to see by Fubini’s theorem (see (29) in the proof of Lemma 3.5) that . Thus
[TABLE]
by (9) and (10). Now, by Taylor expansion, for all small enough (depending on , , and ),
[TABLE]
where the constants in the - notation just depend on (since is in almost surely for some on by the preceding discussion). Since (and can be both positive and negative it follows that,
[TABLE]
Since is bounded above and below on , one can find a linear function such that
[TABLE]
Indeed, such can be found by solving the two linear equations in and given by the above two equations. To see that, for any , the equations are non-degenerate, first observe that one can by a change of variable assume that and . Then the matrix corresponding to the linear equations is nothing but \left[\begin{array}[]{cc}1/2&1\\ 1/3&1/2\end{array}\right] and hence admits a unique solution. Together with (12) this now implies that
[TABLE]
for all polynomials . For this, observe that by Gram-Schmidt orthogonalization any polynomial can be decomposed as where is a linear function and is a polynomial satisfying (9) and (10). Since polynomials are dense in by the Stone-Weierstrass theorem, this implies
[TABLE]
Since is a linear function on all intervals , it follows that it has to be the same linear function on all such intervals and hence for some linear function almost everywhere on the entire interval . Thus for some constants . Integrating and using that and (see Lemma 3.4) we are done. ∎
The next proposition completes the identification of by showing that the constant is given by (2).
Proposition 3.7**.**
The constant is given implicitly by the following equation:
[TABLE]
where is the constant in Theorem 3.6 corresponding to .
Proof.
Clearly we have
[TABLE]
for some . We shall show that which will establish the proposition. Suppose not. As we have pointed out, the left-hand side of this equation is increasing in . Let be the unique solution to the equation
[TABLE]
It is easy to check that implies . Define by . Clearly . A straightforward computation shows that
[TABLE]
The right-hand side here is readily seen to be decreasing in and hence . This contradicts the optimality of , and completes the proof. ∎
Observe that, . This expression is the same as the constant in Theorem 1.9 which is consistent with our heuristic explanation at the beginning of this section. We prove this theorem next.
4. Law of large numbers
With the preparation from the previous section we now turn to the proof of Theorem 1.9. Fix as before. The idea of the proof is as follows. We first show that if a path follows approximately the blow up of the deterministic curve (and also satisfies the area constraint) then it is overwhelmingly likely that the path has length at least for arbitrarily small. We further show that any path satisfying the area constraint is extremely likely to have length less than . We begin with the following trivial but useful lemma that is an immediate consequence of continuity and monotonicity of .
Lemma 4.1**.**
Given any for all small enough there exist such that if and if .
Next we need a couple of preparatory lemmas about appropriate discretisations. Let be the discretisation of the unit interval; (we will take to be the reciprocal of a positive integer to avoid rounding errors). Consider any non-decreasing function that corresponds to an absolutely continuous measure on : by identifying with its graph, we shall interpret as an increasing path on the unit square directed from to . Also let be the piecewise affine function that agrees on with .
Lemma 4.2**.**
We have .
Proof.
First notice that by integration by parts or by Fubini’s theorem, for any absolutely continuous function on . The lemma now follows from the observation that . Let be the midpoint of the interval . Notice that by definition is constant on and is equal to . Thus
[TABLE]
The proof now follows by observing .
∎
We now discretise the vertical direction as well. Let us choose (to be specified exactly later), and let . Given as before let us now set, to be the piecewise linear curve determined by the points . Clearly for all and hence for
[TABLE]
Before proceeding further we make a few comments about notation. Recall that till now, our underlying noise space has been a point process on and we have been concerned about geodesics in . However in the last section while solving variational problems we switched to a normalized picture where every path lives in . We will continue with this convention throughout this section. Equivalently the noise space can be thought of as a Poisson point process of intensity in . In an abuse of notation, we will define for two points to be the length of the geodesic between and in the same noise space. In light of properties of Poisson process under scaling, Moreover, all the estimates regarding stated in the previous sections continue to hold after the appropriate variable change. We omit further elaboration. Next, we state a uniform version of Theorem 2.3 in the large deviation regime.
Lemma 4.3**.**
Fix as above. There exists such that, simultaneously for all and for all large :
- (1)
With probability at least
[TABLE] 2. (2)
With probability at least
[TABLE]
Proof.
The proof follows from the large deviation probabilities for the length of unconstrained geodesics in [28]. In particular the theorem states that for any as in the statement of the theorem,
[TABLE]
for some constant . A union bound over points , the total number of which is , completes the proof. ∎
We are now ready to prove Theorem 1.9. We start by showing the upper bound. Recall that denotes the length of the constrained geodesic.
Proposition 4.4**.**
Fix . There exists such that with probability at least we have
[TABLE]
Proof.
Recall that for any increasing path we denote its length or the number of points of the Poisson process it passes through by . Let us now notice that
[TABLE]
Thus by the previous lemma, with probability at least we have for all increasing paths, (from to in the rescaled space)
[TABLE]
An argument involving truncating at shows that, with probability at least , for all increasing paths
[TABLE]
Thus, for , with probability at least for all
[TABLE]
Now let be an increasing path that traps area at least (which corresponds to area in the unscaled model). By (14), it follows that and hence, by continuity of , we have by choosing sufficiently small. By choosing suitably small, this implies that, with probability at least , the bound for such increasing paths . This completes the proof of the proposition. ∎
We now show the corresponding lower bound.
Proposition 4.5**.**
Fix . There exists such that, with probability at least , we have
[TABLE]
Proof.
The derivation of this lower bound is straightforward: we will take a discretisation of and then use the continuity of . Fix . Choose and consider . Then, by definition, Choose small enough that
By using the continuity of and , we see that, for given , there exist sufficiently small choices of such that the piecewise affine function interpolating between the points satisfies
[TABLE]
Now let be the geodesic between the points and . Let be the path obtained by concatenating the paths for Using Lemma 4.3, it follows that, with probability at least ,
[TABLE]
where we take and sufficiently small. Now by Lemma 4.2, we find that
[TABLE]
since and agree on . Hence, for small enough, . Thus, is at least as large as . Hence, we are done. ∎
Proof of Theorem 1.9.
Combining Proposition 4.4 and Proposition 4.5, we complete the proof of Theorem 1.9 by noting that an upper tail bound of the form for all is easily obtained by bounding the upper tail of the Poisson-distributed total number of points. ∎
4.1. Law of large numbers for the geodesic
We now prove Theorem 1.10. The proof is by contradiction: if , and the noise space is such that the events listed in Lemma 4.3 occur, then we would be able to construct an absolutely continuous function that traps area at least and for which . This would contradict extremality of . To show the above inequality, we will employ a concavity argument. For notational brevity, let and . For , recall the definition of from the previous section. We will consider the function . Fixing parameters and we will restrict attention to the event , on which:
- (1)
2. (2)
.
By Propositions 4.4 and 4.5, and (15), occurs with probability at least . Observe that Proposition 3.6 implies that is bounded away from zero and infinity on . Thus, lies in where . Suppose that . We now claim that if are small enough compared to , then there exists such that
[TABLE]
To see this, we choose such that . Let be such that . Now we consider two cases:
- (1)
If , then
[TABLE]
These implications, excepting the last, follow by definition. The last implication is due to having Lipschitz constant at most . 2. (2)
If , then, similarly,
[TABLE]
Thus, by (16),
[TABLE]
Also, note that, since both and start at and end at , . Hence,
[TABLE]
where denotes . Moreover, on ,
[TABLE]
for some . Observing that , we see that the concavity of implies that is non-negative. Furthermore, simple algebra shows that, for all ,
[TABLE]
The proof is now completed by observing that a length gain has been realized:
[TABLE]
On the event we see, by means of this inequality and the definition of , that if holds, then
[TABLE]
for some constant that depends only on . Also, both and are at least by definition, and hence by (14), we have
[TABLE]
where can be made arbitrarily small by choosing and hence small enough. This inference contradicts the continuity of in . Hence we are done. ∎
We now use similar arguments as those employed to prove the law of large numbers in order to establish a variant of Theorem 2.2 that is also uniform in . This particular variant will be crucial in the proof of Theorem 1.7.
Theorem 4.6**.**
Fix . For any small enough , there exist and such that, with probability at least , all -interior facets of for which make an angle with the -axis that lies .
Proof.
Recall that the proof of Theorem 2.2 used Theorem 1.10 and the strict convexity of the function . Since is uniformly convex for all , this proof will be complete, using the same arguments as in the proof of Theorem 2.2, once we prove the following uniform version of Theorem 1.10: for any , with probability at least ,
[TABLE]
where depends on and the interval . We fix an to be specified later and discretise the interval to obtain the set . Fixing parameters and , again as before we restrict attention to the event on which, for all ,
- (1)
; 2. (2)
and .
Similarly to a previous argument, by Propositions 4.4 and 4.5 and (15), followed by a union bound, . Now if and are chosen to be sufficiently small depending on by the previous result, Theorem 1.10, and a simple union bound, we obtain
[TABLE]
The proof will proceed along the same lines as the proof of Theorem 1.10 did. With the aim of arriving at a contradiction, let be such that
[TABLE]
Clearly, holds by definition. Since is a continuous function of in the supremum norm, we see that, for small enough ,
[TABLE]
Now, as we argued in the proof of Theorem 1.10, this implies that
[TABLE]
Note then that
[TABLE]
where where can be made small enough by choosing small enough. The first inequality follows by definition, and the second by the occurrence of .
Thus, using (15), we find that
[TABLE]
This along with (21) allows us to apply the concavity argument that appears in the proof of Theorem 1.10: by choosing much smaller than , we thus contradict the continuity of at . ∎
5. Lower Bound for Scaling Exponents
In this section we provide proofs of the lower bounds on and , i.e., we prove Theorem 1.3 and Theorem 1.4. Most of the work goes into proving the lower bound Theorem 1.3, since the lower bound for local roughness is a reasonably easy corollary of Theorem 2.4. Let and be fixed for the rest of the section. Let denote the event that . We shall show that the event is extremely unlikely. We start with an overview of the proof. We shall need a geometric definition.
Definition 5.1**.**
Let be given constants. A sequence of points is called a -regular sequence if the following conditions hold.
- (i)
The union of line segments joining to for is convex. 2. (ii)
The gradient of the all the line segments joining to is . 3. (iii)
The distance between the first and last point in the sequence i.e., . 4. (iv)
The distance between the consecutive points in the sequence is small: . 5. (v)
Let and be the angles that the line segments and make with the positive -axis (clearly by hypothesis). Then .
See Figure 3 for an illustration of this definition.
Before proceeding let us try to motivate the item (v) of the above definition. Consider the least concave majorant of an increasing path from to as described in Definition 1.2 The total change of angle made by the line segments constituting the concave majorant with the -axis is roughly around over a length of around . So over a distance of around , the change of angle should be around on average. The item (v) of the above definition asserts that on a regular sequence the change of angle is not much more than this average.
The following basic geometric consequence will be useful.
Lemma 5.2**.**
Let be a -regular sequence for some . Let denote the union of line segments joining the consecutive points of . Let denote the parallelogram with two vertical sides of length whose bottom side is the line segment joining and ; see Figure 3(a). Then there exists a point in such that the triangle formed by the points is an isosceles triangle (with the sides adjacent to being of equal length) contained in such that the two sides of adjacent to lie above the piecewise affine curve obtained by joining the consecutive points of .
Proof.
Consider the angles and made by the line segments and respectively with the line segment . Also, let be the point of intersection obtained by extending the line segments and . By convexity, the piecewise affine curve obtained by joining the points of lies inside the triangle . Moreover, it follows from elementary geometric arguments that . Now let us consider the isosceles triangle where forms the base and is the value of the two equal angles. Since is at least as big as and , it follows that the triangle is contained inside the triangle . Moreover, the latter is clearly contained in a parallelogram of height where the constant in the notation depends on . Since for all large enough , , we are done. ∎
Let us now record the main steps of the proof of Theorem 1.3. Let denote the constrained geodesic. Recall that denotes least concave majorant of and is an union of the facets as described in Definition 1.2.
Step 1: We shall fix a -regular sequence , and consider the best path from to that passes through all the points in the sequence. We shall show that with very high probability the length of this path is much smaller than the length of the best path between and . The reason that this event is likely is the following: because the lengths of the segments are much smaller than that of the segment , it will turn out that the path will have a much smaller transversal fluctuation compared to the typical geodesic between and . Thus, by Theorem 2.10, it is extremely likely that this path has a much smaller length.
Step 2: Next we will show that there exists a path between and that lies above the line segments joining the consecutive points of and whose length is comparable to that of the geodesic between and . This will follow from the definition of regular sequence together with an application of Lemma 5.2 and Theorem 2.12.
Step 3: Finally, we will show that, on the event , it is overwhelmingly likely that there exists a -regular sequence made out of consecutive corners of . Once we establish this, we will arrive at a contradiction: using the first two steps, we will construct a path that traps more area than does and that also has a greater length.
The next proposition treats the first step.
Proposition 5.3**.**
Let be a -regular sequence. For let be the geodesic between and . Let denote the concatenation of the paths . Then there exists such that, with probability at least , we have
[TABLE]
Proof.
Let be the parallelogram with sides parallel to the sides of such that and are the midpoints of the vertical sides of ; and the height of the vertical sides is . For each , let denote the parallelogram with the following properties:
- (1)
has one pair of vertical sides and the other pair of sides is parallel to the line segment joining and . 2. (2)
The vertical sides have midpoints and . 3. (3)
The height of the vertical sides is .
It is straightforward to check from Definition 5.1 that all the rectangles are contained in the rectangle . Now it follows from Theorem 2.5 that, with probability at least , each geodesic is contained in the parallelogram . In particular, on this event,
[TABLE]
The result now follows using Theorem 2.10 and the assumed lower bound on . ∎
Next we move onto Step 2 where we show the existence of a “good” path between and . We have the following proposition.
Proposition 5.4**.**
Let be a -regular sequence. Let denote the union of line segments joining to .Then there exists such that, with probability at least , there exists a path from to lying above such that
[TABLE]
Proof.
We will use the notation from Lemma 5.2. Let be the point in that satisfies the conclusion of that lemma. Let denote a path from to lying above the line segment joining and that achieves the length . Similarly, let denote a path from to lying above the line segment joining and that achieves the length . See Figure 3 (b).
Let denote the concatenation of the paths and . Clearly lies above . We shall show that, with overwhelming probability, also satisfies the other condition in the statement of the proposition. It follows by definition and some elementary geometry that both of the equal sides of the isosceles triangle have gradient in , and also . It follows using Theorem 2.12 that with probability at least one has
[TABLE]
Also observe that is equidistant from and and that this point lies within the parallelogram whose height is . Thus, by a standard calculation,
[TABLE]
Combining these inferences, we find that, with probability at least ,
[TABLE]
This completes the proof of the proposition. ∎
In the final step, we establish that, on , that is if is smaller than , it is extremely likely that there exists a regular sequence whose points are consecutive corners of (the least concave majorant of ). Let denote the event that there exist consecutive corners of such that is a -regular sequence.
Proposition 5.5**.**
There exist such that, except for a sub-event of exponentially small probability, the event is contained in the event i.e.
[TABLE]
for some universal constant .
On , we shall find a regular sequence among interior facets. Before proceeding we state an easy geometric lemma that will be used. The proof is provided in Section 7.
For any two points , denote by the acute angle between the lines joining the points and to the point , i.e., the bottom right corner of the square (see Figure 5).
Lemma 5.6**.**
There exists such that with probability at least simultaneously for all on with , then .
Proof of Proposition 5.5.
Observe that by definition, on , any sequence of consecutive corners of satisfies condition (i) and (iv) of Definition 5.1. Fix . By Theorem 4.6, with failure probability at most all the interior facets have gradient in the interval for some . For the remainder of the proof, we shall assume that this event occurs. Now we partition all the -interior vertices of (it is easy to see they are non-empty on ) into consecutive segments
[TABLE]
(where ’s are the consecutive corners on ) such that
[TABLE]
for all where .
We denote the segment by Thus if are all such segments, then . It follows from convexity and the boundedness of the gradients (see Lemma 5.6 and Figure 5) that . Let denote the angle made by the line segment with the positive -axis. For the sequence , let . Notice that, by convexity, is nonnegative for all . Also observe that
[TABLE]
This together with Markov’s inequality and the fact that the number of ’s is implies that, for some constant , there exists at least one such that . Setting to be equal to such a sequence, we see that satisfies all conditions in the Definition 5.1 for some . This completes the proof of the proposition. ∎
With all this preparation, finally we are ready to prove Theorem 1.3.
Proof of Theorem 1.3.
Let and be fixed as before. Let be such that the conclusion of Proposition 5.5 holds. Let denote the event that there exists a -regular sequence for which at least one of the conclusions in Proposition 5.3 and Proposition 5.4 does not hold. Using the proofs of the said propositions, along with taking an union bound over all pairs of grid points obtained by coarse graining (exactly as Corollary 2.6 followed from Theorem 2.3), that for some . By Proposition 5.5, it suffices to show that
[TABLE]
By way of contradiction, let us assume that the set is non-empty. Fix a configuration in the set , and consider the least concave majorant of the constrained geodesic. On , there exists a -regular sequence consisting of consecutive corners of . On , there exists a path from to satisfying the conclusion of Proposition 5.4. Let denote the restriction of between and . Clearly,
[TABLE]
It follows from Propositions 5.3 and 5.4 that, on , . Also observe that lies below the line segments joining to whereas lies above these segments. Hence the increasing path from to that coincides with between and and between and and coincides with between and traps at least as much area as does . However, by the above discussion, . This contradicts the extremality of and completes the proof of the theorem. ∎
5.1. Proof of lower bound of
In this subsection we prove Theorem 1.4. That is, we show that the maximum local roughness of the facets has scaling exponent at least . The basic idea of the proof is to use KPZ scaling to argue that, if there is a facet of length roughly , then along that facet, the local roughness is likely to be at least . We now make this more precise.
Fix . We have just proved that, with high probability, there exists a facet of length at least . In fact, by the proof of Theorem 1.3, more is true. Fix a large constant. Let denote the event that (see Definition 1.2) has a facet of length at least with endpoints and such that the straight line joining and has gradient . The following lemma is a consequence of the proof of Theorem 1.3.
Lemma 5.7**.**
For all large enough (depending on ), for all sufficiently large, where is a constant depending only on and .
Proof.
Note that the proof of Theorem 1.3 in fact showed that there must be a -interior facet of length at least with sufficiently large probability. Since all the -interior facets satisfy the gradient requirement (see Theorem 4.6), we are done. ∎
Proof of Theorem 1.4.
Let denote the event that . Thus, to prove Theorem 1.4, it suffices to show that
[TABLE]
Let denote the constrained geodesic. On , let and be corners of satisfying the conditions in the definition of . Consider the restriction of between and . As ; it follows that there exists such that the restriction of (call it ) between and is contained in the parallelogram that has a pair of vertical sides of height and whose top side is the line segment joining and . Now observe that the height of the parallelogram is much smaller than the on scale transversal fluctuation of geodesics between and , these fluctuations being at least
[TABLE]
Thus, Corollary 2.7 implies that the bound
[TABLE]
fails with probability at most . By Corollary 2.13,
[TABLE]
except, again, on a set of probability at most . Consider now the path that agrees with outside the segment and that between and equals , which recall is a path from to lying above the line segment that joins these two points and achieves length . We see then that has greater length, and traps as much area as, . This contradicts the assumption of length maximality for ; (similarly to the proof of Theorem 1.3. See Figure 4(b).) ∎
6. Upper Bound for Scaling Exponents
This section is devoted to the proof of Theorem 1.7. That is, it will be shown here that, for a dense set of that may depend on , the maximum facet length of the constrained geodesic is very likely to be at most . Theorem 1.8 will then follow by the KPZ scaling enjoyed by transversal fluctuations.
We explain the main ideas before giving proofs. Recall Definition 1.6. The basic idea is to show, using Corollary 2.13, that if a certain value of is not ‘good’ (recall Definition 1.6), we may perform a “landgrab” operation. More formally let us assume that there is a facet which has length and has a reasonable gradient bounded away from zero and infinity. Theorem 2.12 allows us to find a path from to which lies above the facet at a characteristic height of and has characteristic fluctuations (we have room to allow some error) i.e. by Corollary 2.13 we can assume
[TABLE]
Similarly by an Corollary 2.6 we can assume that
[TABLE]
where is the restriction of the constrained geodesic between and . Thus the path which is obtained from by replacing by traps at least more area than does and loses at most in length. Repeating this operation about times (we can do that provided there are no good in this interval), one gains an area that is while losing at most in length with very high probability. This contradicts the fact that for (an easy consequence of Theorem 1.9 using is strictly decreasing) using Theorem 2.1. Next we provide the details needed to make the above argument precise.
Fix and also and . Let denote the event that no is -good. Let be the set of all pairs satisfying the following conditions.
- (1)
. 2. (2)
The straight line joining and has gradient . 3. (3)
.
For , let denote the event that and where denotes the best path between and that is constrained to stay below the straight line joining and . Let denote the event that holds for all . Further let denote the event in the statement of Theorem 4.6, i.e., all the interior facets of has moderate gradients for all . We have the following proposition.
Proposition 6.1**.**
There exists sufficiently small such that, on , there exists for which
[TABLE]
Proof.
We perform the following recursive construction. Let . For construct recursively as follows: find the longest -interior facet in . On , the longest -interior facet has length at least . Note that on , the endpoints and of this facet satisfy for some . Now pick a point at orthogonal distance from the midpoint of the line segment joining and ; (see Figure 6). Thus the area of the triangle is at least for some constant that does not depend on . Set . Now consider the path that coincides with outside the facet , and is formed by concatenating and between and . Clearly the area under the curve is at least . Also, on ,
[TABLE]
It follows that
[TABLE]
Denote , where is the smallest index for which . It follows that
[TABLE]
Since for all , it follows that the final term is at most and that completes the proof of the proposition. ∎
We may now complete the proof of Theorem 1.7.
Proof of Theorem 1.7.
Let be large enough that the conclusion of Proposition 6.1 holds. Using Theorem 4.6 and Corollary 2.11, it follows that, for this choice of (and for given and ), one has that, for some constant ,
[TABLE]
Hence, using Proposition 6.1, it suffices to show that
[TABLE]
for some . Notice that in the above step we have used the trivial inequality for all . It follows now from Theorem 1.9 that for sufficiently large. The claimed bound (23) now follows from Theorem 2.1 and the fact that . This completes the proof. ∎
6.1. Proof of Theorem 1.8
This derivation is similar to that by which Theorem 1.4 follows from Theorem 1.3. By Theorem 4.6, for all and all small enough , there is a probability at least that all the -interior facets of are steep for some value of . Now for any good (note that the set of good s is a function of the underlying point process and hence is random), by definition, all the interior facets of have length at most . Moreover, by the uniform bounds discussed above we may restrict to the case where all the facets are -steep. Suppose that the maximum local roughness restricted to the -interior facets is at least . Let and be the endpoints of the facet that attains this maximum local roughness. Let be the segment of between and . By using Corollary 2.7, we see that, with probability at least ,
[TABLE]
On the other hand, by Corollary 2.13 again, we find that, except on an event of probability at most ,
[TABLE]
Thus, the path that agrees with from to and from to and equals the path between the points and clearly captures at least as much area as does and also contains more points than does . This contradicts the extremality of the latter path. ∎
6.2. Possible extensions and difficulties
We end this section with a few remarks related to the first two open problems mentioned in Section 1.4. A natural approach to quantifying the proof of Theorem 1.7 is via Proposition 6.1. Namely, one can hope to bound below the density of those that are good (where here we ignore the parameter for the purpose of illustration.) This is because using similar arguments to those used in deriving these two results, one can hope to prove the following uniform bound: with high probability the noise space is such that for all we have for where and where the notation hides poly-logarithmic multiplicative factors (which arise due to the exceptional nature of the facet endpoints that contributes a polynomial entropy factor). Thus, the above implies that the length-to-area gradient in scaled coordinates (with length measured in units of and area measured in units of ) is as by definition . Also, we know that, for all which are bad, the gradient is polynomially small (since by the land-grab argument (see Figure 6), the length loss is much smaller than the area gain). This coupled with the fact that should then allow to conclude that the density of good is at least .
Notice that our approach for proving upper bounds relies on the joint coupling of the process for various values of . This is quite different in spirit from the known proofs of similar statements in other contexts such as phase separation [20] where the upper bound was proven for a fixed value of . The key ingredient there was an understanding of the excess area fluctuation (see Open question (2) in Section 1.4) which then allowed a resampling argument to work. However, since we do not have such bounds, we have to work across various values of simultaneously.
A heuristic argument in our setting proving an upper bound of on the excess area trapped by , assuming that is good (recall Definition 1.6) can be made as follows: Suppose that the excess area is more than . Since, by hypothesis the longest facet length is at most , we may find two points and on such that and segment of between and has average curvature (the average distance of the curve from the line segment joining and is what it should be on for a circle; see Figure 2 (b)). Now consider shortcutting between and and hence replacing the subpath of between and by the unconstrained geodesic between and . This operation will create an area loss (approximately ) which is not enough to violate the area constraint, because the excess area before the shortcut was at least . Moreover, the shortcut increases the overall weight and hence contradicts extremality of .
7. Proofs of some of the earlier statements
It remains to provide proofs of Lemmas 3.2,3.4, 3.5, 5.6 and Theorem 2.1 that were postponed.
7.1. Proof of Lemma 3.2
This subsection follows closely the arguments presented in [12, Section 3]. Let be a sequence of elements in such that
[TABLE]
We equip the space of bounded signed measures on with the weak topology generated by (the space of continuous functions on ). Since for all correspond to sub-probability measures, using compactness, by passing to a subsequence (denoted again by for convenience) let converge to in the weak topology. This in particular implies converges to almost everywhere (since the convergence happens at all continuity points of , see e.g., [16, Section 3.2] ). Since ’s are all bounded by and belong to by the bounded convergence theorem, it follows that . Next we will show that
[TABLE]
Clearly this implies and hence we would be done. The claim in (24) follows from the upper semicontinuity of or equivalently the lower semicontinuity of . To show the latter one represents as an appropriate Legendre transform. To proceed we need some definitions: Clearly (6) extends naturally to all non-negative measures. We extend to all of by setting it to be for all measures which are not non-negative. Moreover, for any define
[TABLE]
Now for any define . This function, by definition, is lower semicontinuous, since for any and a sequence converging to by definition of weak convergence,
[TABLE]
Thus the proof is complete by [12, Lemma 5] which says . ∎
7.2. Proof of Lemma 3.4
As already hinted right after the statement of Lemma 3.4, the proof is by contradiction. Assuming that the singular part of which we denote by (see (5)). has positive mass, we create a modification such that (see (6)). However in the process, it is possible that we violate the area constraint, i.e. . Thus we make a second modification to construct a function with the property and moreover it satisfies the area constraint as well. This contradicts the extremality of which was a part of the hypothesis. The details follow.
Let us assume that has total mass . Then clearly, without loss of generality, we can assume , i.e., there is an atom of mass at zero, since
[TABLE]
Also, because the absolutely continuous part stays the same, . We will now make some local modifications to contradict extremality of .
Let be a small number to be chosen later. Consider a new function , as illustrated in Figure 7, which is a linear function interpolating and and which agrees with on . Since , it follows that
[TABLE]
On the other hand, for all small enough ,
[TABLE]
The second last inequality uses the bound which follows from the Cauchy-Schwarz inequality. To see the last inequality, note that goes to zero as goes to zero. However, it is easy to see that
[TABLE]
Thus a priori need not be an element of ; (see (7)). To ensure that indeed , we have to make another modification. Note that already in the proof of Lemma 3.3 we argued that a priori even if is not unique, is unique. Thus there exist and depending only on such that the set has Lebesgue measure at least . (Note that even though the proof of Lemma 3.3 relied on Lemma 3.4, the uniqueness of the density was argued independently and hence this is not a circular argument.)
For brevity, let us call the set by the name . We now choose arbitrary disjoint subsets of for some , denoted by and , both of measure ; (we take the intersection with to ensure that both the sets are away from [math]). Note that this can always be done if . In case , we can modify by taking it to be a linear function interpolating and for some small enough so that ; (see Figure 7 ii.) Nothing changes in any of the arguments that follow as well as the conclusions and hence we will pretend that throughout the rest of the argument. Let us also choose and such that , and let where
[TABLE]
We will also choose . Note that since on , for all small enough is non-negative. Also, since the measures of and are the same,
[TABLE]
We now compute the area under the curve and see how it differs from that of . For every we have
[TABLE]
Thus,
[TABLE]
The last inequality follows since, as and , the integral above is at least . Thus, the new function traps at least as much area as does since
[TABLE]
for all small enough ; (the last inequality uses (25)).
Moreover, by Taylor expansion (using (27) and on ),
[TABLE]
We use the bound and that crucially in the last inequality, and all the constants depend only on through the Taylor expansion. Thus, by choosing we have , and hence using (26),
[TABLE]
for all small enough . Hence, we obtain a contradiction to the extremality of . ∎
7.3. Proof of Lemma 3.5
(i) The proof follows by taking the monotone rearrangement and using uniqueness. Let be the monotone rearrangement of . Notice that, by Fubini’s theorem,
[TABLE]
where . Only the second inequality above needs justification and it is a consequence of a standard rearrangement inequality. Thus satisfies the area constraint. Also clearly as rearrangement keeps integrals unchanged. This contradicts the uniqueness of unless
(ii) Let be zero on a set of positive measure. By the first part of the lemma, this implies that there exists such that is a constant on the interval . Note that it is easy to contradict extremality of if is not one on this interval. In case it is one on this interval, consider the function (where ). We claim that
[TABLE]
The first equality follows by Fubini’s theorem. The second becomes clear after the change of variable is made. Now, by uniqueness, , and by Lemma 3.4 has no singular part. However, has an atom of mass at [math] which implies . ∎
7.4. Proof of Lemma 5.6
The reader may find it useful to refer to Figure 5. Let and be the acute angles that the line segments and make with the -axis and the -axis. Now, without loss of generality, we can assume ; otherwise, we could work with , since clearly one of the two quantities is at most . Now, as a simple consequence of Theorem 1.10, we see that, with probability at least is at a distance from . Also, since is strictly concave, and , the line segment makes at least an angle (depending only on and not on and ) with the -axis. The proof is now completed by considering the triangle and simple geometric arguments. We omit the details. ∎
7.5. Proof of Theorem 2.1
The proof will follow by constructing a suitable martingale and appealing to well known concentration results for martingales. However things are slightly complicated by the possibility that the martingale may not have bounded increments. A simple truncation argument will allow us to take the increments to be bounded. Our proof strategy follows closely arguments in [10]. The proof relies on some coarse graining. We start by introducing some notation. Let
[TABLE]
Also let . Fix a number to be specified soon. Recall the point process and the path from Section 1.1.1. Let be the increasing path between and with the same constraints as along with the additional constraint that the intersection with is less than for all . Let us denote by the weight of . Consider the Doob Martingale , along the filtration . Note that the martingale increments are deterministically bounded by . The following is a standard consequence of the Azuma-Hoeffding inequality.
Lemma 7.1**.**
\mathbb{P}(\bigl{|}|\Gamma_{k}|-\mathbb{E}(|\Gamma_{k}|)|\geq t)\leq e^{-\frac{t^{2}}{4k^{2}n}}.
In the remainder of the section, we obtain a bound on \bigl{|}|\Gamma|-|\Gamma_{k}|\bigr{|} and thus also on \bigl{|}\mathbb{E}|\Gamma|-\mathbb{E}|\Gamma_{k}|\bigr{|}. Let be the point process obtained from by removing points arbitrarily if necessary from to make sure that for all . Let be the longest path with the same constraints as in the environment .
Lemma 7.2**.**
Deterministically as a consequence of the definitions it follows that .
Proof.
Clearly it suffices to show that intersects none of the ’s at more than points. The proof is by contradiction: assume that there exists such that . Since the points on are totally ordered (recall the ordering introduced in Section 1.1), let and be the smallest and largest points in the set . By definition of ,
[TABLE]
so that intersects at most three , since the number of different indices it can cross in each direction is at most one if (30) is to be satisfied. Thus has to intersect at least one of the boxes at more than points. This contradicts the definition of . ∎
Thus, it follows that , where and . Taking , the proof is now complete in view of the next result.
Lemma 7.3**.**
The random variable satisfies the following:
- (1)
** 2. (2)
.
This is a simple consequence of the observation that are independent Poisson variables with mean one and the following tail bound of a standard Poisson variable : . ∎
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] David Aldous and Persi Diaconis. Hammersley’s interacting particle process and longest increasing subsequences. Probab. Th. Rel. Fields , 103:199–213, 1995.
- 2[2] Kenneth S Alexander. Cube–root boundary fluctuations for droplets in random cluster models. Communications in Mathematical Physics , 224(3):733–781, 2001.
- 3[3] Antonio Auffinger, Michael Damron, and Jack Hanson. 50 years of first passage percolation. ar Xiv preprint ar Xiv:1511.03262 , 2015.
- 4[4] Jinho Baik, Percy Deift, and Kurt Johansson. On the distribution of the length of the longest increasing subsequence of random permutations. J. Amer. Math. Soc , 12:1119–1178, 1999.
- 5[5] Jinho Baik and Eric M. Rains. Symmetrized random permutations. In Random Matrix Models and Their Applications, volume 40 of Mathematical Sciences Research Institute Publications , pages 1–19, 2001.
- 6[6] Jinho Baik and Eric M. Rains. Symmetrized random permutations. MSRI volume: Random Matrix Models and Their Applications(40):1–19, 2001.
- 7[7] Riddhipratim Basu and Alan Hammond. Localization of near geodesics in Brownian Last Passage Percolation. In preparation.
- 8[8] Riddhipratim Basu, Vladas Sidoravicius, and Allan Sly. Last passage percolation with a defect line and the solution of the Slow Bond Problem. Preprint ar Xiv 1408.3464.
