Translation surface explained

In mathematics a translation surface is a surface obtained from identifying the sides of a polygon in the Euclidean plane by translations. An equivalent definition is a Riemann surface together with a holomorphic 1-form.

These surfaces arise in dynamical systems where they can be used to model billiards, and in Teichmüller theory. A particularly interesting subclass is that of Veech surfaces (named after William A. Veech) which are the most symmetric ones.

Definitions

Geometric definition

A translation surface is the space obtained by identifying pairwise by translations the sides of a collection of plane polygons.

Here is a more formal definition. Let

P1,\ldots,Pm

be a collection of (not necessarily convex) polygons in the Euclidean plane and suppose that for every side

si

of any

Pk

there is a side

sj

of some

Pl

with

j\not=i

and

sj=si+\vecvi

for some nonzero vector

\vecvi

(and so that

\vecvj=-\vecvi

. Consider the space obtained by identifying all

si

with their corresponding

sj

through the map

x\mapstox+\vecvi

.

The canonical way to construct such a surface is as follows: start with vectors

\vecw1,\ldots,\vecwn

and a permutation

\sigma

on

\{1,\ldots,n\}

, and form the broken lines

L=x,x+\vecw1,\ldots,x+\vecw1+ … +\vecwn

and

L'=x,x+\vecw\sigma(1),\ldots,x+\vecw\sigma(1)+ … +\vecw\sigma(n)

starting at an arbitrarily chosen point. In the case where these two lines form a polygon (i.e. they do not intersect outside of their endpoints) there is a natural side-pairing.

The quotient space is a closed surface. It has a flat metric outside the set

\Sigma

images of the vertices. At a point in

\Sigma

the sum of the angles of the polygons around the vertices which map to it is a positive multiple of

2\pi

, and the metric is singular unless the angle is exactly

2\pi

.

Analytic definition

Let

S

be a translation surface as defined above and

\Sigma

the set of singular points. Identifying the Euclidean plane with the complex plane one gets coordinates charts on

S\setminus\Sigma

with values in

C

. Moreover, the changes of charts are holomorphic maps, more precisely maps of the form

z\mapstoz+w

for some

w\inC

. This gives

S\setminus\Sigma

the structure of a Riemann surface, which extends to the entire surface

S

by Riemann's theorem on removable singularities. In addition, the differential

dz

where

z:U\toC

is any chart defined above, does not depend on the chart. Thus these differentials defined on chart domains glue together to give a well-defined holomorphic 1-form

\omega

on

S

. The vertices of the polygon where the cone angles are not equal to

2\pi

are zeroes of

\omega

(a cone angle of

2k\pi

corresponds to a zero of order

(k-1)

).

In the other direction, given a pair

(X,\omega)

where

X

is a compact Riemann surface and

\omega

a holomorphic 1-form one can construct a polygon by using the complex numbers \int_\omega where

\gammaj

are disjoint paths between the zeroes of

\omega

which form an integral basis for the relative cohomology.

Examples

The simplest example of a translation surface is obtained by gluing the opposite sides of a parallelogram. It is a flat torus with no singularities.

If

P

is a regular

4g

-gon then the translation surface obtained by gluing opposite sides is of genus

g

with a single singular point, with angle

(2g-1)2\pi

.

If

P

is obtained by putting side to side a collection of copies of the unit square then any translation surface obtained from

P

is called a square-tiled surface. The map from the surface to the flat torus obtained by identifying all squares is a branched covering with branch points the singularities (the cone angle at a singularity is proportional to the degree of branching).

Riemann - Roch and Gauss - Bonnet

Suppose that the surface

X

is a closed Riemann surface of genus

g

and that

\omega

is a nonzero holomorphic 1-form on

X

, with zeroes of order

d1,\ldots,dm

. Then the Riemann–Roch theorem implies that
m
\sum
j=1

dj=2g-2.

If the translation surface

(X,\omega)

is represented by a polygon

P

then triangulating it and summing angles over all vertices allows to recover the formula above (using the relation between cone angles and order of zeroes), in the same manner as in the proof of the Gauss–Bonnet formula for hyperbolic surfaces or the proof of Euler's formula from Girard's theorem.

Translation surfaces as foliated surfaces

If

(X,\omega)

is a translation surface there is a natural measured foliation on

X

. If it is obtained from a polygon it is just the image of vertical lines, and the measure of an arc is just the euclidean length of the horizontal segment homotopic to the arc. The foliation is also obtained by the level lines of the imaginary part of a (local) primitive for

\omega

and the measure is obtained by integrating the real part.

Moduli spaces

Strata

Let

lH

be the set of translation surfaces of genus

g

(where two such

(X,\omega),(X',\omega')

are considered the same if there exists a holomorphic diffeomorphism

\phi:X\toX'

such that

\phi*\omega'=\omega

). Let

lMg

be the moduli space of Riemann surfaces of genus

g

; there is a natural map

lH\tolMg

mapping a translation surface to the underlying Riemann surface. This turns

lH

into a locally trivial fiber bundle over the moduli space.

To a compact translation surface

(X,\omega)

there is associated the data

(k1,\ldots,km)

where

k1\lek2\le

are the orders of the zeroes of

\omega

. If

\alpha=(k1,\ldots,km)

is any integer partition of

2g-2

then the stratum

lH(\alpha)

is the subset of

lH

of translation surfaces which have a holomorphic form whose zeroes match the partition.

The stratum

lH(\alpha)

is naturally a complex orbifold of complex dimension

2g+m-1

(note that

lH(0)

is the moduli space of tori, which is well-known to be an orbifold; in higher genus, the failure to be a manifold is even more dramatic). Local coordinates are given by

(X,\omega)\mapsto

\left(\int
\gamma1

\omega,\ldots,

\int
\gamman

\omega\right)

where

n=\dim(H1(S,\{x1,\ldots,xm\}))=2g+m-1

and

\gamma1,\ldots,\gammak

is as above a symplectic basis of this space.

Masur-Veech volumes

The stratum

lH(\alpha)

admits a

{C}*

-action and thus a real and complex projectivization

{lH(\alpha)}\to{lH}1(\alpha)\to{lH}2(\alpha)

. The real projectivization admits a natural section

{lH}1(\alpha)\to{lH}(\alpha)

if we define it as the space of translation surfaces of area 1.

The existence of the above period coordinates allows to endow the stratum

lH(\alpha)

with an integral affine structure and thus a natural volume form

\nu

. We also get a volume form

\nu1(\alpha)

on

{lH}1(\alpha)

by disintegration of

\nu

. The Masur-Veech volume

Vol(\alpha)

is the total volume of

{lH}1(\alpha)

for

\nu1(\alpha)

. This volume was proved to be finite independently by William A. Veech[1] and Howard Masur.[2]

In the 90's Maxim Kontsevich and Anton Zorich evaluated these volumes numerically by counting the lattice points of

{lH}(\alpha)

. They observed that

Vol(\alpha)

should be of the form

\pi2g

times a rational number. From this observation they expected the existence of a formula expressing the volumes in terms of intersection numbers on moduli spaces of curves.

Alex Eskin and Andrei Okounkov gave the first algorithm to compute these volumes. They showed that the generating series of these numbers are q-expansions of computable quasi-modular forms. Using this algorithm they could confirm the numerical observation of Kontsevich and Zorich.[3]

More recently Chen, Möller, Sauvaget, and don Zagier showed that the volumes can be computed as intersection numbers on an algebraic compactification of

{lH}2(\alpha)

. Currently the problem is still open to extend this formula to strata of half-translation surfaces.[4]

The SL2(R)-action

If

(X,\omega)

is a translation surface obtained by identifying the faces of a polygon

P

and

g\inSL2(R)

then the translation surface

g(X,\omega)

is that associated to the polygon

g(P)

. This defined a continuous action of

SL2(R)

on the moduli space

lH

which preserves the strata

lH(\alpha)

. This action descends to an action on

{lH}1(\alpha)

that is ergodic with respect to

\nu1

.

Half-translation surfaces

Definitions

A half-translation surface is defined similarly to a translation surface but allowing the gluing maps to have a nontrivial linear part which is a half turn. Formally, a translation surface is defined geometrically by taking a collection of polygons in the Euclidean plane and identifying faces by maps of the form

z\mapsto\pmz+w

(a "half-translation"). Note that a face can be identified with itself. The geometric structure obtained in this way is a flat metric outside of a finite number of singular points with cone angles positive multiples of

\pi

.

As in the case of translation surfaces there is an analytic interpretation: a half-translation surface can be interpreted as a pair

(X,\phi)

where

X

is a Riemann surface and

\phi

a quadratic differential on

X

. To pass from the geometric picture to the analytic picture one simply takes the quadratic differential defined locally by

(dz)2

(which is invariant under half-translations), and for the other direction one takes the Riemannian metric induced by

\phi

, which is smooth and flat outside of the zeros of

\phi

.

Relation with Teichmüller geometry

If

X

is a Riemann surface then the vector space of quadratic differentials on

X

is naturally identified with the tangent space to Teichmüller space at any point above

X

. This can be proven by analytic means using the Bers embedding. Half-translation surfaces can be used to give a more geometric interpretation of this: if

(X,g),(Y,h)

are two points in Teichmüller space then by Teichmüller's mapping theorem there exists two polygons

P,Q

whose faces can be identified by half-translations to give flat surfaces with underlying Riemann surfaces isomorphic to

X,Y

respectively, and an affine map

f

of the plane sending

P

to

Q

which has the smallest distortion among the quasiconformal mappings in its isotopy class, and which is isotopic to

h\circg-1

.

Everything is determined uniquely up to scaling if we ask that

f

be of the form

fs

, where

ft:(x,y)\mapsto(etx,e-ty)

, for some

s>0

; we denote by

Xt

the Riemann surface obtained from the polygon

ft(P)

. Now the path

t\mapsto(Xt,ft\circg)

in Teichmüller space joins

(X,g)

to

(Y,h)

, and differentiating it at

t=0

gives a vector in the tangent space; since

(Y,g)

was arbitrary we obtain a bijection.

In facts the paths used in this construction are Teichmüller geodesics. An interesting fact is that while the geodesic ray associated to a flat surface corresponds to a measured foliation, and thus the directions in tangent space are identified with the Thurston boundary, the Teichmüller geodesic ray associated to a flat surface does not always converge to the corresponding point on the boundary,[5] though almost all such rays do so.[6]

Veech surfaces

The Veech group

If

(X,\omega)

is a translation surface its Veech group is the Fuchsian group which is the image in

PSL2(R)

of the subgroup

SL(X,\omega)\subsetSL2(R)

of transformations

g

such that

g(X,\omega)

is isomorphic (as a translation surface) to

(X,\omega)

. Equivalently,

SL(X,\omega)

is the group of derivatives of affine diffeomorphisms

(X,\omega)\to(X,\omega)

(where affine is defined locally outside the singularities, with respect to the affine structure induced by the translation structure). Veech groups have the following properties:

PSL2(R)

;

Veech groups can be either finitely generated or not.[7]

Veech surfaces

A Veech surface is by definition a translation surface whose Veech group is a lattice in

PSL2(R)

, equivalently its action on the hyperbolic plane admits a fundamental domain of finite volume. Since it is not cocompact it must then contain parabolic elements.

PSL2(Z)

. The square can be replaced by any parallelogram (the translation surfaces obtained are exactly those obtained as ramified covers of a flat torus). In fact the Veech group is arithmetic (which amounts to it being commensurable to the modular group) if and only if the surface is tiled by parallelograms.

There exists Veech surfaces whose Veech group is not arithmetic, for example the surface obtained from two regular pentagons glued along an edge: in this case the Veech group is a non-arithmetic Hecke triangle group. On the other hand, there are still some arithmetic constraints on the Veech group of a Veech surface: for example its trace field is a number field that is totally real.[8]

Geodesic flow on translation surfaces

Geodesics

A geodesic in a translation surface (or a half-translation surface) is a parametrised curve which is, outside of the singular points, locally the image of a straight line in Euclidean space parametrised by arclength. If a geodesic arrives at a singularity it is required to stop there. Thus a maximal geodesic is a curve defined on a closed interval, which is the whole real line if it does not meet any singular point. A geodesic is closed or periodic if its image is compact, in which case it is either a circle if it does not meet any singularity, or an arc between two (possibly equal) singularities. In the latter case the geodesic is called a saddle connection.

If

(X,\omega)

\theta\inR/2\piZ

(or

\theta\inR/\piZ

in the case of a half-translation surface) then the geodesics with direction theta are well-defined on

X

: they are those curves

c

which satisfy

\omega(\overset{}{c})=ei\theta

(or

\phi(\overset{}{c})=ei\theta

in the case of a half-translation surface

(X,\phi)

). The geodesic flow on

(X,\omega)

with direction

\theta

is the flow

\phit

on

X

where

t\mapsto\phit(p)

is the geodesic starting at

p

with direction

\theta

if

p

is not singular.

Dynamical properties

On a flat torus the geodesic flow in a given direction has the property that it is either periodic or ergodic. In general this is not true: there may be directions in which the flow is minimal (meaning every orbit is dense in the surface) but not ergodic. On the other hand, on a compact translation surface the flow retains from the simplest case of the flat torus the property that it is ergodic in almost every direction.

Another natural question is to establish asymptotic estimates for the number of closed geodesics or saddle connections of a given length. On a flat torus

T

there are no saddle connections and the number of closed geodesics of length

\leL

is equivalent to

L2/\operatorname{volume}(T)

. In general one can only obtain bounds: if

(X,\omega)

is a compact translation surface of genus

g

then there exists constants (depending only on the genus)

c1,c2

such that the both

Ncg(L)

of closed geodesics and

Nsc(L)

of saddle connections of length

\leL

satisfy
c1L2
\operatorname{volume

(X,\omega)}\leNcg(L),Nsc(L)\le

c2L2
\operatorname{volume

(X,\omega)}.

Restraining to a probabilistic results it is possible to get better estimates: given a genus

g

, a partition

\alpha

of

g

and a connected component

lC

of the stratum

lH(\alpha)

there exists constants

ccgcsc

such that for almost every

(X,\omega)\inlC

the asymptotic equivalent holds:

Ncg(L)\sim

ccgL2
\operatorname{volume

(X,\omega)}

,

Nsc(L)\sim

cscL2
\operatorname{volume

(X,\omega)}.

The constants

ccg,csc

are called Siegel - Veech constants. Using the ergodicity of the

SL2(R)

-action on

l{H}(\alpha)

, it was shown that these constants can explicitly be computed as ratios of certain Masur-Veech volumes.[9]

Veech dichotomy

The geodesic flow on a Veech surface is much better behaved than in general. This is expressed via the following result, called the Veech dichotomy:

Let

(X,\omega)

be a Veech surface and

\theta

a direction. Then either all trajectories defied over

R

are periodic or the flow in the direction

\theta

is ergodic.

Relation with billiards

If

P0

is a polygon in the Euclidean plane and

\theta\inR/2\piZ

a direction there is a continuous dynamical system called a billiard. The trajectory of a point inside the polygon is defined as follows: as long as it does not touch the boundary it proceeds in a straight line at unit speed; when it touches the interior of an edge it bounces back (i.e. its direction changes with an orthogonal reflection in the perpendicular of the edge), and when it touches a vertex it stops.

This dynamical system is equivalent to the geodesic flow on a flat surface: just double the polygon along the edges and put a flat metric everywhere but at the vertices, which become singular points with cone angle twice the angle of the polygon at the corresponding vertex. This surface is not a translation surface or a half-translation surface, but in some cases it is related to one. Namely, if all angles of the polygon

P0

are rational multiples of

\pi

there is ramified cover of this surface which is a translation surface, which can be constructed from a union of copies of

P0

. The dynamics of the billiard flow can then be studied through the geodesic flow on the translation surface.

For example, the billiard in a square is related in this way to the billiard on the flat torus constructed from four copies of the square; the billiard in an equilateral triangle gives rise to the flat torus constructed from an hexagon. The billiard in a "L" shape constructed from squares is related to the geodesic flow on a square-tiled surface; the billiard in the triangle with angles

\pi/5,\pi/5,3\pi/5

is related to the Veech surface constructed from two regular pentagons constructed above.

Relation with interval exchange transformations

Let

(X,\omega)

be a translation surface and

\theta

a direction, and let

\phit

be the geodesic flow on

(X,\omega)

with direction

\theta

. Let

I

be a geodesic segment in the direction orthogonal to

\theta

, and defined the first recurrence, or Poincaré map

\sigma:I\toI

as follows:

\sigma(p)

is equal to

\phit(p)

where

\phis(p)\not\inI

for

0<s<t

. Then this map is an interval exchange transformation and it can be used to study the dynamic of the geodesic flow.

References

Notes and References

  1. gaussmeas. Veech . William A. . Gauss Measures for Transformations on the Space of Interval Exchange Maps . Annals of Mathematics . 115 . 2 . 1982 . 201 - 242 . 10.2307/1971391 . 1971391 .
  2. measfol. Masur . Howard . Interval Exchange Transformations and Measured Foliations . Annals of Mathematics . 115 . 1 . 1982 . 169 - 200 . 10.2307/1971341 . 1971341 .
  3. asy. Eskin . Alex . Okounkov . Andrei. Asymptotics of numbers of branched coverings of a torus and volumes of moduli spaces of holomorphic differentials . Inventiones Mathematicae . 145 . 2001 . 1 . 59 - 103 . 10.1007/s002220100142. math/0006171 . 2001InMat.145...59E . 14125769 .
  4. intersection. Chen . Dawei . Möller . Martin. Sauvaget . Adrien . Zagier . Don Bernhard. Masur-Veech volumes and intersection theory on moduli spaces of abelian differentials. Inventiones Mathematicae . 2019 . 222 . 1 . 283 . 10.1007/s00222-020-00969-4 . 1901.01785. 2020InMat.222..283C . 119655348 .
  5. Lenzhen . Anna . Teichmüller geodesics that do not have a limit in PMF . Geometry and Topology . 12 . 2008 . 177 - 197 . 10.2140/gt.2008.12.177. math/0511001 . 16047629 .
  6. Masur . Howard . Two boundaries of TeichmÛller space . Duke Math. J. . 49 . 1982 . 183 - 190 . 650376 . 10.1215/s0012-7094-82-04912-2.
  7. McMullen . Curtis T. . Teichmüller geodesics of infinite complexity . Acta Math. . 191 . 2 . 2003 . 191 - 223 . 10.1007/bf02392964. free .
  8. Hubert . Pascal . Lanneau . Erwan . Veech groups without parabolic elements . Duke Mathematical Journal . 2006 . 133 . 2 . 335–346 . 10.1215/s0012-7094-06-13326-4 . math/0503047 . 14274833 .
  9. principal . Eskin . Alex . Masur . Howard . Zorich. Anton. Moduli spaces of abelian differentials : the principal boundary, counting problems, and the Siegel-Veech constants . Publications Mathématiques de l'IHÉS . 2003 . 97 . 61–179 . 10.1007/s10240-003-0015-1 . math/0202134 . 119713402 .