geometry and dynamics on infinite-type flat surfaces

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Geometry and dynamics on infinite-type flat surfaces. Ferr´ an Valdez [email protected] UNAM ´ Ecole en Syst` emes Dynamiques Contemporains, 2017. Universit´ e de Montr´ eal Ferr´ an Valdez Geometry and dynamics on infinite type flat surfaces .

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Page 1: Geometry and dynamics on infinite-type flat surfaces

Geometry and dynamics on infinite-type flatsurfaces.

Ferran Valdez

[email protected]

Ecole en Systemes Dynamiques Contemporains, 2017.Universite de Montreal

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 2: Geometry and dynamics on infinite-type flat surfaces

Index

1 Examples of infinite-type translation surfaces.2 Main definitions and general aspects.3 Affine symmetries and Veech groups.4 Dynamical properties of the translation flow (recurrence

and ergodicity).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 3: Geometry and dynamics on infinite-type flat surfaces

Examples of infinite-typetranslation surfaces.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 4: Geometry and dynamics on infinite-type flat surfaces

Example: polygonal billiards

Consider the dynamical system defined by the frictionless motionof a point inside an Euclidean polygon P where collisions with theboundary are elastic, that is, each time a point hits a side of thepolygon its angle of incidence is equal to its angle of reflection.

Convention: the motion of a point ends when reaching a corner.

Conjecture: every triangular billiard has a closedtrajectory.

“It is fair to say that this 200-year-old problem is widely regarded as impenetrable.” R.E. Schwartz

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 5: Geometry and dynamics on infinite-type flat surfaces

Example: polygonal billiards

Consider the dynamical system defined by the frictionless motionof a point inside an Euclidean polygon P where collisions with theboundary are elastic, that is, each time a point hits a side of thepolygon its angle of incidence is equal to its angle of reflection.

Convention: the motion of a point ends when reaching a corner.

Conjecture: every triangular billiard has a closedtrajectory.

“It is fair to say that this 200-year-old problem is widely regarded as impenetrable.” R.E. Schwartz

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 6: Geometry and dynamics on infinite-type flat surfaces

Example: polygonal billiards

Consider the dynamical system defined by the frictionless motionof a point inside an Euclidean polygon P where collisions with theboundary are elastic, that is, each time a point hits a side of thepolygon its angle of incidence is equal to its angle of reflection.

Convention: the motion of a point ends when reaching a corner.

Conjecture: every triangular billiard has a closedtrajectory.

“It is fair to say that this 200-year-old problem is widely regarded as impenetrable.” R.E. Schwartz

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 7: Geometry and dynamics on infinite-type flat surfaces

The unfolding trick

Idea: construct a surface SP out of P on which billiard trayectoriesbecome “straight lines”.

1 Reflect P w.r.t each of its sides & glue along these sides.Iterate on each new copy.

2 Identify any two copies on P that differ by a translation (usingthe corresponding translation) .

Remark. By construction, change of coordinates in SP aretranslations.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 8: Geometry and dynamics on infinite-type flat surfaces

The unfolding trick

Idea: construct a surface SP out of P on which billiard trayectoriesbecome “straight lines”.

1 Reflect P w.r.t each of its sides & glue along these sides.Iterate on each new copy.

2 Identify any two copies on P that differ by a translation (usingthe corresponding translation) .

Remark. By construction, change of coordinates in SP aretranslations.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 9: Geometry and dynamics on infinite-type flat surfaces

The unfolding trick

Idea: construct a surface SP out of P on which billiard trayectoriesbecome “straight lines”.

1 Reflect P w.r.t each of its sides & glue along these sides.Iterate on each new copy.

2 Identify any two copies on P that differ by a translation (usingthe corresponding translation) .

Remark. By construction, change of coordinates in SP aretranslations.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 10: Geometry and dynamics on infinite-type flat surfaces

The unfolding trick

Idea: construct a surface SP out of P on which billiard trayectoriesbecome “straight lines”.

1 Reflect P w.r.t each of its sides & glue along these sides.Iterate on each new copy.

2 Identify any two copies on P that differ by a translation (usingthe corresponding translation) .

Remark. By construction, change of coordinates in SP aretranslations.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 11: Geometry and dynamics on infinite-type flat surfaces

Example: polygonal billiards

A

A

B

B C

C

D

D

P

SP

P

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 12: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards

Thm. Let F tθ be the translation flow on T 2 = R2/Z2.

1 F tθ is periodic iff tan(θ) = p

q2 F t

θ is uniquely ergodic iff tan(θ) is irrational.

A similar statement is valid for the 2-torus arising from the triangle(π2 ,

π8 ). (Key word: Veech’s dychotomy.)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 13: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards

Thm. Let F tθ be the translation flow on T 2 = R2/Z2.

1 F tθ is periodic iff tan(θ) = p

q2 F t

θ is uniquely ergodic iff tan(θ) is irrational.

A similar statement is valid for the 2-torus arising from the triangle(π2 ,

π8 ). (Key word: Veech’s dychotomy.)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 14: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards

Exercise. Let P be a polygon whose interior angles are ofthe form pi

qiπ, i = 1, . . . , n and N = lcm(q1, . . . , qn). Then

SP is a closed oriented surface whose genus g(SP) is givenby:

g(SP) = 1 + N2

(n − 2−

n∑1

1qi

)

These kind of polygons are called rational polygons. All other poly-gons are said to be irrational.

Natural question: what can be said about the topology of SP whenP is irrational?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 15: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards

Exercise. Let P be a polygon whose interior angles are ofthe form pi

qiπ, i = 1, . . . , n and N = lcm(q1, . . . , qn). Then

SP is a closed oriented surface whose genus g(SP) is givenby:

g(SP) = 1 + N2

(n − 2−

n∑1

1qi

)

These kind of polygons are called rational polygons. All other poly-gons are said to be irrational.

Natural question: what can be said about the topology of SP whenP is irrational?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 16: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards

Exercise. Let P be a polygon whose interior angles are ofthe form pi

qiπ, i = 1, . . . , n and N = lcm(q1, . . . , qn). Then

SP is a closed oriented surface whose genus g(SP) is givenby:

g(SP) = 1 + N2

(n − 2−

n∑1

1qi

)

These kind of polygons are called rational polygons. All other poly-gons are said to be irrational.

Natural question: what can be said about the topology of SP whenP is irrational?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 17: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards, irrational case

Theorem. Let P be an irrational polygon. Then SP hasinfinite genus and only one end.

Up to homeo. there is only one orientable surface of infinitegenus and one end. It is called the Loch Ness monster (Phillips-Sullivan/Ghys).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 18: Geometry and dynamics on infinite-type flat surfaces

Example:polygonal billiards, irrational case

Theorem. Let P be an irrational polygon. Then SP hasinfinite genus and only one end.

Up to homeo. there is only one orientable surface of infinitegenus and one end. It is called the Loch Ness monster (Phillips-Sullivan/Ghys).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 19: Geometry and dynamics on infinite-type flat surfaces

Back to periodic orbits

Conjecture. Let P be an irrational polygon and SP thecorresponding Loch Ness monster obtained by the unfolding-trick. There exists a direction θ for which F t

θ has a periodicorbit.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 20: Geometry and dynamics on infinite-type flat surfaces

Example:The Ehrenfest2 Wind-tree model (1912)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 21: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 22: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

a

b

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 23: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 24: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 25: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 26: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 27: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 28: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 29: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 30: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 31: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 32: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 33: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 34: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 35: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 36: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 37: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 38: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 39: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 40: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model (1980)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 41: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 42: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 43: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 44: Geometry and dynamics on infinite-type flat surfaces

Example: Hardy-Weber’s periodic wind-tree model is acovering of this genus 5 surface

D00

D01

D01

D00

C00 C10 C10 C00

D10

D11

D11

D10

C01 C11 C11 C01

B00

B00

B01

B01

B10

B10

B11

B11

A00 A00

A10 A10

A01 A01

A11 A11

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 45: Geometry and dynamics on infinite-type flat surfaces

Example: the infinite staircase

A−2

B−2

A−1

B−1

A0

B0

A1

B1

A2

B2

A2

B3

A1

B2

A0

B1

A−1

B0

A−2

B−1

2

1

0

-1

-2

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 46: Geometry and dynamics on infinite-type flat surfaces

Example: baker’s surface

A1 A2 A3 A4. . .

.

.

.B4

B3

B2

B1

A1A2A3A4. . .

.

.

.

B4

B3

B2

B1

a b

cd

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 47: Geometry and dynamics on infinite-type flat surfaces

Example: Thurston-Veech-McMullen-Hooper’sconstruction of pseudo-Anosovs

INPUT: (1) G bipartite graph with a ribbon structure. V (G) =HtV . (2) A posivite eigenfunction f : V (G)→ R+ of the adjacencyoperator.

OUTPUT: a very symmetric infinite type translation surface witha“pseudo-Anosov” homeomorphism. We have two natural maps:

Hor : E (G)→ H, Vert : E (G)→ V

These and the ribbon structure define two permutations on the setof edges of G :

E(e) = pHor(e)(e), N (e) = pVert(e)(e).

For each edge e let

Re = [0, f ◦ Vert(e)]× [0, f ◦ Hor(e)]

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 48: Geometry and dynamics on infinite-type flat surfaces

Example: Thurston-Veech-McMullen-Hooper’sconstruction of pseudo-Anosovs

INPUT: (1) G bipartite graph with a ribbon structure. V (G) =HtV . (2) A posivite eigenfunction f : V (G)→ R+ of the adjacencyoperator.

OUTPUT: a very symmetric infinite type translation surface witha“pseudo-Anosov” homeomorphism.

We have two natural maps:

Hor : E (G)→ H, Vert : E (G)→ V

These and the ribbon structure define two permutations on the setof edges of G :

E(e) = pHor(e)(e), N (e) = pVert(e)(e).

For each edge e let

Re = [0, f ◦ Vert(e)]× [0, f ◦ Hor(e)]

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 49: Geometry and dynamics on infinite-type flat surfaces

Example: Thurston-Veech-McMullen-Hooper’sconstruction of pseudo-Anosovs

INPUT: (1) G bipartite graph with a ribbon structure. V (G) =HtV . (2) A posivite eigenfunction f : V (G)→ R+ of the adjacencyoperator.

OUTPUT: a very symmetric infinite type translation surface witha“pseudo-Anosov” homeomorphism. We have two natural maps:

Hor : E (G)→ H, Vert : E (G)→ V

These and the ribbon structure define two permutations on the setof edges of G :

E(e) = pHor(e)(e), N (e) = pVert(e)(e).

For each edge e let

Re = [0, f ◦ Vert(e)]× [0, f ◦ Hor(e)]

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 50: Geometry and dynamics on infinite-type flat surfaces

Example: Thurston-Veech-McMullen-Hooper’sconstruction of pseudo-Anosovs

INPUT: (1) G bipartite graph with a ribbon structure. V (G) =HtV . (2) A posivite eigenfunction f : V (G)→ R+ of the adjacencyoperator.

OUTPUT: a very symmetric infinite type translation surface witha“pseudo-Anosov” homeomorphism. We have two natural maps:

Hor : E (G)→ H, Vert : E (G)→ V

These and the ribbon structure define two permutations on the setof edges of G :

E(e) = pHor(e)(e), N (e) = pVert(e)(e).

For each edge e let

Re = [0, f ◦ Vert(e)]× [0, f ◦ Hor(e)]

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 51: Geometry and dynamics on infinite-type flat surfaces

Example: T-V-McM-H’s construction of p.Anosovs

We have two natural maps:

Hor : E (G)→ H, Vert : E (G)→ V

These and the ribbon structure define two permutations on the setof edges of G :

E(e) = pHor(e)(e), N (e) = pVert(e)(e).

For each edge e let

R = [0, f ◦ Vert(e)]× [0, f ◦ Hor(e)]

GLUEING RULES (using translations). For each edge e ∈ E (G):1 Glue the right side of Re to the left side of RE(e) and2 the top side of Re to the bottom side of RN (e).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 52: Geometry and dynamics on infinite-type flat surfaces

Example: T-V-McM-H’s construction of p.Anosovs

Exercise.1 Suppose that S = S(G , f ) is a

Thurston-Veech-McMullen-Hooper surface. Show that:

Area(S) = λ

2∑

v∈V(G)f(v)2

2 Perform the construction for:√23

√23

√23

1√22

12

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 53: Geometry and dynamics on infinite-type flat surfaces

Main definitions and generalaspects.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 54: Geometry and dynamics on infinite-type flat surfaces

Three definitions: constructive

Definition. Let P be an at most countable set of Euclideanpolygons and f : E (P)→ E (P) a pairing of edges. Let M be⊔

P∈P P/ ∼ deprived of all vertices of infinite degree. If Mis connected we call it the translation surface obtained fromthe family of polygons P.

For each vertex v ∈ P ∈ P we denote by αv ∈ (0, 2π) the interiorangle of P at v . For each finite degre vertex v ∈ P there existspositive integer kv so that∑

w∈π−1(π(v))αw = 2kvπ. (1)

If kv > 1, the point π(v) ∈ M is called a (finite) conical singularityof angle 2πkv while if k = 1 it is called a regular point.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 55: Geometry and dynamics on infinite-type flat surfaces

Three definitions: constructive

Definition. Let P be an at most countable set of Euclideanpolygons and f : E (P)→ E (P) a pairing of edges. Let M be⊔

P∈P P/ ∼ deprived of all vertices of infinite degree. If Mis connected we call it the translation surface obtained fromthe family of polygons P.

For each vertex v ∈ P ∈ P we denote by αv ∈ (0, 2π) the interiorangle of P at v . For each finite degre vertex v ∈ P there existspositive integer kv so that∑

w∈π−1(π(v))αw = 2kvπ. (1)

If kv > 1, the point π(v) ∈ M is called a (finite) conical singularityof angle 2πkv while if k = 1 it is called a regular point.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 56: Geometry and dynamics on infinite-type flat surfaces

Three definitions: constructive

Definition. Let P be an at most countable set of Euclideanpolygons and f : E (P)→ E (P) a pairing of edges. Let M be⊔

P∈P P/ ∼ deprived of all vertices of infinite degree. If Mis connected we call it the translation surface obtained fromthe family of polygons P.

For each vertex v ∈ P ∈ P we denote by αv ∈ (0, 2π) the interiorangle of P at v . For each finite degre vertex v ∈ P there existspositive integer kv so that∑

w∈π−1(π(v))αw = 2kvπ. (1)

If kv > 1, the point π(v) ∈ M is called a (finite) conical singularityof angle 2πkv while if k = 1 it is called a regular point.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 57: Geometry and dynamics on infinite-type flat surfaces

Three definitions: geometric

Remark that by construction M deprived from all conical singularitiesadmits an atlas whose transition functions are translations.

Definition. A translation surface is a pair (S, T ) made ofa connected topological surface S and a maximal translationatlas T on S \ Σ, where:

1 Σ is a discrete subset of S and2 every z ∈ Σ is a finite conical singularity*.

The maximal translation atlas T is called a translation surfacestructure on S and its charts are called the flat charts or flatcoordinates.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 58: Geometry and dynamics on infinite-type flat surfaces

Three definitions: geometric

Remark that by construction M deprived from all conical singularitiesadmits an atlas whose transition functions are translations.

Definition. A translation surface is a pair (S, T ) made ofa connected topological surface S and a maximal translationatlas T on S \ Σ, where:

1 Σ is a discrete subset of S and2 every z ∈ Σ is a finite conical singularity*.

The maximal translation atlas T is called a translation surfacestructure on S and its charts are called the flat charts or flatcoordinates.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 59: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide structure

At any point x of M \ Σ we can pull-back using flat charts theEuclidean metric of C. This gives rise to a globally well-defined flatmetric µ on M \ Σ.

This metric provides a notion of distance andarea. If z = x + iy is a flat chart on M \Σ then µ is given in thesecoordinates by dx2 + dy2 and the area by dx ∧ dy = i

2 dz ∧ dz .Wedenote by M the metric completion of M \ Σ w.r.t. (the intrinsicmetric induced by) µ. We also have a well defined Lebegue measureλ on M.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 60: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide structure

At any point x of M \ Σ we can pull-back using flat charts theEuclidean metric of C. This gives rise to a globally well-defined flatmetric µ on M \ Σ.This metric provides a notion of distance andarea. If z = x + iy is a flat chart on M \Σ then µ is given in thesecoordinates by dx2 + dy2 and the area by dx ∧ dy = i

2 dz ∧ dz .

Wedenote by M the metric completion of M \ Σ w.r.t. (the intrinsicmetric induced by) µ. We also have a well defined Lebegue measureλ on M.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 61: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide structure

At any point x of M \ Σ we can pull-back using flat charts theEuclidean metric of C. This gives rise to a globally well-defined flatmetric µ on M \ Σ.This metric provides a notion of distance andarea. If z = x + iy is a flat chart on M \Σ then µ is given in thesecoordinates by dx2 + dy2 and the area by dx ∧ dy = i

2 dz ∧ dz .Wedenote by M the metric completion of M \ Σ w.r.t. (the intrinsicmetric induced by) µ.

We also have a well defined Lebegue measureλ on M.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 62: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide structure

At any point x of M \ Σ we can pull-back using flat charts theEuclidean metric of C. This gives rise to a globally well-defined flatmetric µ on M \ Σ.This metric provides a notion of distance andarea. If z = x + iy is a flat chart on M \Σ then µ is given in thesecoordinates by dx2 + dy2 and the area by dx ∧ dy = i

2 dz ∧ dz .Wedenote by M the metric completion of M \ Σ w.r.t. (the intrinsicmetric induced by) µ. We also have a well defined Lebegue measureλ on M.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 63: Geometry and dynamics on infinite-type flat surfaces

Conical and wild singularities

Definition. A point p ∈ M is called a conical singularity ifthere exists a neighborhood U of p in M such that U \ p isisometric to a flat cyclic covering Uk of degree k over thepunctured disc {z ∈ C | 0 < |z | < ε}, for some ε > 0 andk ∈ {2, 3, . . . ,∞}. If the degre k of the covering is finite wesay that p is a conical singularity of finite angle 2πk and ifk =∞ we say that p is an infinite angle singularity.

Definition. A point p ∈ M \M which is not a conical singu-larity is called a wild singularity. The subset of M formed byall conic and wild singularities is called the set of singularitiesof M and will be denoted by Sing(M).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 64: Geometry and dynamics on infinite-type flat surfaces

Conical and wild singularities

Definition. A point p ∈ M is called a conical singularity ifthere exists a neighborhood U of p in M such that U \ p isisometric to a flat cyclic covering Uk of degree k over thepunctured disc {z ∈ C | 0 < |z | < ε}, for some ε > 0 andk ∈ {2, 3, . . . ,∞}. If the degre k of the covering is finite wesay that p is a conical singularity of finite angle 2πk and ifk =∞ we say that p is an infinite angle singularity.

Definition. A point p ∈ M \M which is not a conical singu-larity is called a wild singularity. The subset of M formed byall conic and wild singularities is called the set of singularitiesof M and will be denoted by Sing(M).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 65: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide symmetries

Definition. A homeomorphism f : M → M which in flatcharts is an R-affine map is called an affine automorphism.Let Aff+(M) be the group of affine automorphisms of Mwhich preserve orientation.

The image of the derivative map:

D : Aff+(M)→ GL+2 (R)

is called the Veech group of M. We denoted it by Γ(M).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 66: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide symmetries

Definition. A homeomorphism f : M → M which in flatcharts is an R-affine map is called an affine automorphism.Let Aff+(M) be the group of affine automorphisms of Mwhich preserve orientation. The image of the derivative map:

D : Aff+(M)→ GL+2 (R)

is called the Veech group of M. We denoted it by Γ(M).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 67: Geometry and dynamics on infinite-type flat surfaces

Translation atlases provide dynamics

Definition. For each direction θ ∈ R/2πZ the vectorfield dz

zt = eiθ in C is translation invariant. The pull-backof this vector field through flat charts is well-defined onM \Sing(M) and the associated “flow” F t

θ is called the trans-lation/straightline/geodesic in direction θ.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 68: Geometry and dynamics on infinite-type flat surfaces

Veech’s dychotomy

Thm.(Veech ’89). Let M be a compact translation surfacesuch that Γ(M) is a lattice. Then F t

θ is either periodic* oruniquely ergodic.

A

A

B

B C

C

D

D

P

SP

P

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 69: Geometry and dynamics on infinite-type flat surfaces

Veech’s dychotomy

Thm.(Veech ’89). Let M be a compact translation surfacesuch that Γ(M) is a lattice. Then F t

θ is either periodic* oruniquely ergodic.

A

A

B

B C

C

D

D

P

SP

P

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 70: Geometry and dynamics on infinite-type flat surfaces

Three definitions:analytic

Definition. A translation surface is a pair (X , ω) formed by aRiemann surface X and a holomorphic 1–form ω on X whichis not identically zero.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 71: Geometry and dynamics on infinite-type flat surfaces

Infinite type

A translation surface M = (X , ω) is said to be of finite type ifX is of finite type* (as a Riemann surface) and M has finitearea. If M is not of finite type we say it is of infinite type.

A translation surface whose fundamental group is not finitely gen-erated is of infinite type. We will focus on this kind of infinite typesurfaces.

How do we classify them topologically?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 72: Geometry and dynamics on infinite-type flat surfaces

Infinite type

A translation surface M = (X , ω) is said to be of finite type ifX is of finite type* (as a Riemann surface) and M has finitearea. If M is not of finite type we say it is of infinite type.

A translation surface whose fundamental group is not finitely gen-erated is of infinite type. We will focus on this kind of infinite typesurfaces.

How do we classify them topologically?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 73: Geometry and dynamics on infinite-type flat surfaces

Ends of a topological space

Definition. Let U1 ⊇ U2 ⊇ . . . be an infinite sequence ofnon-empty connected open subsets of X such that for eachi ∈ N the boundary ∂Ui of Ui is compact and

⋂i∈N

Ui = ∅.

Two such sequences U1 ⊇ U2 ⊇ . . . and U ′1 ⊇ U ′

2 ⊇ . . . aresaid to be equivalent if for every i ∈ N there exist j suchthat Ui ⊇ U ′

j and viceversa. The corresponding equivalenceclasses are also called topological ends of X and we will de-note it by Ends(X ).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 74: Geometry and dynamics on infinite-type flat surfaces

Ends of a surface

An end [U1 ⊇ U2 ⊇ . . .] is called planar if there exists Ui of genuszero.

Definition.We define Ends∞(S) ⊂ Ends(S) as the set of allends which are not planar.

Thm.(Kerekjarto-Richards, ’63). Two non-compact ori-entable surfaces S and S ′ of the same genus are homeomor-phic if and only if they have the same genus g ∈ N∪{0,∞},and both Ends∞(S) ⊂ Ends(S) and Ends∞(S ′) ⊂ Ends(S ′)are homeomorphic as nested topological spaces, that is, thereexists a homeomorphism h : Ends(S)→ Ends(S)′ such thath(Ends∞(S)) = Ends∞(S ′)

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 75: Geometry and dynamics on infinite-type flat surfaces

Ends of a surface

Thm.(Kerekjarto-Richards’63). Two non-compact orientablesurfaces S and S ′ of the same genus are homeomorphic if andonly if Ends∞(S) ⊂ Ends(S) and Ends∞(S ′) ⊂ Ends(S ′)are homeomorphic as nested topological spaces, that is, thereexists a homeomorphism h : Ends(S)→ Ends(S)′ such thath(Ends∞(S)) = Ends∞(S ′)

Thm.(Kerekjarto-Richards’63). Let C ′ ⊂ C be a nested pairof closed subset of the Cantor set. Then there exist a surfaceS such that Ends∞(S) ⊂ Ends(S) is homeomorphic to C ′ ⊂C as nested pair of topological spaces.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 76: Geometry and dynamics on infinite-type flat surfaces

Affine symmetries and Veechgroups.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 77: Geometry and dynamics on infinite-type flat surfaces

Veech groups: compact case

Let M be a compact translation surface and Γ(M) its Veech group.Then:

1 Γ(M) is Fuchsian (but generically trivial).2 Γ(M) is never co-compact.

Open questions:1 Does there exist Γ(M) of the second kind?2 Does there exist Γ(M) cyclic and hyperbolic?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 78: Geometry and dynamics on infinite-type flat surfaces

Veech groups: compact case

Let M be a compact translation surface and Γ(M) its Veech group.Then:

1 Γ(M) is Fuchsian (but generically trivial).

2 Γ(M) is never co-compact.Open questions:

1 Does there exist Γ(M) of the second kind?2 Does there exist Γ(M) cyclic and hyperbolic?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 79: Geometry and dynamics on infinite-type flat surfaces

Veech groups: compact case

Let M be a compact translation surface and Γ(M) its Veech group.Then:

1 Γ(M) is Fuchsian (but generically trivial).2 Γ(M) is never co-compact.

Open questions:1 Does there exist Γ(M) of the second kind?2 Does there exist Γ(M) cyclic and hyperbolic?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 80: Geometry and dynamics on infinite-type flat surfaces

Veech groups: compact case

Let M be a compact translation surface and Γ(M) its Veech group.Then:

1 Γ(M) is Fuchsian (but generically trivial).2 Γ(M) is never co-compact.

Open questions:1 Does there exist Γ(M) of the second kind?2 Does there exist Γ(M) cyclic and hyperbolic?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 81: Geometry and dynamics on infinite-type flat surfaces

Veech groups: compact case

Let M be a compact translation surface and Γ(M) its Veech group.Then:

1 Γ(M) is Fuchsian (but generically trivial).2 Γ(M) is never co-compact.

Open questions:1 Does there exist Γ(M) of the second kind?2 Does there exist Γ(M) cyclic and hyperbolic?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 82: Geometry and dynamics on infinite-type flat surfaces

Veech groups and billiards

Thm. Let P be an irrational polygon whose interior anglesare λjπ, j = 1, . . . , n. Then the group of rotations z →e2πλj i z has finite index Γ(SP).

Question. Can any countable subgroup of GL+2 (R) be the

Veech group of an infinite type translation surface?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 83: Geometry and dynamics on infinite-type flat surfaces

Veech groups and billiards

Thm. Let P be an irrational polygon whose interior anglesare λjπ, j = 1, . . . , n. Then the group of rotations z →e2πλj i z has finite index Γ(SP).

Question. Can any countable subgroup of GL+2 (R) be the

Veech group of an infinite type translation surface?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 84: Geometry and dynamics on infinite-type flat surfaces

Veech groups of LNM

Thm.(Przytycki-Schmithusen-V.) Every countable subgroupG < GL+

2 (R) is the Veech group of a translation surface MGhomeomorphic to the Loch Ness monster.

RemarksThe translation surface MG has infinite area.The dynamic of the translation flow F t

θ in MG is uninteresting.The Veech group of the infinite staircase is a lattice and, as we willsee later, in this particular example we have an analog of Veech’sdychotomy.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 85: Geometry and dynamics on infinite-type flat surfaces

Veech groups of LNM

Thm.(Przytycki-Schmithusen-V.) Every countable subgroupG < GL+

2 (R) is the Veech group of a translation surface MGhomeomorphic to the Loch Ness monster.

RemarksThe translation surface MG has infinite area.The dynamic of the translation flow F t

θ in MG is uninteresting.

The Veech group of the infinite staircase is a lattice and, as we willsee later, in this particular example we have an analog of Veech’sdychotomy.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 86: Geometry and dynamics on infinite-type flat surfaces

Veech groups of LNM

Thm.(Przytycki-Schmithusen-V.) Every countable subgroupG < GL+

2 (R) is the Veech group of a translation surface MGhomeomorphic to the Loch Ness monster.

RemarksThe translation surface MG has infinite area.The dynamic of the translation flow F t

θ in MG is uninteresting.The Veech group of the infinite staircase is a lattice and, as we willsee later, in this particular example we have an analog of Veech’sdychotomy.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 87: Geometry and dynamics on infinite-type flat surfaces

Open questions

Question. Let C∞ ⊂ C be a nested couple of closed sub-spaces of the Cantor set and G any countable subgroup ofGL+

2 (R). Is it possible to find a translation surface M suchthat Ends∞(S) = C∞, Ends(S) = C and whose Veech groupis G?

Question. Does there exist a translation surface M homeo-morphic to Jacob’s ladder and whose Veech group is SL2(Z)?a lattice?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 88: Geometry and dynamics on infinite-type flat surfaces

Open questions

Question. Let C∞ ⊂ C be a nested couple of closed sub-spaces of the Cantor set and G any countable subgroup ofGL+

2 (R). Is it possible to find a translation surface M suchthat Ends∞(S) = C∞, Ends(S) = C and whose Veech groupis G?

Question. Does there exist a translation surface M homeo-morphic to Jacob’s ladder and whose Veech group is SL2(Z)?

a lattice?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 89: Geometry and dynamics on infinite-type flat surfaces

Open questions

Question. Let C∞ ⊂ C be a nested couple of closed sub-spaces of the Cantor set and G any countable subgroup ofGL+

2 (R). Is it possible to find a translation surface M suchthat Ends∞(S) = C∞, Ends(S) = C and whose Veech groupis G?

Question. Does there exist a translation surface M homeo-morphic to Jacob’s ladder and whose Veech group is SL2(Z)?a lattice?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 90: Geometry and dynamics on infinite-type flat surfaces

Veech groups in finite area

Thm.(Hooper,2015) Let M be a Thurston-Veech translationsurface constructed from a bipartite graph G and a positiveeigenfunction f with eigenvalue λ. Then the group Hλ gen-erated by the matrices(

1 λ0 1

) (1 0λ 1

)

is a subgroup of Γ(M).

Proposition. The Veech group of Baker’s surface is a non-elementary Fuchsian group of the second kind.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 91: Geometry and dynamics on infinite-type flat surfaces

Veech groups in finite area

Thm.(Hooper,2015) Let M be a Thurston-Veech translationsurface constructed from a bipartite graph G and a positiveeigenfunction f with eigenvalue λ. Then the group Hλ gen-erated by the matrices(

1 λ0 1

) (1 0λ 1

)

is a subgroup of Γ(M).

Proposition. The Veech group of Baker’s surface is a non-elementary Fuchsian group of the second kind.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Veech groups in finite area and dynamics

Thm.(Trevino,2013). Let M be a translation surface of in-finite genus and finite area whose Veech group is a lattice.Then for a.e. direction F t

θ is ergodic.

Question Does there exist an infinite type and finite areatranslation surface whose Veech group is SL2(Z)? a lattice?of the first kind?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 93: Geometry and dynamics on infinite-type flat surfaces

Veech groups in finite area and dynamics

Thm.(Trevino,2013). Let M be a translation surface of in-finite genus and finite area whose Veech group is a lattice.Then for a.e. direction F t

θ is ergodic.

Question Does there exist an infinite type and finite areatranslation surface whose Veech group is SL2(Z)? a lattice?of the first kind?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Dynamical properties of thetranslation flow (recurrence and

ergodicity).

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Z-covers

A (connected) cover π : M → M \Σ with deck transf. groupisomorphic to Z is called a Z-cover. These are determined bynon-primitive classes in H1(M,Σ;Z).

Every translation surface has a holonomy map:

hol : H1(M,Σ;Z)→ R2

It is defined by developing a representative of the class in theplane and then taking the difference of the starting and endpoints.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 96: Geometry and dynamics on infinite-type flat surfaces

Z-covers

A (connected) cover π : M → M \Σ with deck transf. groupisomorphic to Z is called a Z-cover. These are determined bynon-primitive classes in H1(M,Σ;Z).

Every translation surface has a holonomy map:

hol : H1(M,Σ;Z)→ R2

It is defined by developing a representative of the class in theplane and then taking the difference of the starting and endpoints.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Recurrence in Z-covers

Thm.(Hooper-Weiss.’12) Let M → M be a Z-cover definedby a class c ∈ H1(M,Σ;Z) such that hol(c) = 0. If θ is adirection for which F t

θ is ergodic, then F tθ is recurrent.

A classical theorem by Kerckhoff-Masur-Smillie implies:

Cor. Let M → M be a Z-cover defined by a class c ∈H1(M,Σ;Z) such that hol(c) = 0.Then F t

θ is recurrent fora.e. direction θ.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Recurrence in Z-covers

Thm.(Hooper-Weiss.’12) Let M → M be a Z-cover definedby a class c ∈ H1(M,Σ;Z) such that hol(c) = 0. If θ is adirection for which F t

θ is ergodic, then F tθ is recurrent.

A classical theorem by Kerckhoff-Masur-Smillie implies:

Cor. Let M → M be a Z-cover defined by a class c ∈H1(M,Σ;Z) such that hol(c) = 0.Then F t

θ is recurrent fora.e. direction θ.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 99: Geometry and dynamics on infinite-type flat surfaces

Skew-products over IET’s

Let T : I → I be a IET and f : I → Z a measurable function. Thedyn. system on I × Z defined by:

Tf (x , n) = (T (x), n + f (x))

is called a skew-product.

Thm.(Atkinson-Krygin) Suppose that f is integrable and T isergodic. If

∫I f dλ = 0 then the skew product Tf is recurrent.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 100: Geometry and dynamics on infinite-type flat surfaces

Recurrence in the staircase

γA

γA

γB

γB

γC

γC

A B C

C B A

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Recurrence in general Abelian coverings

Atkinson’s theorem cannot be generalized to skew products whosefiber is Zd , d ≥ 2.

However, Avila and Hubert developed a ge-ometric criterion that guarantees recurrence of certain Zd -covers(existence of tunneling curves).

Thm.(Avila-Hubert) Let Pa,b be a periodic wind-tree model.Then for a.e. direction θ the billiard flow on Pa,b is recurrent.

Question. Does there existe M → M a Zd -cover, d ≥2, defined by a cycle c ∈ H1(M,Σ;Zd ) such that M is asquare-tiled surface, Re(hol(c)) = 0 and the translation flowis dissipative in almost every direction?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 102: Geometry and dynamics on infinite-type flat surfaces

Recurrence in general Abelian coverings

Atkinson’s theorem cannot be generalized to skew products whosefiber is Zd , d ≥ 2. However, Avila and Hubert developed a ge-ometric criterion that guarantees recurrence of certain Zd -covers(existence of tunneling curves).

Thm.(Avila-Hubert) Let Pa,b be a periodic wind-tree model.Then for a.e. direction θ the billiard flow on Pa,b is recurrent.

Question. Does there existe M → M a Zd -cover, d ≥2, defined by a cycle c ∈ H1(M,Σ;Zd ) such that M is asquare-tiled surface, Re(hol(c)) = 0 and the translation flowis dissipative in almost every direction?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 103: Geometry and dynamics on infinite-type flat surfaces

Recurrence in general Abelian coverings

Atkinson’s theorem cannot be generalized to skew products whosefiber is Zd , d ≥ 2. However, Avila and Hubert developed a ge-ometric criterion that guarantees recurrence of certain Zd -covers(existence of tunneling curves).

Thm.(Avila-Hubert) Let Pa,b be a periodic wind-tree model.Then for a.e. direction θ the billiard flow on Pa,b is recurrent.

Question. Does there existe M → M a Zd -cover, d ≥2, defined by a cycle c ∈ H1(M,Σ;Zd ) such that M is asquare-tiled surface, Re(hol(c)) = 0 and the translation flowis dissipative in almost every direction?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 104: Geometry and dynamics on infinite-type flat surfaces

Recurrence in general Abelian coverings

Atkinson’s theorem cannot be generalized to skew products whosefiber is Zd , d ≥ 2. However, Avila and Hubert developed a ge-ometric criterion that guarantees recurrence of certain Zd -covers(existence of tunneling curves).

Thm.(Avila-Hubert) Let Pa,b be a periodic wind-tree model.Then for a.e. direction θ the billiard flow on Pa,b is recurrent.

Question. Does there existe M → M a Zd -cover, d ≥2, defined by a cycle c ∈ H1(M,Σ;Zd ) such that M is asquare-tiled surface, Re(hol(c)) = 0 and the translation flowis dissipative in almost every direction?

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 105: Geometry and dynamics on infinite-type flat surfaces

Ergodicity. Case study: the infinite staircase

Thm.(Hopper-Hubert-Weiss) Let F tθ be the translation flow

on the infinite staircase M.1 If θ = p

q with p or q EVEN, then F tθ decomposes M

into infinitely many cylinders,2 If θ = p

q with p and q ODD, then F tθ decomposes M

into two infinite strips, and3 If θ is irrational, then F t

θ is ergodic w.r.t. Lebesgue.

4 For every irrational direction θ, the locally finite Borelergodic measures for the flow in direction of slope θ areprecisely the Maharam measures.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 106: Geometry and dynamics on infinite-type flat surfaces

Ergodicity. Case study: the infinite staircase

Thm.(Hopper-Hubert-Weiss) Let F tθ be the translation flow

on the infinite staircase M.1 If θ = p

q with p or q EVEN, then F tθ decomposes M

into infinitely many cylinders,2 If θ = p

q with p and q ODD, then F tθ decomposes M

into two infinite strips, and3 If θ is irrational, then F t

θ is ergodic w.r.t. Lebesgue.4 For every irrational direction θ, the locally finite Borel

ergodic measures for the flow in direction of slope θ areprecisely the Maharam measures.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 107: Geometry and dynamics on infinite-type flat surfaces

Ergodicity: Z-covers

Thm.(Hubert-Weiss) Let M → M be a Z-cover for whichΓ(M) is a lattice and has an infinite strip. Then for a.e.direction θ, the flow F t

θ is ergodic.

Definition. Let Tf be a Z-valued skew-product over an IET.An element N ∈ Z is called an essential value if for everyA ⊂ I of positive measure, there exists n ∈ Z such thatT n

f (A× 1) ∩ A× N has positive measure.

Proposition. With the aforementioned hypothesis, if thereexist an essential value different from zero then Tf is ergodic.

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Page 108: Geometry and dynamics on infinite-type flat surfaces

Ergodicity: Z-covers

Thm.(Hubert-Weiss) Let M → M be a Z-cover for whichΓ(M) is a lattice and has an infinite strip. Then for a.e.direction θ, the flow F t

θ is ergodic.

Definition. Let Tf be a Z-valued skew-product over an IET.An element N ∈ Z is called an essential value if for everyA ⊂ I of positive measure, there exists n ∈ Z such thatT n

f (A× 1) ∩ A× N has positive measure.

Proposition. With the aforementioned hypothesis, if thereexist an essential value different from zero then Tf is ergodic.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 109: Geometry and dynamics on infinite-type flat surfaces

Ergodicity: Z-covers

Thm.(Hubert-Weiss) Let M → M be a Z-cover for whichΓ(M) is a lattice and has an infinite strip. Then for a.e.direction θ, the flow F t

θ is ergodic.

Definition. Let Tf be a Z-valued skew-product over an IET.An element N ∈ Z is called an essential value if for everyA ⊂ I of positive measure, there exists n ∈ Z such thatT n

f (A× 1) ∩ A× N has positive measure.

Proposition. With the aforementioned hypothesis, if thereexist an essential value different from zero then Tf is ergodic.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 110: Geometry and dynamics on infinite-type flat surfaces

Ergodicity: Z2-covers and beyond

Thm.(Fraczek-Ulcigrai) For all parameteres (a, b) and for a.e.direction θ the translation flow F t

θ on the periodic wind-treemodel is not ergodic.

Thm.(Malaga-Troubetzkoy) There are families ofnon-periodic wind-tree models for which for a.e. direc-tion θ the translation flow F t

θ is ergodic.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

Page 111: Geometry and dynamics on infinite-type flat surfaces

Ergodicity: Z2-covers and beyond

Thm.(Fraczek-Ulcigrai) For all parameteres (a, b) and for a.e.direction θ the translation flow F t

θ on the periodic wind-treemodel is not ergodic.

Thm.(Malaga-Troubetzkoy) There are families ofnon-periodic wind-tree models for which for a.e. direc-tion θ the translation flow F t

θ is ergodic.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .

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Ergodicity: Z2-covers and beyond

Thm.(Hooper) Let M be a Thurston-Veech surface con-structed from a bipartite infinite graph which has no verticesof valance one. Then for a “small” set of directions θ ∈ Θ itis possible to classify all locally finite ergodic invariant mea-sures.

Ferran Valdez Geometry and dynamics on infinite type flat surfaces .