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Helicoidal Surfaces in S2 × R(joint work with Brian White)
David Hoffman, Stanford University
Sevilla, 7 abril 2011
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
The helicoid, H, is a minimal surface in R3 with the followingproperties.
! H contains a vertical line (the Axis, which we will denote byZ );
! H is ruled by horizontal lines;
! H is invariant under the screw motion σκt,t for some nonzeroreal number κ.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
The helicoid, H, is a minimal surface in R3 with the followingproperties.
! H contains a vertical line (the Axis, which we will denote byZ );
! H is ruled by horizontal lines;
! H is invariant under the screw motion σκt,t for some nonzeroreal number κ.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
The helicoid, H, is a minimal surface in R3 with the followingproperties.
! H contains a vertical line (the Axis, which we will denote byZ );
! H is ruled by horizontal lines;
! H is invariant under the screw motion σκt,t for some nonzeroreal number κ.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
! For some fixed real number κ,H is invariant under the screw motion σκt,t
which is rotation around Z by an angle κt, followed byvertical translation by t.
! The pitch of H is twice the distance between successive sheetsand equals 2π/κ.
! Pitch =∞ when κ = 0, and the surface is a vertical plane! Pitch → 0 as κ→∞ and the limit is a lamination by
horizontal planes with curvature blowing up on Z .
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
! For some fixed real number κ,H is invariant under the screw motion σκt,t
which is rotation around Z by an angle κt, followed byvertical translation by t.
! The pitch of H is twice the distance between successive sheetsand equals 2π/κ.
! Pitch =∞ when κ = 0, and the surface is a vertical plane! Pitch → 0 as κ→∞ and the limit is a lamination by
horizontal planes with curvature blowing up on Z .
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
! For some fixed real number κ,H is invariant under the screw motion σκt,t
which is rotation around Z by an angle κt, followed byvertical translation by t.
! The pitch of H is twice the distance between successive sheetsand equals 2π/κ.
! Pitch =∞ when κ = 0, and the surface is a vertical plane! Pitch → 0 as κ→∞ and the limit is a lamination by
horizontal planes with curvature blowing up on Z .
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
! For some fixed real number κ,H is invariant under the screw motion σκt,t
which is rotation around Z by an angle κt, followed byvertical translation by t.
! The pitch of H is twice the distance between successive sheetsand equals 2π/κ.
! Pitch =∞ when κ = 0, and the surface is a vertical plane
! Pitch → 0 as κ→∞ and the limit is a lamination byhorizontal planes with curvature blowing up on Z .
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids in R3
! For some fixed real number κ,H is invariant under the screw motion σκt,t
which is rotation around Z by an angle κt, followed byvertical translation by t.
! The pitch of H is twice the distance between successive sheetsand equals 2π/κ.
! Pitch =∞ when κ = 0, and the surface is a vertical plane! Pitch → 0 as κ→∞ and the limit is a lamination by
horizontal planes with curvature blowing up on Z .David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids H in S2 × R
! Let X be a great circle in S2 × 0.
! Choose antipodal points O and O∗ on X , and letZ = O × RandZ ∗ = O∗ × R.Z and Z ∗ will be the axes of a helicoid
! Fix a value of κ.
H = Hκ =⋃
t∈R
σκt,t(X )
where σκt,t is rotation by κt followed by vertical translationby t
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids H in S2 × R
! Let X be a great circle in S2 × 0.! Choose antipodal points O and O∗ on X , and let
Z = O × RandZ ∗ = O∗ × R.
Z and Z ∗ will be the axes of a helicoid
! Fix a value of κ.
H = Hκ =⋃
t∈R
σκt,t(X )
where σκt,t is rotation by κt followed by vertical translationby t
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids H in S2 × R
! Let X be a great circle in S2 × 0.! Choose antipodal points O and O∗ on X , and let
Z = O × RandZ ∗ = O∗ × R.Z and Z ∗ will be the axes of a helicoid
! Fix a value of κ.
H = Hκ =⋃
t∈R
σκt,t(X )
where σκt,t is rotation by κt followed by vertical translationby t
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoids H in S2 × R
! Let X be a great circle in S2 × 0.! Choose antipodal points O and O∗ on X , and let
Z = O × RandZ ∗ = O∗ × R.Z and Z ∗ will be the axes of a helicoid
! Fix a value of κ.
H = Hκ =⋃
t∈R
σκt,t(X )
where σκt,t is rotation by κt followed by vertical translationby t
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properties of Helicoids H in S2 × R
! They are properly embedded annuli
! They are minimal surfaces
! Helicoids with different pitch (i.e. different values of |κ|) arenot homothetically related as in R3. (There are nohomotheties in S2 × R.)
! When κ = 0 we get a flat cylinder X × R
! As κ→∞ we get a lamination of S2 × R by level spheresS2 × t with curvature blowing up on the axes Z ∪ Z ∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properties of Helicoids H in S2 × R
! They are properly embedded annuli
! They are minimal surfaces
! Helicoids with different pitch (i.e. different values of |κ|) arenot homothetically related as in R3. (There are nohomotheties in S2 × R.)
! When κ = 0 we get a flat cylinder X × R
! As κ→∞ we get a lamination of S2 × R by level spheresS2 × t with curvature blowing up on the axes Z ∪ Z ∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properties of Helicoids H in S2 × R
! They are properly embedded annuli
! They are minimal surfaces
! Helicoids with different pitch (i.e. different values of |κ|) arenot homothetically related as in R3. (There are nohomotheties in S2 × R.)
! When κ = 0 we get a flat cylinder X × R
! As κ→∞ we get a lamination of S2 × R by level spheresS2 × t with curvature blowing up on the axes Z ∪ Z ∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properties of Helicoids H in S2 × R
! They are properly embedded annuli
! They are minimal surfaces
! Helicoids with different pitch (i.e. different values of |κ|) arenot homothetically related as in R3. (There are nohomotheties in S2 × R.)
! When κ = 0 we get a flat cylinder X × R
! As κ→∞ we get a lamination of S2 × R by level spheresS2 × t with curvature blowing up on the axes Z ∪ Z ∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properties of Helicoids H in S2 × R
! They are properly embedded annuli
! They are minimal surfaces
! Helicoids with different pitch (i.e. different values of |κ|) arenot homothetically related as in R3. (There are nohomotheties in S2 × R.)
! When κ = 0 we get a flat cylinder X × R
! As κ→∞ we get a lamination of S2 × R by level spheresS2 × t with curvature blowing up on the axes Z ∪ Z ∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
More Properties of Helicoids H in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c! Let Y be the great circle in S2 × O that passes through thepoints O and O∗ and is orthogonal to X .
180-rotation about Y is an isometry of H.
! This symmetry is referred to as a normal symmetry.
! H has the symmetry of reflection through a vertical cylinderC × 0, This symmetry does not exist in the Euclideansetting.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
More Properties of Helicoids H in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c! Let Y be the great circle in S2 × O that passes through thepoints O and O∗ and is orthogonal to X .
180-rotation about Y is an isometry of H.
! This symmetry is referred to as a normal symmetry.
! H has the symmetry of reflection through a vertical cylinderC × 0, This symmetry does not exist in the Euclideansetting.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
More Properties of Helicoids H in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c! Let Y be the great circle in S2 × O that passes through thepoints O and O∗ and is orthogonal to X .
180-rotation about Y is an isometry of H.
! This symmetry is referred to as a normal symmetry.
! H has the symmetry of reflection through a vertical cylinderC × 0, This symmetry does not exist in the Euclideansetting.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Let M be a properly embedded minimal surface with finitetopology in S2 × R.
! If M is compact, then M = S2 × t.! (Rosenberg) All noncompact M have two ends, both annular,
one diverging upwards, the other downwards.
! (Meeks-Rosenberg) The Gauss curvature of M is bounded.
! (Hauswirth) Suppose E is an annulus (genus=0) fibred byhorizontal circles. Then E belongs to a two-parameter familyof examples on the boundary of which reside the helicoids. Itcontains examples constructed by Ritore and Pedrosa.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Let M be a properly embedded minimal surface with finitetopology in S2 × R.
! If M is compact, then M = S2 × t.
! (Rosenberg) All noncompact M have two ends, both annular,one diverging upwards, the other downwards.
! (Meeks-Rosenberg) The Gauss curvature of M is bounded.
! (Hauswirth) Suppose E is an annulus (genus=0) fibred byhorizontal circles. Then E belongs to a two-parameter familyof examples on the boundary of which reside the helicoids. Itcontains examples constructed by Ritore and Pedrosa.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Let M be a properly embedded minimal surface with finitetopology in S2 × R.
! If M is compact, then M = S2 × t.! (Rosenberg) All noncompact M have two ends, both annular,
one diverging upwards, the other downwards.
! (Meeks-Rosenberg) The Gauss curvature of M is bounded.
! (Hauswirth) Suppose E is an annulus (genus=0) fibred byhorizontal circles. Then E belongs to a two-parameter familyof examples on the boundary of which reside the helicoids. Itcontains examples constructed by Ritore and Pedrosa.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Let M be a properly embedded minimal surface with finitetopology in S2 × R.
! If M is compact, then M = S2 × t.! (Rosenberg) All noncompact M have two ends, both annular,
one diverging upwards, the other downwards.
! (Meeks-Rosenberg) The Gauss curvature of M is bounded.
! (Hauswirth) Suppose E is an annulus (genus=0) fibred byhorizontal circles. Then E belongs to a two-parameter familyof examples on the boundary of which reside the helicoids. Itcontains examples constructed by Ritore and Pedrosa.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Let M be a properly embedded minimal surface with finitetopology in S2 × R.
! If M is compact, then M = S2 × t.! (Rosenberg) All noncompact M have two ends, both annular,
one diverging upwards, the other downwards.
! (Meeks-Rosenberg) The Gauss curvature of M is bounded.
! (Hauswirth) Suppose E is an annulus (genus=0) fibred byhorizontal circles. Then E belongs to a two-parameter familyof examples on the boundary of which reside the helicoids. Itcontains examples constructed by Ritore and Pedrosa.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Theorem. (Hauswirth) Suppose E is an annulus (genus=0) fibredby horizontal circles. Then E belongs to a two-parameter family ofexamples on the boundary of which reside the helicoids.
QUESTION
! Is it true that each end of M asymptotic to one of theseannuli?
ANSWER (partial)
(H—,White) If M contains a vertical line, then the answer is ”Yes.”
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Theorem. (Hauswirth) Suppose E is an annulus (genus=0) fibredby horizontal circles. Then E belongs to a two-parameter family ofexamples on the boundary of which reside the helicoids.
QUESTION
! Is it true that each end of M asymptotic to one of theseannuli?
ANSWER (partial)
(H—,White) If M contains a vertical line, then the answer is ”Yes.”
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Theorem. (Hauswirth) Suppose E is an annulus (genus=0) fibredby horizontal circles. Then E belongs to a two-parameter family ofexamples on the boundary of which reside the helicoids.
QUESTION
! Is it true that each end of M asymptotic to one of theseannuli?
ANSWER (partial)
(H—,White) If M contains a vertical line, then the answer is ”Yes.”
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Theorem. (Hauswirth) Suppose E is an annulus (genus=0) fibredby horizontal circles. Then E belongs to a two-parameter family ofexamples on the boundary of which reside the helicoids.
QUESTION
! Is it true that each end of M asymptotic to one of theseannuli?
ANSWER (partial)
(H—,White) If M contains a vertical line, then the answer is ”Yes.”
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces in S2 × Rwith finite topology
Theorem. (Hauswirth) Suppose E is an annulus (genus=0) fibredby horizontal circles. Then E belongs to a two-parameter family ofexamples on the boundary of which reside the helicoids.
QUESTION
! Is it true that each end of M asymptotic to one of theseannuli?
ANSWER (partial)
(H—,White) If M contains a vertical line, then the answer is ”Yes.”
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Properly embedded minimal surfaces of finite topology inS2 × R of higher genus
Let κ and g ≥ 1 be given. Let µ be reflection in the verticalcylinder C × R.
Theorem (—–,White)
There exists a pair of properly embedded, genus = g, embeddedaxial minimal surfaces, M+1,M−1, each of whose ends isasymptotic to a helicoid with pitch 2π/κ.
If g is odd, µ(M+1) = M−1.
If g is even, µ(M+1) = M+1 and µ(M−1) = M+1, but M+1,M−1
are not congruent.
*Recent result of Pacard & Rosenberg: STATE IT
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Definition. A properly embedded minimal surface of finite topologyis Axial provided it contains a vertical line.
Axial Minimal Surfaces.
Theorem (H—,White) Suppose M is an axial minimal surface
i) If E is an annular end of M, then E is asymptotic to a helicoid.
ii.) If M is an annulus, then M is a helicoid
iii.) The annular ends of M are both asymptotic to helicoids withthe same pitch. (However, the two ends may not be ends of thesame helicoid Hκ.)
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Definition. A properly embedded minimal surface of finite topologyis Axial provided it contains a vertical line.
Axial Minimal Surfaces.
Theorem (H—,White) Suppose M is an axial minimal surface
i) If E is an annular end of M, then E is asymptotic to a helicoid.
ii.) If M is an annulus, then M is a helicoid
iii.) The annular ends of M are both asymptotic to helicoids withthe same pitch. (However, the two ends may not be ends of thesame helicoid Hκ.)
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Definition. A properly embedded minimal surface of finite topologyis Axial provided it contains a vertical line.
Axial Minimal Surfaces.
Theorem (H—,White) Suppose M is an axial minimal surface
i) If E is an annular end of M, then E is asymptotic to a helicoid.
ii.) If M is an annulus, then M is a helicoid
iii.) The annular ends of M are both asymptotic to helicoids withthe same pitch. (However, the two ends may not be ends of thesame helicoid Hκ.)
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Definition. A properly embedded minimal surface of finite topologyis Axial provided it contains a vertical line.
Axial Minimal Surfaces.
Theorem (H—,White) Suppose M is an axial minimal surface
i) If E is an annular end of M, then E is asymptotic to a helicoid.
ii.) If M is an annulus, then M is a helicoid
iii.) The annular ends of M are both asymptotic to helicoids withthe same pitch. (However, the two ends may not be ends of thesame helicoid Hκ.)
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Definition. A properly embedded minimal surface of finite topologyis Axial provided it contains a vertical line.
Axial Minimal Surfaces.
Theorem (H—,White) Suppose M is an axial minimal surface
i) If E is an annular end of M, then E is asymptotic to a helicoid.
ii.) If M is an annulus, then M is a helicoid
iii.) The annular ends of M are both asymptotic to helicoids withthe same pitch. (However, the two ends may not be ends of thesame helicoid Hκ.)
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Proposition. An axial minimal surface M contains two verticallines.
Proof. S2 × R \M consists of two components, M+, and M−.Suppose Z = O× R is contained in M. Define
Z ∗ = O′× R.
We claim that Z ∗ ⊂ M. Define
ρZ = rotation by π around Z .
The isometry ρZ fixes both Z and Z ∗. It also interchanges M+
and M−.Hence no point of M+ ∪M− can be on Z ∗.Therefore Z ∗ ⊂ M.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Proposition. An axial minimal surface M contains two verticallines.Proof. S2 × R \M consists of two components, M+, and M−.
Suppose Z = O× R is contained in M. Define
Z ∗ = O′× R.
We claim that Z ∗ ⊂ M. Define
ρZ = rotation by π around Z .
The isometry ρZ fixes both Z and Z ∗. It also interchanges M+
and M−.Hence no point of M+ ∪M− can be on Z ∗.Therefore Z ∗ ⊂ M.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Proposition. An axial minimal surface M contains two verticallines.Proof. S2 × R \M consists of two components, M+, and M−.Suppose Z = O× R is contained in M. Define
Z ∗ = O′× R.
We claim that Z ∗ ⊂ M. Define
ρZ = rotation by π around Z .
The isometry ρZ fixes both Z and Z ∗. It also interchanges M+
and M−.Hence no point of M+ ∪M− can be on Z ∗.Therefore Z ∗ ⊂ M.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Proposition. An axial minimal surface M contains two verticallines.Proof. S2 × R \M consists of two components, M+, and M−.Suppose Z = O× R is contained in M. Define
Z ∗ = O′× R.
We claim that Z ∗ ⊂ M. Define
ρZ = rotation by π around Z .
The isometry ρZ fixes both Z and Z ∗. It also interchanges M+
and M−.Hence no point of M+ ∪M− can be on Z ∗.Therefore Z ∗ ⊂ M.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Proposition. An axial minimal surface M contains two verticallines.Proof. S2 × R \M consists of two components, M+, and M−.Suppose Z = O× R is contained in M. Define
Z ∗ = O′× R.
We claim that Z ∗ ⊂ M. Define
ρZ = rotation by π around Z .
The isometry ρZ fixes both Z and Z ∗. It also interchanges M+
and M−.
Hence no point of M+ ∪M− can be on Z ∗.Therefore Z ∗ ⊂ M.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial minimal surfaces in S2 × R are helicoidal
Proposition. An axial minimal surface M contains two verticallines.Proof. S2 × R \M consists of two components, M+, and M−.Suppose Z = O× R is contained in M. Define
Z ∗ = O′× R.
We claim that Z ∗ ⊂ M. Define
ρZ = rotation by π around Z .
The isometry ρZ fixes both Z and Z ∗. It also interchanges M+
and M−.Hence no point of M+ ∪M− can be on Z ∗.Therefore Z ∗ ⊂ M.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
The angle function θ on S2 × R \ (Z ∪ Z ∗)
OnS2 × 0 \ O,O∗,
define θ by first identifying S2 × 0 \ O,O∗ with the complexplane via stereographic projection from O∗ , and then choosing θon this sphere to be the angle function in the plane.Extend θ to
S2 × R \ (Z ∪ Z ∗)
by vertical translation.
The function θ is defined up to an additive multiple of 2π
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
The angle function θ on S2 × R \ (Z ∪ Z ∗)
OnS2 × 0 \ O,O∗,
define θ by first identifying S2 × 0 \ O,O∗ with the complexplane via stereographic projection from O∗ , and then choosing θon this sphere to be the angle function in the plane.Extend θ to
S2 × R \ (Z ∪ Z ∗)
by vertical translation.
The function θ is defined up to an additive multiple of 2π
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: a single-valued angle function
Let I ⊂ R be a closed interval (possibly infinite).
Suppose that
E = M ∩ (S2 × I )
is an annulus. ThenE \ (Z ∪ Z ∗)
is the union of two simply connected domains congruent under theinvolution ρZ . Let D be one of them.
The function θ has a single-valued branch that is well defined on D.This θ extends continuously to D.
DEFINE
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: a single-valued angle function
Let I ⊂ R be a closed interval (possibly infinite).Suppose that
E = M ∩ (S2 × I )
is an annulus.
ThenE \ (Z ∪ Z ∗)
is the union of two simply connected domains congruent under theinvolution ρZ . Let D be one of them.
The function θ has a single-valued branch that is well defined on D.This θ extends continuously to D.
DEFINE
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: a single-valued angle function
Let I ⊂ R be a closed interval (possibly infinite).Suppose that
E = M ∩ (S2 × I )
is an annulus. ThenE \ (Z ∪ Z ∗)
is the union of two simply connected domains congruent under theinvolution ρZ .
Let D be one of them.
The function θ has a single-valued branch that is well defined on D.This θ extends continuously to D.
DEFINE
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: a single-valued angle function
Let I ⊂ R be a closed interval (possibly infinite).Suppose that
E = M ∩ (S2 × I )
is an annulus. ThenE \ (Z ∪ Z ∗)
is the union of two simply connected domains congruent under theinvolution ρZ . Let D be one of them.
The function θ has a single-valued branch that is well defined on D.
This θ extends continuously to D.
DEFINE
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: a single-valued angle function
Let I ⊂ R be a closed interval (possibly infinite).Suppose that
E = M ∩ (S2 × I )
is an annulus. ThenE \ (Z ∪ Z ∗)
is the union of two simply connected domains congruent under theinvolution ρZ . Let D be one of them.
The function θ has a single-valued branch that is well defined on D.This θ extends continuously to D.
DEFINE
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: a single-valued angle function
Let I ⊂ R be a closed interval (possibly infinite).Suppose that
E = M ∩ (S2 × I )
is an annulus. ThenE \ (Z ∪ Z ∗)
is the union of two simply connected domains congruent under theinvolution ρZ . Let D be one of them.
The function θ has a single-valued branch that is well defined on D.This θ extends continuously to D.
DEFINE
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,
β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
Observe that for a fixed value of t,
α(t) = β(t) ⇐⇒ D ∩ (S2 × t) is a great semicircle.
Observe that E is a part of a helicoid if and only if
α(t) ≡ β(t) ≡ κt + b,
for some real constants κ and b.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Axial Minimal surfaces: the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t,
β(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
φ(t) = α(t)− β(t).
Observe that for a fixed value of t,
α(t) = β(t) ⇐⇒ D ∩ (S2 × t) is a great semicircle.
Observe that E is a part of a helicoid if and only if
α(t) ≡ β(t) ≡ κt + b,
for some real constants κ and b.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity Lemma for the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tβ(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
————————–
Lemma. i.) α(t) and −β(t) are both strictly convex functionsunless D is part of a half-helicoid (in which case they are linear).
ii.)φ(t) = α(t)− β(t) is either strictly convex or D is part of ahalf-helicoid, in which case φ(t) ≡ 0.
Proof. We prove this for α(t). The same proof works for −β(t).φ(t) is the sum of convex functions, and so is strictly convex if oneof the functions is strictly convex. If they are not both strictlyconvex, then D lies on a half-helicoid and therefore
φ(t) ≡ 0.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity Lemma for the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tβ(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
————————–
Lemma. i.) α(t) and −β(t) are both strictly convex functionsunless D is part of a half-helicoid (in which case they are linear).
ii.)φ(t) = α(t)− β(t) is either strictly convex or D is part of ahalf-helicoid, in which case φ(t) ≡ 0.
Proof. We prove this for α(t). The same proof works for −β(t).φ(t) is the sum of convex functions, and so is strictly convex if oneof the functions is strictly convex. If they are not both strictlyconvex, then D lies on a half-helicoid and therefore
φ(t) ≡ 0.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity Lemma for the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tβ(t) = minθ(p, t) : (p, t) ∈ D ∩ S2 × t,
————————–
Lemma. i.) α(t) and −β(t) are both strictly convex functionsunless D is part of a half-helicoid (in which case they are linear).
ii.)φ(t) = α(t)− β(t) is either strictly convex or D is part of ahalf-helicoid, in which case φ(t) ≡ 0.
Proof. We prove this for α(t). The same proof works for −β(t).φ(t) is the sum of convex functions, and so is strictly convex if oneof the functions is strictly convex. If they are not both strictlyconvex, then D lies on a half-helicoid and therefore
φ(t) ≡ 0.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity Lemma for the the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × t
————————–
If α(t) is not strictly convex, there exists values t1 < t2, such thatfor some value t1 ≤ t3 ≤ t2,
α(t3) ≥ κ(t3 − t1) + α(t1),
where κ is the slope of the line connecting (t1,α(t1)) to(t2,α(t2)). It follows that there is a parallel line of the form
y = κt + b,
that touches the graph at a point (t∗,α(t∗)) for some t∗ ∈ (t1, t2)and is above the graph of α(t) over some interval (t∗ − ε, t∗ + ε).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity of the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tIt follows that there is a parallel line of the form
y = κt + b,
that touches the graph at a point (t∗,α(t∗)) for some t∗ ∈ (t1, t2)and is above the graph of α(t) over some interval (t∗ − ε, t∗ + ε).
————————–
Let (p∗, t∗) ∈ S2 × t∗ be the point where θ(p∗, t∗) = α(t∗).It follows from the definition of α(t) that in some neighborhood of(p∗, t∗) in D, the half-helicoid
H represented by y = κt + b
lies on one side of D and touches D at (p∗, t∗), the point whereθ(p∗, t∗) = α(t∗). By the maximum principle (or the boundarymaximum principle) D ⊂ H.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity of the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tIt follows that there is a parallel line of the form
y = κt + b,
that touches the graph at a point (t∗,α(t∗)) for some t∗ ∈ (t1, t2)and is above the graph of α(t) over some interval (t∗ − ε, t∗ + ε).
————————–
Let (p∗, t∗) ∈ S2 × t∗ be the point where θ(p∗, t∗) = α(t∗).
It follows from the definition of α(t) that in some neighborhood of(p∗, t∗) in D, the half-helicoid
H represented by y = κt + b
lies on one side of D and touches D at (p∗, t∗), the point whereθ(p∗, t∗) = α(t∗). By the maximum principle (or the boundarymaximum principle) D ⊂ H.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity of the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tIt follows that there is a parallel line of the form
y = κt + b,
that touches the graph at a point (t∗,α(t∗)) for some t∗ ∈ (t1, t2)and is above the graph of α(t) over some interval (t∗ − ε, t∗ + ε).
————————–
Let (p∗, t∗) ∈ S2 × t∗ be the point where θ(p∗, t∗) = α(t∗).It follows from the definition of α(t) that in some neighborhood of(p∗, t∗) in D, the half-helicoid
H represented by y = κt + b
lies on one side of D and touches D at (p∗, t∗), the point whereθ(p∗, t∗) = α(t∗).
By the maximum principle (or the boundarymaximum principle) D ⊂ H.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Convexity of the angle functions
α(t) = maxθ(p, t) : (p, t) ∈ D ∩ S2 × tIt follows that there is a parallel line of the form
y = κt + b,
that touches the graph at a point (t∗,α(t∗)) for some t∗ ∈ (t1, t2)and is above the graph of α(t) over some interval (t∗ − ε, t∗ + ε).
————————–
Let (p∗, t∗) ∈ S2 × t∗ be the point where θ(p∗, t∗) = α(t∗).It follows from the definition of α(t) that in some neighborhood of(p∗, t∗) in D, the half-helicoid
H represented by y = κt + b
lies on one side of D and touches D at (p∗, t∗), the point whereθ(p∗, t∗) = α(t∗). By the maximum principle (or the boundarymaximum principle) D ⊂ H.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem
i) If E is an annular end of M, then E is asymptotic to a helicoid.
Assume E ⊂ S2 × [a,∞). As usual let D be one of the simplyconnected regions defined by removing the axes from E . Define
c = lim supt→∞
φ(t).
Let tn be a diverging sequence with c = limn→∞ φ(tn).
Pull down E and D by a translation of −tn to produce En and Dn.We get subsequential convergence
En → E Dn → D with φ(t + tn) =: φn(t)→ φ(t).
where φn(t) and φ(t) are the angle-difference functions associatedwith Dn and D.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem
i) If E is an annular end of M, then E is asymptotic to a helicoid.Assume E ⊂ S2 × [a,∞). As usual let D be one of the simplyconnected regions defined by removing the axes from E .
Define
c = lim supt→∞
φ(t).
Let tn be a diverging sequence with c = limn→∞ φ(tn).
Pull down E and D by a translation of −tn to produce En and Dn.We get subsequential convergence
En → E Dn → D with φ(t + tn) =: φn(t)→ φ(t).
where φn(t) and φ(t) are the angle-difference functions associatedwith Dn and D.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem
i) If E is an annular end of M, then E is asymptotic to a helicoid.Assume E ⊂ S2 × [a,∞). As usual let D be one of the simplyconnected regions defined by removing the axes from E . Define
c = lim supt→∞
φ(t).
Let tn be a diverging sequence with c = limn→∞ φ(tn).
Pull down E and D by a translation of −tn to produce En and Dn.We get subsequential convergence
En → E Dn → D with φ(t + tn) =: φn(t)→ φ(t).
where φn(t) and φ(t) are the angle-difference functions associatedwith Dn and D.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem
i) If E is an annular end of M, then E is asymptotic to a helicoid.Assume E ⊂ S2 × [a,∞). As usual let D be one of the simplyconnected regions defined by removing the axes from E . Define
c = lim supt→∞
φ(t).
Let tn be a diverging sequence with c = limn→∞ φ(tn).
Pull down E and D by a translation of −tn to produce En and Dn.We get subsequential convergence
En → E Dn → D with φ(t + tn) =: φn(t)→ φ(t).
where φn(t) and φ(t) are the angle-difference functions associatedwith Dn and D.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem continued
i) If E is an annular end of M, then E is asymptotic to a helicoid.
c = lim supt→∞
φ(t) ≥ limn→∞
φ(t + tn) =: limn→∞
φn(t)→ φ(t),
where φn(t) and φ(t) are the angle-difference functions associatedwith Dn and D. The equality above implies: φ(0) = c . Apply the
lemma to D, noticing that since 0 ≤ φ(t) ≤ c , we must haveφ ≡ 0. In particular,
c = 0.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem concluded
i) If E is an annular end of M, then E is asymptotic to a helicoid.
c = lim supt→∞
φ(t) = 0
Let A+ be the open region in the plane above the graph of α.Let B− be the open region in the plane below the graph of β.These are disjoint convex regions and therefore can be separatedby a line
y = κt + b.
Since α(t)− β(t)→ c = 0 as t →∞, the graphs of α and β areasymptotic to the line y = κt + b.
Therefore, D is C 0-asymptotic to the half-helicoid given byθ = κt + b.Because D has bounded curvature, it is smoothly asymptotic tothis helicoid.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem concluded
i) If E is an annular end of M, then E is asymptotic to a helicoid.
c = lim supt→∞
φ(t) = 0
Let A+ be the open region in the plane above the graph of α.Let B− be the open region in the plane below the graph of β.These are disjoint convex regions and therefore can be separatedby a line
y = κt + b.
Since α(t)− β(t)→ c = 0 as t →∞, the graphs of α and β areasymptotic to the line y = κt + b.Therefore, D is C 0-asymptotic to the half-helicoid given byθ = κt + b.
Because D has bounded curvature, it is smoothly asymptotic tothis helicoid.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the first statment of the theorem concluded
i) If E is an annular end of M, then E is asymptotic to a helicoid.
c = lim supt→∞
φ(t) = 0
Let A+ be the open region in the plane above the graph of α.Let B− be the open region in the plane below the graph of β.These are disjoint convex regions and therefore can be separatedby a line
y = κt + b.
Since α(t)− β(t)→ c = 0 as t →∞, the graphs of α and β areasymptotic to the line y = κt + b.Therefore, D is C 0-asymptotic to the half-helicoid given byθ = κt + b.Because D has bounded curvature, it is smoothly asymptotic tothis helicoid.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the second statment of the theorem
ii) If M is an annulus, then M is a helicoid.Let D be one of the simply connected components M \ (Z ∪ Z ∗)The angle-difference function φ is defined on all of R and isnonnegative.By the Lemma, either φ is strictly convex, D must lie on ahalf-helicoid. Apply the first statement of the theorem to concludethat
limt→±∞
φ(t) = 0.
Hence φ cannot be strictly convex, so D is a half-helicoid, and
M = D ∪ ρz(D)
is a helicoid.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Proof of the third statment of the theorem
ii) The helicoids to which the two ends of M are asymptotic differby a rotationLet ∂/∂θ be the Killiing field of rotation around Z ∪ Z ∗.Let Ma = M ∩ (S2 × a). The ROTATIONAL FLUX of M
∫
Ma
< ∂/∂θ, ν > ds,
where ν is the outward-pointing normal to M ∩ (S2 × t ≤ a), isindependent of a.The helicoids asymptotic to the top and bottom ends of M, havethe same rotational flux (equal to the rotational flux of M).
Two helicoids θ = κ1 + b1(mod π) and θ = κ2 + b2(mod π) havethe same rotational flux if and only if κ1 = κ2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
The vertical flux of a helicoid is determined by itspitch=2π/κ
Two helicoids θ = κ1 + b1(mod π) and θ = κ2 + b2(mod π) havethe same rotational flux if and only if κ1 = κ2.The vertical flux of the helicoid H given by θ = κt + b (mod π) is
∫
C< ∂/∂θ, ν > ds,
where C is great circle H ∩ (S2 × 0)∂/∂θ is tangent to S2 × 0 (and orthogonal to C ).At each point of C \ O,O∗ the angle that the ν makes withS2 × 0 is a monotonic increasing function of the|pitch| = 2π/|κ|. Hence the integrand is a monotonic decreasingfunction of the absolute value of the pitch. The vertical fluxes ofhelicoids with different values κ are different.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why do we use rotational flux and not vertical flux?
Why Rotational Flux and not Vertical Flux∫
Ma
< ∂/∂t, ν > ds ?
The vertical flux will not distinguish between helicoids Hκ and H−κ.The rotational flux does make that distinction.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why do we use rotational flux and not vertical flux?
Why Rotational Flux and not Vertical Flux∫
Ma
< ∂/∂t, ν > ds ?
The vertical flux will not distinguish between helicoids Hκ and H−κ.The rotational flux does make that distinction.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why aren’t the two ends of M asymptotic to the samehelicoid?
We are not claiming that the helicoids asymptotic to the ends ofM differ by a rotation.
After all this is not true if M is a helicoid!However there is good reason to believe that in general they dodiffer by a rotation.A rotation by γ is equivalent to a vertical translation by b = γ/κ.The examples of higher genus we mentioned at the beginning ofthe lecture (and will discuss soon) can be thought of asdesingularizing the intersection of S2 × 0 and a helicoid H. .Such desingularization might well cause a vertical separation of thetop and bottom of ends of H in order to “make room” for handles.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why aren’t the two ends of M asymptotic to the samehelicoid?
We are not claiming that the helicoids asymptotic to the ends ofM differ by a rotation. After all this is not true if M is a helicoid!
However there is good reason to believe that in general they dodiffer by a rotation.A rotation by γ is equivalent to a vertical translation by b = γ/κ.The examples of higher genus we mentioned at the beginning ofthe lecture (and will discuss soon) can be thought of asdesingularizing the intersection of S2 × 0 and a helicoid H. .Such desingularization might well cause a vertical separation of thetop and bottom of ends of H in order to “make room” for handles.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why aren’t the two ends of M asymptotic to the samehelicoid?
We are not claiming that the helicoids asymptotic to the ends ofM differ by a rotation. After all this is not true if M is a helicoid!However there is good reason to believe that in general they dodiffer by a rotation.A rotation by γ is equivalent to a vertical translation by b = γ/κ.
The examples of higher genus we mentioned at the beginning ofthe lecture (and will discuss soon) can be thought of asdesingularizing the intersection of S2 × 0 and a helicoid H. .Such desingularization might well cause a vertical separation of thetop and bottom of ends of H in order to “make room” for handles.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why aren’t the two ends of M asymptotic to the samehelicoid?
We are not claiming that the helicoids asymptotic to the ends ofM differ by a rotation. After all this is not true if M is a helicoid!However there is good reason to believe that in general they dodiffer by a rotation.A rotation by γ is equivalent to a vertical translation by b = γ/κ.The examples of higher genus we mentioned at the beginning ofthe lecture (and will discuss soon) can be thought of asdesingularizing the intersection of S2 × 0 and a helicoid H.
.Such desingularization might well cause a vertical separation of thetop and bottom of ends of H in order to “make room” for handles.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why aren’t the two ends of M asymptotic to the samehelicoid?
We are not claiming that the helicoids asymptotic to the ends ofM differ by a rotation. After all this is not true if M is a helicoid!However there is good reason to believe that in general they dodiffer by a rotation.A rotation by γ is equivalent to a vertical translation by b = γ/κ.The examples of higher genus we mentioned at the beginning ofthe lecture (and will discuss soon) can be thought of asdesingularizing the intersection of S2 × 0 and a helicoid H. .Such desingularization might well cause a vertical separation of thetop and bottom of ends of H in order to “make room” for handles.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoidal minimal surfaces in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c
THECONSRUCTION PROCEDURE
! Y -Surfaces: Symmetry
! Helicoidal Barrier: A Y -symmetric, mean-convex region
! Double the surface by rotating about the axes
! Degree Theory with symmetries.
! Curvature Estimates in order to get limit surface.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoidal minimal surfaces in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c
THECONSRUCTION PROCEDURE
! Y -Surfaces: Symmetry
! Helicoidal Barrier: A Y -symmetric, mean-convex region
! Double the surface by rotating about the axes
! Degree Theory with symmetries.
! Curvature Estimates in order to get limit surface.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoidal minimal surfaces in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c
THECONSRUCTION PROCEDURE
! Y -Surfaces: Symmetry
! Helicoidal Barrier: A Y -symmetric, mean-convex region
! Double the surface by rotating about the axes
! Degree Theory with symmetries.
! Curvature Estimates in order to get limit surface.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoidal minimal surfaces in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c
THECONSRUCTION PROCEDURE
! Y -Surfaces: Symmetry
! Helicoidal Barrier: A Y -symmetric, mean-convex region
! Double the surface by rotating about the axes
! Degree Theory with symmetries.
! Curvature Estimates in order to get limit surface.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoidal minimal surfaces in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c
THECONSRUCTION PROCEDURE
! Y -Surfaces: Symmetry
! Helicoidal Barrier: A Y -symmetric, mean-convex region
! Double the surface by rotating about the axes
! Degree Theory with symmetries.
! Curvature Estimates in order to get limit surface.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoidal minimal surfaces in S2 × R
Z Z*
X
0
0*Y+
Tc
T-c
THECONSRUCTION PROCEDURE
! Y -Surfaces: Symmetry
! Helicoidal Barrier: A Y -symmetric, mean-convex region
! Double the surface by rotating about the axes
! Degree Theory with symmetries.
! Curvature Estimates in order to get limit surface.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Y -surfaces
Consider a connected and open surface Σ, (possibly the interior ofa surface with boundary) in a three-manifold N.Suppose that Σ is invariant under an isometric involution ρ of Nthat preserves orientation.
! Here are three possible properties of ρ:
! 1. ρ∗ acts on the homology of Σ by multiplication by −1.
! 2. The quotient surface Σ/ρ is a disk.
! 3. If k is the number of fixed points of ρ in Σ, then
k = 2− χ(Σ).
! Proposition. The three conditions are equivalent.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Y -surfaces
Consider a connected and open surface Σ, (possibly the interior ofa surface with boundary) in a three-manifold N.Suppose that Σ is invariant under an isometric involution ρ of Nthat preserves orientation.
! Here are three possible properties of ρ:
! 1. ρ∗ acts on the homology of Σ by multiplication by −1.
! 2. The quotient surface Σ/ρ is a disk.
! 3. If k is the number of fixed points of ρ in Σ, then
k = 2− χ(Σ).
! Proposition. The three conditions are equivalent.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Y -surfaces
Consider a connected and open surface Σ, (possibly the interior ofa surface with boundary) in a three-manifold N.Suppose that Σ is invariant under an isometric involution ρ of Nthat preserves orientation.
! Here are three possible properties of ρ:
! 1. ρ∗ acts on the homology of Σ by multiplication by −1.
! 2. The quotient surface Σ/ρ is a disk.
! 3. If k is the number of fixed points of ρ in Σ, then
k = 2− χ(Σ).
! Proposition. The three conditions are equivalent.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Y -surfaces
Consider a connected and open surface Σ, (possibly the interior ofa surface with boundary) in a three-manifold N.Suppose that Σ is invariant under an isometric involution ρ of Nthat preserves orientation.
! Here are three possible properties of ρ:
! 1. ρ∗ acts on the homology of Σ by multiplication by −1.
! 2. The quotient surface Σ/ρ is a disk.
! 3. If k is the number of fixed points of ρ in Σ, then
k = 2− χ(Σ).
! Proposition. The three conditions are equivalent.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Y -surfaces
Consider a connected and open surface Σ, (possibly the interior ofa surface with boundary) in a three-manifold N.Suppose that Σ is invariant under an isometric involution ρ of Nthat preserves orientation.
! Here are three possible properties of ρ:
! 1. ρ∗ acts on the homology of Σ by multiplication by −1.
! 2. The quotient surface Σ/ρ is a disk.
! 3. If k is the number of fixed points of ρ in Σ, then
k = 2− χ(Σ).
! Proposition. The three conditions are equivalent.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Y -surfaces
Consider a connected and open surface Σ, (possibly the interior ofa surface with boundary) in a three-manifold N.Suppose that Σ is invariant under an isometric involution ρ of Nthat preserves orientation.
! Here are three possible properties of ρ:
! 1. ρ∗ acts on the homology of Σ by multiplication by −1.
! 2. The quotient surface Σ/ρ is a disk.
! 3. If k is the number of fixed points of ρ in Σ, then
k = 2− χ(Σ).
! Proposition. The three conditions are equivalent.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why the name Y -surface?
Consider a connected and open minimal surface Σ, (possibly theinterior of a surface with boundary) in a three-manifold N.Suppose that Σ is invariant under the isometric involution, ρY , ofN, consisting of 180-rotation about a geodesic Y .
! The fixed points of ρY acting on Σ are the points in Y ∩ Σ.
! Definition. Σ is a Y -surface if it satisfies one of the equivalentconditions 1., 2. or 3.
! Example. The helicoid in R3 (or S2 × R), with Y the normalline (or great circle).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why the name Y -surface?
Consider a connected and open minimal surface Σ, (possibly theinterior of a surface with boundary) in a three-manifold N.Suppose that Σ is invariant under the isometric involution, ρY , ofN, consisting of 180-rotation about a geodesic Y .
! The fixed points of ρY acting on Σ are the points in Y ∩ Σ.
! Definition. Σ is a Y -surface if it satisfies one of the equivalentconditions 1., 2. or 3.
! Example. The helicoid in R3 (or S2 × R), with Y the normalline (or great circle).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Why the name Y -surface?
Consider a connected and open minimal surface Σ, (possibly theinterior of a surface with boundary) in a three-manifold N.Suppose that Σ is invariant under the isometric involution, ρY , ofN, consisting of 180-rotation about a geodesic Y .
! The fixed points of ρY acting on Σ are the points in Y ∩ Σ.
! Definition. Σ is a Y -surface if it satisfies one of the equivalentconditions 1., 2. or 3.
! Example. The helicoid in R3 (or S2 × R), with Y the normalline (or great circle).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 8
2− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ)
= 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ))
=2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ)
= 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
! By “inspection,” ρY acts by multiplication by −1 onhomology.
! |Y ∩ Σ| = 82− χ(Σ) = 2− (2− 2genus(Σ)− ends(Σ)) =2 genus(Σ) + ends(Σ) = 6 + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y
The quotient Σ/σY is a disk.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
The quotient Σ/σY is a disk.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
“Proof” by example.
Y Y
The quotient Σ/σY is a disk.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoidal barrier: a Y -symmetric mean convex region
! Let H ⊂ S2 × R be a helicoid.
! H divides S2 × R into two connected regions. Label one ofthem H+.
! Fix a value c > 0. Then
N = Nc = (p, t) ∈ S2 × R | p ∈ H+, |t| < c..
! ∂N consists of part of H and totally geodesic hemispheres atthe levels ±c . Therefore N is mean convex.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoidal barrier: a Y -symmetric mean convex region
! Let H ⊂ S2 × R be a helicoid.! H divides S2 × R into two connected regions. Label one of
them H+.
! Fix a value c > 0. Then
N = Nc = (p, t) ∈ S2 × R | p ∈ H+, |t| < c..
! ∂N consists of part of H and totally geodesic hemispheres atthe levels ±c . Therefore N is mean convex.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoidal barrier: a Y -symmetric mean convex region
! Let H ⊂ S2 × R be a helicoid.! H divides S2 × R into two connected regions. Label one of
them H+.! Fix a value c > 0. Then
N = Nc = (p, t) ∈ S2 × R | p ∈ H+, |t| < c.
.! ∂N consists of part of H and totally geodesic hemispheres at
the levels ±c . Therefore N is mean convex.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Helicoidal barrier: a Y -symmetric mean convex region
! Let H ⊂ S2 × R be a helicoid.! H divides S2 × R into two connected regions. Label one of
them H+.! Fix a value c > 0. Then
N = Nc = (p, t) ∈ S2 × R | p ∈ H+, |t| < c..
! ∂N consists of part of H and totally geodesic hemispheres atthe levels ±c . Therefore N is mean convex.
Z Z*
X
0
0*Y+
Tc
T-c
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M) = 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)
Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M) = 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M) = 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M) = 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M)
= 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M) = 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Constructing the desired surface of desired genus =k
Z Z*
X
0
0*Y+
Tc
T-c
Suppose S ⊂ N is a Y -surface with boundary Γ.Suppose |Y ∩ S | = k(We have not yet indicated how to do this...)Extend S by rotation about Z to produce M.M has two boundary components, they arefull circles at levels ±c .
M is also a Y -surface, and|Y ∩M| = |Y ∩ S |+ |Y ∩ ρZ (S)|+ |O,O∗|
= k + k + 2 = 2k + 2
|Y ∩M| = 2− χ(M) = 2− (2− 2genus(M)− ends(M))
or2k + 2 = 2genus(M)) + 2.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Producing the desired example of genus = k by taking alimit as c →∞
We have produced a genus = k surface in S2 × (−c , c) thatcontains the axes Z ∪ Z ∗ and has Y -symmetry. We prove uniformcurvature estimates for
M = Mc ⊂ S2 × (−c , c)
and take subsequential limits as cn →∞.
! The limit surface M contains the axes, so each end must beasymptotic to helicoid—in fact the helicoid H used as thebarrier, or a rotation of H.
! M ∩H = Z ∪ Z ∗ ∪ X .
! Each Mc is a Y -surface, so M is a Y -surface
! The intersection of each Mc with Y contains 2k + 2 points,so the same is true for M. Hence genus(M) = k
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Counting minimal surfaces.
Let Σ be a fixed compact 2-manifold with boundary. andLet N be a compact three-manifold with boundary.
If Γ is an embedded curve in ∂N diffeomorphic to ∂Σ, we make thefollowing definitions:
Definition. M∗(N, Γ) denotes the set of embedded minimalsurfaces in N that are diffeomorphic to Σ and that have boundaryΓ.
Definition. |M∗(N, Γ)| denote the number of surfaces inM∗(N, Γ).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Counting minimal surfaces.
Let Σ be a fixed compact 2-manifold with boundary. andLet N be a compact three-manifold with boundary.
If Γ is an embedded curve in ∂N diffeomorphic to ∂Σ, we make thefollowing definitions:
Definition. M∗(N, Γ) denotes the set of embedded minimalsurfaces in N that are diffeomorphic to Σ and that have boundaryΓ.
Definition. |M∗(N, Γ)| denote the number of surfaces inM∗(N, Γ).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Counting minimal surfaces.
Let Σ be a fixed compact 2-manifold with boundary. andLet N be a compact three-manifold with boundary.
If Γ is an embedded curve in ∂N diffeomorphic to ∂Σ, we make thefollowing definitions:
Definition. M∗(N, Γ) denotes the set of embedded minimalsurfaces in N that are diffeomorphic to Σ and that have boundaryΓ.
Definition. |M∗(N, Γ)| denote the number of surfaces inM∗(N, Γ).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Counting minimal surfaces.
Let Σ be a fixed compact 2-manifold with boundary. andLet N be a compact three-manifold with boundary.
If Γ is an embedded curve in ∂N diffeomorphic to ∂Σ, we make thefollowing definitions:
Definition. M∗(N, Γ) denotes the set of embedded minimalsurfaces in N that are diffeomorphic to Σ and that have boundaryΓ.
Definition. |M∗(N, Γ)| denote the number of surfaces inM∗(N, Γ).
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Counting G-invariant minimal surfaces, mod 2.
Fix Σ.
Theorem (White)
Let N be a smooth, compact, mean convex riemannian 3-manifoldthat is homeomorphic to a ball, that has piecewise smoothboundary, and that contains no closed minimal surfaces. Let G bea group of isometries of N. Let Γ ⊂ ∂N be a smooth curve that isG-invariant and G-bumpy.Suppose that no two contiguous connected components of(∂N) \ Γ form a smooth, G-invariant minimal surface.Suppose also that Γ = ∂Ω for some G-invariant region Ω ⊂ ∂N. ∗∗
Then |M∗G (N, Γ)| is even unless Σ is a union of disks, in which
case |M∗G (N, Γ)| is odd.
The subscript “G” in M∗G (N, Γ) means we are looking only at
G -invariant surfaces.
∗∗ We need this condition on Γ in order to be able to deform it toa point in a G -invariant fashion.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Counting G-invariant minimal surfaces, mod 2.
Fix Σ.
Theorem (White)
Let N be a smooth, compact, mean convex riemannian 3-manifoldthat is homeomorphic to a ball, that has piecewise smoothboundary, and that contains no closed minimal surfaces. Let G bea group of isometries of N. Let Γ ⊂ ∂N be a smooth curve that isG-invariant and G-bumpy.Suppose that no two contiguous connected components of(∂N) \ Γ form a smooth, G-invariant minimal surface.Suppose also that Γ = ∂Ω for some G-invariant region Ω ⊂ ∂N. ∗∗
Then |M∗G (N, Γ)| is even unless Σ is a union of disks, in which
case |M∗G (N, Γ)| is odd.
The subscript “G” in M∗G (N, Γ) means we are looking only at
G -invariant surfaces.∗∗ We need this condition on Γ in order to be able to deform it toa point in a G -invariant fashion.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Orienting Γ.
Z Z*
X
0
0*Y+
Tc
T-c
Near the point O, the axis Z is oriented.
We may orient Y (not on Γ) by the choice of H+. This allows usto orient X . We can now talk about positive and negativequadrants at O and at O∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Orienting Γ.
Z Z*
X
0
0*Y+
Tc
T-c
Near the point O, the axis Z is oriented.We may orient Y (not on Γ) by the choice of H+.
This allows usto orient X . We can now talk about positive and negativequadrants at O and at O∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Orienting Γ.
Z Z*
X
0
0*Y+
Tc
T-c
Near the point O, the axis Z is oriented.We may orient Y (not on Γ) by the choice of H+. This allows usto orient X .
We can now talk about positive and negativequadrants at O and at O∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Orienting Γ.
Z Z*
X
0
0*Y+
Tc
T-c
Near the point O, the axis Z is oriented.We may orient Y (not on Γ) by the choice of H+. This allows usto orient X . We can now talk about positive and negativequadrants at O and at O∗.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Positive Roundings of Γ
0
0
0*
0*
! When k is even (left) we connect positively at O∗ to producetwo components.
! When k is odd (right), we connect negatively at O∗ toproduce one component.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Positive Roundings of Γ
0
0
0*
0*
! When k is even (left) we connect positively at O∗ to producetwo components.
! When k is odd (right), we connect negatively at O∗ toproduce one component.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: Positive Roundings of Γ
0
0
0*
0*
! When k is even (left) we connect positively at O∗ to producetwo components.
! When k is odd (right), we connect negatively at O∗ toproduce one component.
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: The fundamentalrelationship
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
Suppose k = 0 or k = 1.This is the case when Σ is either two disks or one disk.
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ 0
By Counting Mod Two Theorem:
1 ∼= |M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: The fundamentalrelationship
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
Suppose k = 0 or k = 1.This is the case when Σ is either two disks or one disk.
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ 0
By Counting Mod Two Theorem:
1 ∼= |M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: The fundamentalrelationship
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
Suppose k = 0 or k = 1.This is the case when Σ is either two disks or one disk.
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ 0
By Counting Mod Two Theorem:
1 ∼= |M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: The fundamentalrelationship
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
Suppose k = 0 or k = 1.This is the case when Σ is either two disks or one disk.
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ 0
By Counting Mod Two Theorem:
1 ∼= |M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: The fundamentalrelationship
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
Suppose k = 0 or k = 1.This is the case when Σ is either two disks or one disk.
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ 0
By Counting Mod Two Theorem:
1 ∼= |M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)
Higher genus helicoids in S2 × R: The fundamentalrelationship
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
Suppose k = 0 or k = 1.This is the case when Σ is either two disks or one disk.
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ |M∗Y (Γ, k − 2,−)|
|M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|+ 0
By Counting Mod Two Theorem:
1 ∼= |M∗Y (Γt , k)| = |M∗
Y (Γ, k,+)|
David Hoffman, Stanford University Helicoidal Surfaces in S2 × R (joint work with Brian White)