ricci flow in homogeneous manifolds - ime.unicamp.brrmiranda/talks/palestra-geometria.pdf · oops,...
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Ricci flow in homogeneousmanifolds:geometry meets dynamical systems.
Ricardo M. [email protected]://www.ime.unicamp.br/~rmiranda
SEMINARIOS DE GEOMETRIA DIFERENCIAL
IMECC/UNICAMP - 11/05/2018
Oops, last slide: references
This talk is based on the following papers:
# L. Grama, R. M. Martins, The Ricci flow of left invariant metrics on full flag
manifold SU(3)/T from a dynamical systems point of view. Bull. Sci. math. 133(5) (2009) 463 – 469.
# L. Grama, R. M. Martins, Global behavior of the Ricci flow on homogeneous
manifolds with two isotropy summands. Indagationes Mathematicae 23 (2012)95–104.
# L. Grama, R. M. Martins, A brief survey on the Ricci flow in homogeneous
manifolds. Sao Paulo Journal of Mathematical Sciences 9 (2015) 37–52.
# L. Grama, R. M. Martins, A numerical treatment to the problem of the quantity
of Einstein metrics on flag manifolds SU(5)/T 4 and SU(6)/T 5, preprint.
Ricci flow
Reference: N. Sheridan, Hamilton’s Ricci Flow. PhD thesis, 2006.
Let M be a Riemannian manifold with metric g0.
The Ricci flow equation (Hamilton’82) is given by∂g(t)
∂t= −2Ric(g(t)),
g(0) = g0
where Ric(g(t)) is the Ricci curvature of the metric g(t)
Hamilton, 1982
Let M be a closed 3-dimensional which admits a Riemannian metricwith strictly positive Ricci curvature. Then M also admits a metric ofconstant positive curvature.
Ricci flow
Corollary
Any simply-connected closed 3-dimensional manifold which admitsa metric of strictly positive Ricci curvature is diffeomorphic to the3-sphere.
Poincare’s Conjecture
Every simply connected closed 3-manifold is homeomorphic to the3-sphere.
Ricci flow
The Ricci flow equation∂g(t)
∂t= −2Ric(g(t)),
g(0) = g0
in general is a system of PDEs. In some special cases we can solve these
equations.
Sn
Let M be the sphere of radius r > 0. The metric is given by g = r2g1,where g1 is the metric on the unit sphere. The curvatures are given
by 1/r2 so Ric(v , v) =n − 1
r2and thus Ric = (n − 1)g1.
Ricci flow
Sn
The Ricci flow equation in this case is given by
∂r2(t)
∂t= −2(n − 1),
g(0) = g0
The solution is r(t) =√
R20 − 2(n − 1)t, where R0 is the initial radius
(note that M → ? when t → R20/(2n − 2).
Hn
If M = Hn then r(t) =√R20 + 2(n − 1)t so r(t)→∞ with r →∞.
Ricci flow on homogeneous manifolds
Very interesting reference: Jorge Lauret, Ricci flow of homogeneous
manifolds. Math. Z. 274 (2013). (Lie Groups)
Theorem
The Ricci flow equation for a homogeneous manifold is a system of
ODEs.
So the Ricci flow is the flow of a system of autonomous differential
equations (a dynamical system) on the finite dimensional space of the
metrics.
If g(t) is the flow with inicial condition g(0) = g0, what happens if
t →∞ (or even t → t0 for some t0 > 0)? Or: how to classify/calculate
the ω-limits of the Ricci flow?
First step: how to obtain the ODE?
New context: left-invariant metrics on flag manifolds.
Bonus: the space of invariant metrics can be parametrized by a
low-dimensional manifold.
The Ricci tensor Ric(g) of (M, g) is given by
Ric(g)(X ,Y ) = −1
2
∑i |[X ,Xi ]p|2 +
1
2(X ,X )
+1
4
∑i,j〈[Xi ,Xj ]p,X 〉2 − 〈[Z ,X ]p,X 〉,
where (·, ·) is the Killing form and etc etc (Besse’s book “Einstein
Manifolds”, 1987).
First case: SO(2n + 1)/(U(m)× SO(2k + 1))
If (λ1, λ2) is a Riemannian invariant metric on
SO(2n + 1)/(U(m)× SO(2k + 1)) then the components of the Ricci
tensor are
r1 =
2(m − 1)
2n − 1+
1 + 2k
2(2n − 1)
λ21λ22,
r2 =n + k
2n − 1+
m − 1
2(2n − 1)
(λ22 − (λ1 − λ2)2
)λ1λ2
,
Second case: SU(3)/T
Let Λ = (λ12, λ23, λ13) be a Riemannian invariant metric on
M6 = SU(3)/T 2.
The components of the Ricci tensor are given by
r12 =1
2λ12+
1
12
(λ12
λ13λ23− λ13λ12λ23
− λ23λ12λ13
)r13 =
1
2λ13+
1
12
(λ13
λ12λ23− λ12λ13λ23
− λ23λ12λ13
)r23 =
1
2λ23+
1
12
(λ23
λ12λ13− λ13λ23λ12
− λ12λ23λ13
)
Third case: SU(n + m + p)/S(U(n)× U(m)× U(p))
For SU(n + m + p)/S(U(n)× U(m)× U(p)), the components of the
Ricci tensor are given by
r1 =p
4(m + n + p)
(λ12
λ13λ23− λ23λ12λ13
− λ13λ12λ23
)+
1
2λ12
r2 =n
4(m + n + p)
(− λ12λ13λ23
− λ23λ12λ13
+λ13
λ12λ23
)+
1
2λ13
r3 =m
4(m + n + p)
(− λ12λ13λ23
+λ23
λ12λ13− λ13λ12λ23
)+
1
2λ23
Turning into polynomials (SO(2n+1)/(U(m)×SO(2k+1)))
For λ1, λ2 > 0 systems
r1 =
2(m − 1)
2n − 1+
1 + 2k
2(2n − 1)
λ21λ22,
r2 =n + k
2n − 1+
m − 1
2(2n − 1)
(λ22 − (λ1 − λ2)2
)λ1λ2
,
and
x = −
(2 + 4k
8n − 4
)x2 −
(2m − 2
2n − 1
)y2,
y = −(2− 2m
8n − 4
)xy −
(n + k +m − 1
2n − 1
)y2,
are equivalent in the first quadrant (x = λ1, y = λ2). The same is true
for the other systems: they are equivalent to a polynomial system.
Qualitative Theory of Differential Equations
x = −
(2 + 4k
8n − 4
)x2 −
(2m − 2
2n − 1
)y2,
y = −(2− 2m
8n − 4
)xy −
(n + k +m − 1
2n − 1
)y2,
Take initial conditions (x0, y0) and consider the flow φt(x0, y0) (the
solution of the above differential equation with initial conditions
x(0) = x0, y(0) = y0).
Note that {φt(x0, y0)}t∈R is a curve with limt→−∞
φt(x0, y0) = 0 and
limt→∞
||φt(x0, y0)|| =∞.
So it is not possible to distinguish the ω-limit sets!
End of the talk?
Poincare compactification I
The Poincare compactification allows us to take a vector field defined on
a non-compact manifold to the sphere (compact) so we can better
understand its behavior at infinity (Velasco, TAMS ’69; Poincare’1881).
Consider the polynomial differential system{x1 = P1(x1, x2),
x2 = P2(x1, x2),
with the associated vector field X = (P1,P2). The degree of X is defined
as d = max{deg(P1), deg(P2)}.
Poincare compactification II
Let
S2 = {y = (y1, y2, y3) ∈ R3; ||y || = 1}
be the unit sphere with northern hemisphere S2+ = {y ∈ S2; y3 > 0},
southern hemisphere S2− = {y ∈ S2; y3 < 0} and equator
S20 = {y ∈ S2; y3 = 0}.
Consider the central projections f+ : R2 → S2+ and f− : R2 → S2
− given by
f+(x) =1
∆(x)(x1, x2, 1)
and
f−(x) = − 1
∆(x)(x1, x2, 1),
where ∆(x) =√
1 + x21 + x22 . We shall use coordinates y = (y1, y2, y3)
for a point y ∈ S2.
Poincare compactification III
As f+ and f− are homeomorphisms, we can identify R2 with both S2+ and
S2−.
The maps f+ and f− define two copies of X , Df+(x)X (x) in the northern
hemisphere, based on f+(x), and Df−(x)X (x) in the southern
hemisphere, based on f−(x).
Note that, for x ∈ R2, when ||x || → ∞, f+(x), f−(x) converge to points
on the equation S20 . This allow us to identify S2
0 with the infinity of R2.
Denote by X the vector field on S2 \ S20 = S2
+ ∪ S2−.
Poincare compactification IV
To extend X (y) to the sphere S2, we define the Poincare
compactification of X as
p(X )(y) = yd−13 X (y).
Theorem (Poincare)
The vector field p(X ) extends X analytically to the whole sphere, and
in such a way that the equator is invariant.
If we know the behavior of p(X ) around the equator S20 ≡ S1, then we
know the behavior of X in the neighborhood of infinity.
Poincare compactification V
The natural projection π of S2 on y3 = 0 is called the Poincare disc and
it is denoted by D2. If we understand the dynamics of p(X ) on D2, then
we completely understand the dynamics of X , even at infinity.
We remark that Theorem 2 works just for polynomial vector fields.
Poincare compactification: charts I
Consider the coordinate neighborhoods Ui = {y ∈ S2, yi > 0} and
Vi = {y ∈ S2, yi < 0}, for i = 1, 2, 3, and the corresponding coordinate
maps φi : Ui → R2 and ψi : Vi → R2, given by
φi (y1, y2, y3) =
(yjyi,ykyi
), ψi (y1, y2, y3) =
(yjyi,ykyi
),
for i , j , k ∈ {1, 2, 3} with j < k . Denote by z = (z1, z2) the value of
φi (y) or ψi (y), according to the local chart that is being used.
Poincare compactification: charts II
Then we have the following expressions for p(X ) written in local charts:
U1 :zd2
(∆(z))d−1
(−z1P1
(1
z2,z1z2
)+ P2
(1
z2,z1z2
),−z2P1
(1
z2,z1z2
));
U2 :zd2
(∆(z))d−1
(−z1P2
(z1z2,
1
z2
)+ P1
(z1z2,
1
z2
),−z2P2
(z1z2,
1
z2
));
U3 :1
(∆(z))d−1(P1(z1, z2),P2(z1, z2)) .
For the charts V1, V2 and V3, we obtain the same expressions (18), (18)
and (18), now multiplied by (−1)d−1.
Poincare compactification: charts III
In this way, the expression of p(X ) is polynomial in each local chart.
Note that the singularities at infinity have z2 = 0.
Poincare comp: SO(2n + 1)/(U(m)× SO(2k + 1)) I
• Chart U1:z1 =
1
2
(m + 2 k) z12 n − 1
− 1
2
(2 k + 2 n + 2m − 2) z12
2 n − 1− 1
2
(4− 4m) z13
2 n − 1,
z2 =1
2
z2 (1 + 2 k)
2 n − 1+
1
2
(4m − 4) z12z2
2 n − 1;
(1)
The singularities at infinity (that is, with z2 = 0) with their local behavior
are:
p1 =
(1
2
m + 2k
m − 1, 0
): stable node; p2 =
(1
2, 0
): saddle; p3 = (0, 0):
stable node.
Poincare comp: SO(2n + 1)/(U(m)× SO(2k + 1)) II
• Chart U2:z1 = −
1
2
(−m − 2 k) z1
2 n − 1−
1
2
(2 k + 2 n + 2m − 2) z12
2 n − 1−
1
2
(−4m + 4) z13
2 n − 1,
z2 =1
2
z2 (1 + 2 k)
2 n − 1+
1
2
(4m − 4) z12z2
2 n − 1.
The singularities at infinity with their local behavior are:
q1 = (2, 0) (≡ p2): saddle; q2 =
(2(m − 1)
m + 2k, 0
)(≡ p1): stable node.
Poincare comp: SO(2n + 1)/(U(m)× SO(2k + 1)) III
Using the coordinates maps φi , ψi , i = 1, 2, 3, see that these singularities
correspond to the following points in S2:
p1 =
(2(m − 1)
√5m2 − 8m + 4mk + 4k2 + 4
,(m + 2k)
√5m2 − 8m + 4mk + 4k2 + 4
, 0
)(stable
node);
p2 =
(2
5
√5,
1
5
√5, 0
)(saddle);
p3 = (1, 0, 0) (stable node).
Main result for SO(2n + 1)/(U(m)× SO(2k + 1))
Theorem
The invariant lines f+ ◦ γ1, f+ ◦ γ2 and f+ ◦ γ3 satisfy the following:
(i) f+(γ1(0)) = f+(γ2(0)) = f+(γ3(0)) = 0;
(ii) limt→−∞ f+(γ1(t)) = p1;
(iii) limt→−∞ f+(γ2(t)) = p2;
(iv) limt→−∞ f+(γ3(t)) = p3.
Main result for SO(2n + 1)/(U(m)× SO(2k + 1))
Main result for SO(2n + 1)/(U(m)× SO(2k + 1)) I
The following result is the main theorem for the flag manifold
SO(2n + 1)/(U(m)× SO(2k + 1)).
Theorem
Let R1,R2 and R3 be the distinguished open regions in the last figure,
and let ϕt be the flow of the projection of p(X ) to D2.
(a) If (x0, y0) ∈ R1 then limt→−∞ ϕt(x0, y0) = q;
(b) If (x0, y0) ∈ R2 ∪ γ2 ∪ R3 then limt→−∞ ϕt(x0, y0) = p2;
(c) If (x0, y0) ∈ γ1 then limt→−∞ ϕt(x0, y0) = p1.
Complete classification of the flow!
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
Since the Ricci flow equation for a homogeneous manifold is a system of
ODEs, the singularities of this system are something important to
calculate.
A metric g is called an Einstein metric if Ric(g) = λg . The constant λ is
called Einstein constant.
So the Einstein metrics are the singularities of the system of ODEs
produced by the Ricci flow.
Or: the Einstein metrics are the solutions of a system of polynomials
equations in several variables.
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
In general:
Theorem (Wang-Ziller)
G/T full flag manifold. For each α ∈ R+ the Ricci component rαcorresponding to the isotropy summand uα is given by
rα =1
2λα +
1
8
∑β,γ∈R+
λαλβλγ
[α
βγ
]− 1
4
∑β,γ∈R+
λγλαλβ
[γ
αβ
].
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
Definition of
[i
j k
]: Let G/H be a compact homogeneous space of a
compact semissimple Lie group G whose the isotropy representation m
decomposes into k pairwise inequivalent irreducible Ad(H)-submodules
mi as m = m1 ⊕ . . .⊕mk . We choose a Q-orthonormal basis {ep}adapted to m =
⊕ki=1 mi . Let Ar
pq = Q([ep, eq], er ) so that
[ep, eq]m =∑
Arpqer , and set[i
j k
]=∑
(Arpq)2 =
∑(Q([ep, eq], er ))2,
where the sum is taken over all indices p, q, r with ep ∈ mi , eq ∈ mj and
er ∈ mk .
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
For SU(n)/T :
Theorem (Sakane)
The components of the Ricci tensor of an invariant metric on SU(n +
1)/T are given by
rij = rαij =1
2λij+
1
4(n + 1)+∑k 6=i,j
(λij
λikλkj− λikλijλkj
− λjkλijλik
).
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
Example (SU(3)/T 2, Arvanitoyergos 1993)
In this case the Einstein equations are given by
r12 =1
x12+
1
12
(x12
x13x23− x13
x12x23− x23
x12x13
)= k
r13 =1
x13+
1
12
(x13
x12x23− x12
x13x23− x23
x12x13
)= k
r23 =1
x23+
1
12
(x23
x12x13− x13
x12x23− x12
x23x13
)= k.
Solutions: the SU(3)-invariant Einstein metrics:
(1, 1, 1), (2, 1, 1), (1, 2, 1), (1, 1, 2).
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
Arvanitoyergos, 1993: SU(n + 1)/T n admits at least(n + 1)!
2+ n + 1
invariant Einstein metrics.
Recently, Wang and Li proved that there are exactly 29 SU(4)-invariant
Einstein metrics on SU(4)/T 3.
Theorem (Grama-R.)
SU(4)/T 3 admits at least 29 invariant Einstein metrics.
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
Theorem (Grama-R.)
SU(5)/T 4 admits at least 396 invariant Einstein metrics, classified into
12 classes up to isometries and homoteties.
Conjecture
SU(5)/T 4 admits exactly 396 invariant Einstein metrics, classifiedinto 12 classes up to isometries and homoteties.
Theorem (Grama-R.)
SU(6)/T 5 admits at least 3941 invariant Einstein metrics, classified into
at least 35 classes up to isometries and homoteties.
Bonus: Einstein metrics for full flag manifolds SU(n)/T n−1
Proofs.
# Almost exhaustive search
# Probabilistic algorithm
# SU(5)/T : 9 (homogeneous) polynomial equations in 9 variables,108 initial conditions (target in 105).
# SU(6)/T : 14 (homogeneous) polynomial equations in 14variables, 106 initial conditions (not stable).
# Both cases: the estimate of Arvanitoyergos is improved.
References I
A. Arvanitoyergos, I. Chrysikos, Invariant Einstein metrics on flag
manifolds with four isotropy summands, Ann. Glob. Anal. Geom. 37(2010), 185–219.
A. Arvanitoyergos, I. Chrysikos, Y. Sakane, Homogeneous Einstein
metrics on G2/T , Proc. AMS 141 (2013), 2485–2499.
A. Arvanitoyergos, New invariant einstein metrics on generalized
flag manifolds. Trans. Amer. Math. Soc. 337, 981-995 (1993).
C. Bohm, B. Wilking, Nonnegatively curved manifolds with finite
fundamental groups admit metrics with positive Ricci curvature,
GAFA Geometric and Functional Analysis 17, 665-681 (2007).
J. Lauret, Ricci flow of homogeneous manifolds. MathematischeZeitschrift 274, 373–403 (2013)
References II
Y. Sakane, Homogeneous Einstein metrics on flag manifolds,Lobachevskii J. Math. 4 (1999), 71–87.
Y. Wang, T. Li, Invariant Einstein metrics on SU(4)/T . Adv. Math.(China) 43 (2014), no. 5, 781 – 788.
M.Wang, W.ZillerThe existence and nonexistence of
homogeneous Einstein metric. Invent. Math 84, 177–194 (1986).
Thank you!