R ENDICONTI
del
S EMINARIO M ATEMATICO
della
U NIVERSITÀ DI P ADOVA
M ARCOS S ALVAI
On the geometry at infinity of the universal covering of Sl (2, R )
Rendiconti del Seminario Matematico della Università di Padova, tome 104 (2000), p. 91-108
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of the Universal Covering of Sl(2, R).
MARCOS
SALVAI (*)
ABSTRACT - Consider the universal covering of Sl(2, R) endowed with the canoni- cal Riemannian metric (one of Thurston’s
eight geometries).
For this spacewe
give
the lines, characterizeasymptotic geodesics, study
thetopology
of the space of
asymptotic
classes, and compute thespread,
a Riemannian in- variant definedby
J. E. D’Atri which reflects thelong-time
behavior ofgeodesics.
1. Introduction.
An
important part
of theglobal shape
of an open Riemannian mani- fold is the structure atinfinity.
The notion ofasymptoticity
ofgeodesics
has
proved
to beextremely
useful for Hadamard manifolds. In this notewe are concerned with this
subject
for the universalcovering
ofSl(2, R),
endowed with the canonical Riemannian metric. This space, which is oneof Thurston’s
eight geometries,
isdiffeomorphic
toR3
but itsgeometry
isnot
trivial,
ithas,
forexample,
Ricci curvature of bothsigns [6, 8].
Given a Riemannian manifold
M,
letdenote the unit
tangent
bundle of M and let d be the distanceon M. For
X E T 1 M,
let y X denote thegeodesic
with initialvelocity
(*) Indirizzo dell’A.: FaMAF, Ciudad Universitaria, 5000 C6rdoba,
Argenti-
na.
E-mail: [email protected]
Partially supported by
CONICOR, CIEM (CONICET) and SECYT (UNC).Mathematics
Subject
Classification (1991): 53 C 22, 53 C 30.X. Unless otherwise
specified, geodesics
are assumed to be nonconstant andparametrized by arelength.
Two
geodesics
y and a in M are said to beasymptotic ( y ~ a)
if thereexists a constant C such that
d(y(t), ~ ( t ) ) ~
C for all t ~ 0 .Asymptoticity
is an
equivalence
relation. We denoteby y( xJ )
the class which contains agiven geodesic
y andby Aoo (M)
the set of all such classes. We notice that if M is a Hadamardmanifold,
then the map F : definedby F(X)
= is abijection
for[5].
and let
EM2(R) tr X = 0}
be its Liealgebra.
Consider on G the left invariant Riemannianmetric {,)
such that(X, Y)
= 2 tr(XYt )
for allX,
Y E g. Let 3: G - G be the universal Riemanniancovering
of G.Let K =
PSO(2)
and let H =G/K
be endowed with the Riemannian metric such that the canonicalprojection a:
G - H is a Riemannian sub- mersion. H is thehyperbolic plane
of constant curvature -1. We will show that ageodesic
in Gprojects
either to apoint
in H or to a curve ofconstant
geodesic
curvature in H . A nonconstantcomplete
curve c in Hwith constant
geodesic
curvature xsatisfying ( x ~ > 1 (respectively I
=1 )
is a circle(respectively
ahorocycle).
If1,
there exists= lim
c(t)
in theasymptotic
border of H. We recall that ageodesic
t- 00
is called a Line if it minimizes distance between any of its
points.
Theorems 1.1 and 1.2 below describe the
asymptoticity
ofgeodesics
inG,
the former withregard
to theprojection
G - H and the latter with re-spect
to a fixedpoint
in G.1.1 THEOREM. Let y and y 1 be
geodesics
inG,
whichproject
tocurves c and cl in
H, having (constant) geodesic
curvatures K and Kl,respectively (in
caseof
notbeing constant).
Then thefollowing
asser-tions are true:
a) If
c isconstant,
then y 1 - yonly if
cl is constant.b) If > 1,
thenYl-y if
andonLy if
Kl = K.c) If = 1,
then Y 1- y
if
andonly if
there existsto
E suchthat
cl(. ) = c(. + to ).
d) If I 1,
then y 1 - yif
andonly if
x 1= K and= c( 00 ).
Moreover,
y is a lineif
andonly if I K I
~ 1.Consider the Cartan
decomposition
g = RZ + p associated toK,
where . . Let e be the
identity
of Gand
E ~ -1 ( e ).
As usual we shallidentify TeK H with p
andTë G
= g . Let X denote the setof
orientedhorocycles of H .
Given aregular
curve cin
H,
let[c]
be the set ofreparametrizations
of cpreserving
thedirection.
1.2 THEOREM. Given
X,
Y distinct vectors in the unittangent sphere of G
ate,
then y x isasymptotic
to y yif
andonly if X
and Y lieboth in the same
parallel
at a distance less thanfrom
thepoles (we
thinkof
Z as the NorthPole).
Moreover,
there aregeodesics
inG
which are notasymptotic
to anygeodesic through
e.They
are in naturalcorrespondence
with the horo-cycles of
H notcontaining
eK.More
precisely:
Let usdefine
the map F :Te G -~ A ~ (G) by F(X) =
= y
x( 00),
thenb)
The map II :A ~ (G) - Image (F) - ( h
EI eK ft h ~ is
well de-fined by II( y( ~ ) ) _ [(n 0 5í) y]
and is moreover abijection.
In
particular
F is neitherinjective
norsurjective.
D’Atri defined in
[4]
a Riemannian invariantreflecting
thelong-time
behavior of
geodesics.
Given acomplete noncompact
Riemannian mani- fold M of dimension n , let thespread
of M be definedby
spread (M) =
0 ;1~ n ~ I
there exists a distribution E0 of dimension1~,
}
= max defined on the
complement
of acompact
set inM,
such that0 for all unbounded
geodesics
y in MJ
where denotes the norm of the
orthogonal projection
ofto
6DY(t) (unlike
in[4],
we consider unboundedgeodesics
instead ofrays).
For
example spread
= n -1,
since everystraight
line isasymptoti- cally orthogonal
to the distribution onR" - ( 0 ) tangent
to thespheres
centered at zero.
1.3 THEOREM.
spread (G) = 0.
2. Preliminaries.
In this section we introduce some more notation and known or basic facts. We sketch some of the
proofs
for the sake ofcompleteness.
Twounit
tangent
vectorsX ,
Y are said to beasymptotic
if y x isasymptotic
toy y. In this case we shall write X --- Y.
The unit
tangent
spaceof
thehyperbolic plane.
G can be identified via left
multiplication
with the set of orientationpreserving
isometries of Hand, hence,
it actscanonically
onT 1 H.
The connection
operator
X : is well definedby ~) =
= V’ ( o ),
where V is a curve inT 1 M
withV( 0) = ~ ( V’
denotes the covari- ant derivative of Valong
the curve JC 0V,
yr : the canonical pro-jection).
Let carry the canonical(Sasaki) metric,
definedby 11~112
== llR *v Ell2 + llK(E)ll2 for E E TvT1 H, v E T1 H.
H carries a canonical
complex structure,
which comes from the G-in- variantquasi-complex
structure i inducedby
LetX1 =
0 ~1); by
the usual identificationof p
with we can writeXl
Esince
The
map 0 : G ~ T 1 H
definedby Ø( g)
is anisometry (notice
that(exp tY)*eKX1
is theparallel transport
ofX, along
the curve( exp tY) K
since(G, K)
is asymmetric pair).
Geodesics in G.
Using
Sasakiequations
we obtained inProposition
3.1 of[7]
the fol-lowing description
of thegeodesics
in G(or equivalently
inT 1 H).
If V isa smooth curve in
T 1 H,
then V’ will denote the covariant derivativealong
theprojection
of V to H.2.1 PROPOSITION.
a)
Let V be ageodesic
inT 1 H
and let c = no V .Then ()V’ ((
= const, A and oneof
thefollowing possibili-
ties holds:
i) If ~==0,
then V is a constantspeed
curve in the circleT1c(0)H.
ii) If
~, ~0,
then thegeodesic
curvature Kof
c withrespect
to thenormal is constant and
for
all t E where z E cC is such thatV(O)
=z c( 0 ).
b) Conversely,
any curve V inT’H satisfying (i)
or(ii)
~is a con-stant
speed geodesic. Moreover, given
a constantspeed
curve c in Hwith constant
geodesic
curvature, andVo
E there is aunique geodesic
V inT’H
whichprojects
to c and such thatV(O)
=Yo.
c)
For V as in(1)
one has(V, Z) = - AK.
Inparticular
the normof
the vertical
component of V
withrespect
to the submersion T1 H ~
H is= À x (
, hence V has unitspeed if
andonly if
In
fact, part
of the last item is not in the citedproposition
of[7],
but itfollows from the
following computation.
The Riemannian universal
covering of
G.Let S’
= a 1(0
a-’la
>0,
b ER)
and let us consider the Iwasawa de-composition
of Ggiven by
thediffeomorphism 0 :
S xS1 - G, (well)
de- finedby
where
R(e)
denotes the matrix of the rotationthrough
theangle 0
in thecanonical basis of
R2 .
Weidentify S
with theimage
of Sx 111 under
This solvable
subgroup
of G actssimply transitively
on H.Since S is
simply connected,
the map definedby x )
=e ~ )
is a universalcovering
map. Let us consider on S x R the liftedmultiplication
withidentity e
=( e , 0).
Then( s , 0 ). ( s1, 0 )
==
(ssl, 0) and (s, x). (e, xl ) _ (s, x
+xl )
forall s,
x, e R . For the sake ofsimplicity
we shall write s . x =(s, x).
When no confusion arises we shallidentify
s with( s , 0 ), x
with( e , x ),
as well as S with S xx ( 0 )
cG.
We denote P2.2 REMARK. The
following facts
are easy toverify.
a)
The metric onG
isleft
invariant.Furthermore,
theright
mul-tiplication
s.x Hs.(x
+xo)
is anisometry of
Gfor
any xo E sinceadz
is skew
symmetric. Hence, if
gj = Xj with Sj E S and Xj E I~( j
=1, 2 ),
then
N IV
b)
Letd,
d anddH
be the distances onG,
G and Hrespectively.
Since ,~ and 1C are Riemannian
submersions,
thenCurves with constant
geodesic
curvature in the upperhalf plane.
Now,
we consider for thehyperbolic plane
the model H ={z
ewith the metric
(z = x + iy). Then,
We denote
by
aH the border R UI oo I
ofH,
which ishomeomorphic
tothe circle with the relative
topology
in thesphere C
Uf o- }.
The distance
dH
on H isgiven by ([2]
Theorem7.2.1)
G acts
by
orientationpreserving
isometries on the upper halfplane by
g.z= gM (z ),
where gM denotes the M6bius transformation associated to g . In this way we canidentify
eK = i andXl
=( i , i ) = ( dy a
I and theisometry 0
reads now0(g) =
We define the unit vector field I on H
by Iz
=( z , ( Im z ) i ).
We noticethat
Iz
isasymptotic
toIz ,
I for all z , z ’ E H . It can beeasily
checkedthat
We recall Lemma 5.5 of
[1],
which asserts that ifV,
W areasymptotic
unit vectors in
T 1 H,
thenGiven a differentiable curve c in the upper half
plane,
denoteby
E C its derivative at t E R and
by c( t )
=c( t ),
de( t )
the corre-dt dt
sponding
element of TH.2.3 LEMMA. Let c be a curve in H with
II
~II
A and constantgeodesic
curvature K with
respect
to the normal Then theimage of
c is a E~c-clidean circle or
straight
line intersected 2vith H and(8)
c isinjective
~ c is not bounded -->I K
1 .If 1,
there exists limc(t)
= E aH .Moreover, if c( - 00 )
E then therethe
angle
between the orientedirrzage of
c and the real axis atc( - 00 ),
and cos 6 = K.
PROOF. Let a E
( o, z)
and let gt be theone-parameter subgroup
ofisometries of H
given by gt ( z )
= e / z for z E H .By
Lemma 3.2 in[7],
the curve
c( t )
=gt ( e ia )
has constantgeodesic
curvatureequal
tocos a .
It is also
straightforward
to check that = coth r if c is ageodesic
circle of radius r
(using polar coordinates),
and K = --t 1 for the curvec(t)
= i --t t . The assertions follow now from the fact that G acts transi-tively
onT 1
H andconformally
on CI - 0
2.4 REMARK. Let c be a curve in H as in the
preceding
lemma. It canbe derived
from
it that thefollowing
statements are true(the
last three itemsgive parametrizations of
curvesof
constantgeodesic
curvature inthe upper
half plane
modelof
thehyperbolic plane).
a) If 1,
then c iscompletely
determinedby c(0),
K, A andc( 00 ).
b) I K(
- 1if
andonly if
theimage of
c is ahorocycle.
c) If x ~ ~
1 andc( 00), c( - 00)
are both realnumbers,
thenc(t)
== z + Re
for
some zE C,
R > 0 and astrictly
monotonicdifferentiable function
d) If x ~ ~
1 and eitherof
the endsof
cis 00,
then c is thereparametrization of
astraight
line.If c( 00 ) = 00
andI
= 1 we havemore
precisely: c(t)
= z ±( Im z )
At with z E H .If c( 00 ) = 00
andI K I 1,
then c has the
form c(t)
= b + withx(t) = A(sin a) t
+b, IE~,
a E
( o , n),
cos a = K.e) If I
>1,
then theimage of
c is ageodesic
circleof hyperbolic
radius
I r I
andlength
2 RsinhI
rI
, where K = coth r .Therefore c(t)
= z ++ zl e
iy~t~ ,
, with y : astrictly
monotonicdifferentiable function
such that
for
any3.
Asymptotic geodesics
inG.
We
begin
this sectionstating
some lemmata that are necessary to ob- tain Theorem1.1,
from which Theorem 1.2 follows. At the end westudy
the
topology
of3.1 LEMMA. Let V be a
geodesic
inT 1
H such that c = Jio V is notconstant. Let A ~ 0 and let K denote the
geodesic
curvatureof
c(both
are constantaccording
toProposition 2.1). Then,
a) (length Vho, l~ )2 = (length
c/ [0, L~ )2
+(ÀKl)2.
b) If
V realizes the distance between twoasymptotic
vectorsVo and Vl
inT’H,
thenc) If I K
1 andV( o )
=Ic(o),
thenV(t)
=2).Kt),
withy(O)
= 0 andy(t) ~ I
2Jifor
all t.PROOF.
(a)
is immediate from(2),
because V isparametrized by arclength.
b)
Let 1 =d(Vo, V1 ). By (7)
we have thatThen, according
to(2),
1+ x2
= 2 and hencex ~ ~
1.c) Suppose
thatc( 00)
andc( - 00)
are both real numbers. It follows from RemarkIf > 0 for
all t ,
then =Ic(t)Àeix(t). Consequently by ( 1 )
we have thatNow,
Az = sinceV( o ) =1 ~~ ° ~ . Hence,
y : = x -r( 0 )
satisfiesI y(t) I
21r for all t . If 0 for allt ,
oneproceeds
in the same way with x + Jt instead of x .Finally,
if either of the ends of c is 00 one cantake y = 0
(see
Remark 2.4(d)).
3.2 LEMMA.
If g = s. x, gl = sl. xl E G
withs, sl E ,S
andthen
PROOF.
By (3),
It is clear thatd (e, x - x, I
We claim thatd ( s , Sl) ~ 3 d( s , s1 )
+ 2 Z.By
leftinvariance of the metrics it suffices to show that
d (e, 3d(e, sl )
+ 2zfor all s, ES. Let 1 =
d( e , sl )
and let V be ageodesic
inT 1 H
such thatV(o) _ ~(e)
=Ii
andV(L) _ Ø(Sl)
=181. i (see (6)).
Let c = zV and let K be thegeodesic
curvature of c .By
Lemma 3.1(b)
we have that 1and, hence, 2 ~, ~ x ~ ~
2by (2).
Let y be the lift of V to G withy(0)
= e and lets( t )
E ,S such thatØ(s(t»
=Ic(t) (unique by (6) because q5
is a diffeomor-phism).
Sine with
y(0)
= 0 andI
2nby
Lemma3.1
(c),
we have that y =s(t). (y(t) - 2ÀKt).
HenceThe lemma follows now from
(7),
whichimplies
thatd(s,
ý2dH(Ps, Ps1 ),
since Rs = Ps and0(s)
=Ins
isasymptotic
to(P(sl)
forall s , s 1 E ,S .
NOTATION. FrorrL now on,
given
ageodesic
y inG,
we shall denote V= 0 Fr Y,
c =Py ,
Aë II I
and K thegeodesic
curvatureof
c ,provided
0. For the
geodesic
y 1 inG
we shall use the obviousanalogous
notation.
Suppose
thatIK/ I
> 1 andput
3.3 LEMMA.
a) If
c is a curve in H with constantgeodesic
curvatureK and À =
1 / 1 + x2 ,
then theperiod of
c isv I.
.b) If
y is ageodesic
inG
whichprojects
to c as in(a)
andsatisfies y(0) ES,
thenwhere s is a curve in S with
period
2 nI v I
and y : lE~ -~ lE~ is astrictly
monotonic
differentiable function
such thaty(2mnv)
=for
allm E Z.
PROOF.
Using (2)
onecomputes
that sinhr = if K = coth r.Hence, (a)
follows from the first assertion of Remark 2.4(e).
Alsoby
thatremark,
we have that withz1 E C
and y : R-R astrictly
monotonic function such thaty(2mnv)
for any m E Z.Therefore,
and sofor some z2 Etc.
On the other
hand,
it followsby straightforward computations
from(2) that fl 0
= 2AK. Thenby Proposition
2.1(a)
we have thatV( t )
==
c(t)
with z E C.Then, V(t)
=Ic(t)
because Z2 z =1 sincey( o ) = 0 ,
andy(0)
E Simplies
thatV(0)
=Ic(o).
If s is the curve in S suchthat
s(t)(i)
=c(t),
we obtainby (6)
that3y(t)
=o(s(t), e(y(t)-¡lt)i),
whichimplies (b).
3.4 COROLLARY. Let y be as in the
previous lemma,
then there exist continuousI
>f : R~R, satisfy-
ing
that d isinj ective
andI
>1, ~ lf(t) I
2nfor
all K,t ,
such thaty(t) = s ( t ) (d ( x) t + f ( t ) ) ,
where s is a b ounded curve in ,S .PROOF. Take s as in the
lemma, ô = .!. -/1
o v andf ( t )
=?/(~) 2013 2013.
v v
The
required properties
can beeasily
verified.Indeed,
onecomputes
that 6 is odd and >
1,
v ’(K) 0 , provided
that K > 1.Consequently, d ( x)
0and 6’(K)
> 0 if K > 1.Finally,
one checks that- -1.
3.5 PROPOSITION.
a)
Let x > 0 and let k be thelargest integer strictly
smaller than
x .
Then there exist real numbers Kk ... Kl 0 and k + 1 2.7rgeodesic segments
y o , ... , Y k inG j oining e
with x =( e , x )
=6x-p (xZ),
such that y 0
projets
to a constant curve inH,
andfor
n =1,
... , k theprojection of
Y n to H runs n timesalong
a circleof
constantgeodesic
curvature
If
x ~ 2 ir(respectively
x >2,,r),
then y o(respectively
y1)
minimizeslength
between e and x .Moreover,
In
particular,
b)
Nogeodesic
inG
is bounded.PROOF.
c~)
Let y be ageodesic
in G such thaty( o )
= e andy(l) = - ( e , x ) = x .
We have that c = i if andonly
ify ( t ) = t
Suppose
that c is not constant. Then c is notinjective
sincec(0)
= ==
i ,
and henceIKI I
> 1by (8).
Lemma 3.3(b) implies
that x =y( L) _
=
l)
for some monotonic function ysatisfying
= 2mn for all Hence
s( l )
= e .By
Lemma 3.3(a)
we have thatfor some
counting
the number of turns.Thus,
andfor some or
equivalently
Now, ,~( v ) v > 2 yields easily
thatc 0 ,
hence K isnegative, v -1,
In
particular,
if then c is constantand the
unique geodesic
inG joining e
with .r is/(~)=~
and sod(e, x) = x.
Suppose
now that .r > 2 a. Given n E N with n~,
there exists aunique
~ 20131satisfying (11), namely
2,,rFor the existence of Y n, take any curve c~ in H with
Cn (0)
=i ,
con-stant
geodesic
curvature-1 ( v o (n ) )
and /that v :
I
>11 - R
is one toone).
LetV,
be thegeodesic
inT 1 H projecting
-to c~ withV~(0) = Ii . By
the way xn has beenchosen,
wehave that the lift y n of
Vn
toG through e,
restricted to the interval[0, -2~jn~o(~)L
satisfies therequired properties. Therefore,
Since - nv o (n)
is anincreasing
function of n on1, x (a straight-
L
21r Iforward
computation),
it attains its minimum value on that interval atn = 1. Then
d (e, x )
is the minimum between xNow,
x if x > 2jr.
Consequently,
the stated formula ford (e, x)
iscorrect.
Clearly,
its values converge toinfinity
when x ~ ~ .b)
Let y be ageodesic
in G. We may suppose thaty( 0 )
= e. If c isconstant, y(t) = (e, ± t)
is not boundedby (a).
Assume c is not constant and has constantgeodesic
curvature K. If( x ~ ~ 1,
y is unbounded since cis
by (8).
IfI
>1, to
is theperiod
of c, and nz e Z isgiven,
thenand the
geodesic
Q definedby a(t) = y(t +
+
mto )
coincides withy( t ),
since bothproject
to c and have thesame value at t = 0 . In
particular,
fort = to
one hasy( (m + 1 ) to ) _
=
y(to ) y(mto ). By induction, y(nto )
= for all Henceby (10)
we have that as n --~ ~ .
Therefore,
y is not bounded.PROOF OF THEOREM 1.3. Let
a (t) = (e, t) (a geodesic
inG),
let W =Q and let y be a
geodesic
y 1 as inProposition 3.5,
associated to the choice x =Hence,
thegeodesic
V : _ 3 o y isperiodic, V( 0 )
=V(l) =
=
W( 0 ) and y( 1 )
= 4R(here
1 is theperiod Now, by Proposition
2.1(c)
we have that
for all since 3 is a local
isometry.
On the other
hand,
forf3
ER,
the innerautomorphism I~
=I(o,
{3)’~’-~(0,~)~(0, -/3)
is anisometry
of G that fixes of. Its differential fixes and rotates itsorthogonal
spacethrough
theangle ~3 .
Denote
by
thegeodesic
y . We have that ER}
consists of the circle of unit vectors u ETa(4kn)G
suchthat,
is constantand
equal
0(independent
of1~). Therefore,
no choice of~~~4k~>
of dimension 1 or 2 will
satisfy
for all
f3 E R..
3.6 LEMMA. For each
geodesic
G withI K 1
there exists anisometry Vf
such that = e and =Clearly, for
anygeodesic
a inG,
we have that y 2013 aif
andonly if Vfy -
Wa.PROOF. Let c =
Py
and let k e K be such that /c.c(
=(k. c)( oo)
== 00. Let x E R
satisfy q5(e, eix)
= k and defineG - G by fJI(g)
== (e, .r).~.(e, -~). By
Remark 2.2(a),
W is anisometry
ofG and, clearly, fJI(e)
= e. Since Fr is ahomomorphism,
we have that =k -
1for all
g E G and, therefore, Thus,
(P~/)(oo)=~. c(-) =
00..PROOF OF THEOREM 1.1.
By
Remark 2.2(a)
we may suppose without loss ofgenerality
thaty( 0)
= e andyi(0)
E S. This meansby (6)
thatc(0)=z, V(0)==7,
anda)
andb):
If c is constant orI
>1,
then(8) implies
that c is bound-ed.
Assuming
that y 1 o-- y, we haveby (4)
that cl is boundedand, again by (8),
weget
that cl is constant orI Kl I
> 1.If
I
and1
are bothgreater
than1, applying Corollary
3.4 to y and y 1, we obtainby (3)
thatis bounded
by
Lemma 3.2 and(8).
On the otherhand,
since 6 isinjective,
if K # we would have that lim t- 00
|(8(K) - 8(K1))t
+a(t) I = 00,
whichby Proposition
3.5 contradicts theassumption
y 1--- y .In the case when either c or cl is
constant,
oneproceeds
in the sameway
(observe
that161 [
> 1and,
moreover, that c is constant if andonly
ify(t) = g. t
oryet)
=g. ( - t )
forany t
E R and some g EG).
So far we haveproved
the sufficient conditions of(a)
and(b).
Conversely,
ifI K I
> 1 and x = x,by
Lemma 3.2 andapplying
as be-fore
Corollary 3.4,
it follows thatThe first term on the
right
hand side is bounded becauseby (8)
both cand Cl are bounded. Since the second term is bounded
by I
4,~,
we obtain y 1 - y.Thus, (a)
and(b)
areproved.
c)
andd):
If1, by
Remark 2.2(a)
and Lemma 3.6 we may sup- poseadditionally
thatBy
Remark 2.4(d),
= holdsfor some WE C.
Thus, Proposition
2.1(a) implies
thatV( t ) :
= W 3 oy( t )
== e
Hence,
we have for some curves(t)
in S thatAssume that y 1--- y . It follows from
(4)
and(8)
that c and Cl are both notbounded, K 1 ~ ~
1 andThen,
a formulaanalog-
ous to
(12)
holds for y 1, sinceyi(0) eS. Therefore, (3) yields d (y(t), y 1 ( t ) ) ~ d ( e,
K 1-t) - const,
whichby Proposition
3.5 isbounded for t > 0
only
if 1= ÀK. Thisimplies together
with(2)
thatKl = K.
In
particular,
if K = E = ±1,
we haveby
Remark 2.4(d)
thatc( t )
= i ++ EAt
(recall
thatc(0)
=i )
and = z +Now,
it follows from(4)
and(5)
thatwhich,
as it is easy tocompute,
is bounded for t > 0only
if Im z = 1.Thus,
there exists
to E
R such that cl(.)
=c(.
+to ).
So we have verified the suffi- cient conditions in(c)
and(d).
In order to prove the converses, let us suppose that x 1 = x and
c1 ( oo)
=c( 00 ). Then,
a formulaanalogous
to(12)
holds for y 1 and Lemma3.2
implies
that(notice
that ~, _ ~,1 1by (2)).
If
c1(.) = c(. + to)
for some thenTherefore,
y 1--- y and we have checked the necessary condition in(c).
If
I 1, according
to the form of c and cl described in Remark 2.4(d),
then there exist a >0, b E
R such that =ac(t)
+ b for all t E R. It follows then from(5)
thatwhich is bounded for t > 0 because of the form of c.
Hence,
y 1--- y .Next,
we prove the last assertion. Let y be ageodesic
in G withI K
1and take s t such that
ÀV(s)
= andAV(t)
=c( t ).
Theunique g
E Gsatisfying ( dg ) V(s)
=V( t )
ishyperbolic (it
translates thegeodesic join- ing
theendpoints
of c inaH).
Let T be a discretecocompact subgroup
ofG
containing g
andacting freely
andproperly discontinuously
on H.Then I’V is a
periodic geodesic
inT ~T 1 H -== T 1 (T ~H). By
Lemma 3.5 of[7]
we have that minimizeslength
in its freehomotopy
class.Hence any lift of TV is a
line,
inparticular
y . IfI K I
=1,
then y is aline,
since it is a limit of
geodesics
withI K I
1([3]
Lemma1.67).
For the
remaining
cases we may suppose thaty(0)
= e. Ify(t) = - ( e , t ),
y isclearly
not a rayby (9).
IfI
> 1 andto
is theperiod
of c, wehave
by Proposition
3.5 thaty ( to )
=( e , x )
withx ~ I
> 2 a and is notminimizing
since is not one to one.Hence, y ~ ~ o, ~ ~
is not aray.
PROOF OF THEOREM 1.2.
a)
Lety , y 1 be geodesics
in G withy(0)
== y 1 ( 0 ) = e, y( 0 )
= Y. We have that c is constant if andonly
if
0,
orequivalently
X = ± Z . It follows then from Theorem 1.1(a)
that in this caseF(X)
=F(Y)
if andonly
if y 1 = y , orequivalently X
== Y = ± Z . Hence the
equivalence
is true if either c or Cl is constant.Suppose
now that c is not constant andput
as before V = (Po 3 o y .Writing
X = Y +~X , Z) Z
with andidentifying Te G
withTe G
through 3*, , it
follows fromProposition
2.1(c)
and(2)
that2(X, Z~2
> 1 if andonly
if[ K I
>1,
and also that(X - Y, Z)
= 0 if andonly
if K = x 1.Consequently,
ifI K I
>1,
the assertion followsimmediately
from Theo-rem 1.1
b). Finally,
if1,
then X =Y by
Theorem 1.1(c)
and(d)
to-gether
with Remark 2.4(a) (notice
thatc(0)
=c1 ( o )
= eK and that c de-termines y if
y(0)
= eby Proposition
2.1(b)).
b)
Let y be ageodesic
in G. Let usverify
that if either theimage
ofc contains
eK,
or c isconstant,
or1,
then there exists ageodesic
y 1 in G such that andIndeed,
ifc(to ) = eK,
theny(to ) _ (e , xo )
with xo E R.Defining y 1 (t)
=y(t
+to) y(to) -
we have thaty 1 (0)
= e andfor all t E
R,
and so y 1 ~ y.If c is constant or
I K I
>1,
then Theorem 1.1(a)
and(b) implies
that/i:=y(0)’~y
has therequired properties (observe
that cl =_ ,~(Y(o).)_~ c).
If
I K I
1 we may supposeby
Lemma 3.6 thatc( 00 ) = 00.
Ify(0)
== with
So E Sand
we definey 1 ( t )
=so y ( t ) ( e , xo )
for allwhich satisfies
y 1 ( o )
= e. SincePso y
=so Py ,
we obtainby
Lemma3.2 that
for all t E R. But so. z = az + b for some a > 0 and b E R.
Then, proceeding
as in the
proof
of the necessary condition of Theorem 1.1(d),
we concludethat y 1--- y .
Consequently,
we have shown that ifImage (F),
then[c]
is an orientedhorocycle
which does not contain eK(see
Remark 2.4(b)).
Moreover,
Theorem 1.1(c) implies
that II is well defined andinjec-
tive.
Finally, by Proposition
2.1(b),
if Cl is a curve in H with constantgeodesic
curvature x 1 and( 1 + x i ) ~, 2 =1,
then there exists ageodesic
y 1 in G such that
Py
i = cl . From this and the necessary condition of Theorem 1.1(c)
it follows that 77 issurjective. 8
On the
topology of A ~ (G).
Given a Riemannian manifold
M,
wetopologise A ~ (M)
via the obvi-ous identification with
7~M/2013,
the unittangent
bundle of M moduloasymptotic
vectors.Although
our spaceG
ishomogeneous
anddiffeomorphic
tohas not nice
topological properties,
as thefollowing
remarkstates.
3.7 REMARK. is neither
Hausdorff
norcompact.
PROOF. We
begin by defining
the left invariant 1-form cv onG
suchthat
(X, Z)
for all X E g. We denoteby Lg
the leftmultiplication
by g and for X E T1G we putcx=Pyx.
SincellXll = llzll
=1, I w(X) I =
1 ifand
only
if cx N is constant. IfI w(X) I 1,
it follows fromProposition
IV 2.1(c)
and theG-invariance (notice
that =3( g) o P
forall g
EG,
with3( g)
an orientationpreserving isometry
ofH)
thatfor all
X E T 1 G, whereK(X)
is thegeodesic
curvature of cx and= Hence
(2) implies
that2 cv(X)2
>1 (respectively =1, 1)
if andonly
ifI K(X) I
> 1(respectively =1, 1).
Let us take now X E
T 1 G
such that[ cx ]
E X(hence
1by
Remark 2.4
(b)). Choose g
E G such that the orientedhorocycles [g.cx]
and
[cx]
are distinct. LetXn
be a sequence inT 1 G converging
to X suchthat 1 and
I
> 1 for all n . We considernow 11
EG
with3í(g)
= g , and denote andConsequently,
con-verges to
[ Y] ( [ W]
denotes theequivalence
class of W inT 1 G). By (13), (2)
and theG-invariance,
we have that = ThenYn --- Xn by
Theorem 1.1
(b).
Hence G is not Hausdorff since Y is notasymptotic
to Xby
Theorem 1.1(c) ( [Py Y] _ [ g.cx] ~ [cx] by
the choice ofg).
To show that
Aoo (G)
is notcompact,
let us denoteby ~+
the set of allhorocycles
in H withpositive geodesic
curvature andspeed
G actstransitively
on~-C+ .
Let N be theisotropy
group at thehorocycle t
H i ++
~-C+
becomes anoncompact topological
space via the identification with G/N endowed with thequotient topology.
One can show that the
projection
is open and that theset is closed and ----saturated. Hence
U/ --- may be
thought
of as a closedtopological subspace
withthe relative
topology.
Thenby
Theorem 1.1(c)
themap f : U/ --- -~ ~C+
iswell defined
by f([X]) = [cx]. Since f is onto,
to show that is notcompact,
it remainsonly
toverify
thatf
is continuous.Indeed,
one cancheck
by straightforward computations
thatf
lifts tof :
U- G definedby/(X) = ~~(z’B/2c~(0)),
which isclearly
continuous.REFERENCES
[1] W. BALLMANN - M. BRIN - K. BURNS, On
surfaces
with noconjugate points,
J.Diff.
Geometry,
25 (1987), pp. 249-273.[2] A. BEARDON, The
Geometry of
DiscreteGroups, Springer-Verlag
(1983).[3] A. BESSE, Einstein
manifolds, Springer-Verlag
(1987).[4] J. E. D’ATRI, The
long-time
behaviorof geodesics
in certainleft
invariant metrics, Proc. Amer. Math. Soc., 116 (1992), pp. 813-817.[5] P. EBERLEIN - B. O’NEILL,
Visibility Manifolds,
Pacific J. of Math., 46 (1973),pp. 45-109.
[6] J. MILNOR, Curvatures
of left
invariants metrics on Lie groups, Adv. inMath., 21 (1976), pp. 293-329.
[7] M. SALVAI,
Spectra of
unit tangent bundlesof hyperbolic
Riemannsurfaces,
Ann. Global Anal. Geom., 16 (1988), pp. 357-370.
[8] P. SCOTT, The
geometries of 3-manifolds,
Bull. London Math. Soc., 15 (1983),pp. 401-487.
Manoscritto pervenuto in redazione il 31 marzo 1999.