A NNALES DE L ’I. H. P., SECTION A
V ADIM A. K AIMANOVICH
Invariant measures of the geodesic flow and measures at infinity on negatively curved manifolds
Annales de l’I. H. P., section A, tome 53, n
o4 (1990), p. 361-393
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361
Invariant
measuresof the geodesic flow and
measuresat infinity
onnegatively curved manifolds
Vadim A. KAIMANOVICH
Department of Applied Mathematics, Leningrad Shipbuilding Institute, Lotsmanskaya 3, Leningrad 190008, U.R.S.S.
and Mathematics Institute, University of Warwick, Coventry CV4 7AL, U.K.
Vol. 53, n° 4, 1990, Physique théorique
ABSTRACT. -
Basing
upon thecorrespondence
between the invariantmeasures of the
geodesic
flow on anegatively
curved manifold and themeasures on the
sphere
atinfinity,
wegive
new constructions of the maximal entropy and the harmonic invariant measures of thegeodesic
flow.
Key words : Negatively curved manifold, sphere at infinity, geodesic flow, Patterson
measure, Brownian motion, harmonic measure.
RESUME. 2014 En partant de la
correspondance
entre les mesures inva-riantes pour le flot
géodésique
sur une variete a courburenegative
et lesmesures sur la
sphere
al’infini,
nous donnons des constructions nouvelles des mesures invariantes(la
mesured’entropie
maximale et la mesureharmonique)
pour le flotgeodesique.
Classification A.M.S. : Primary 58 F 11, 58 F 17, 58 G 32, Secondary 28 D 20, 53 C 20, 60J45.
Annales de l’lnstitut Henri Poincaré - Physique théorique - 0246-0211 1
362 V. A. KAIMANOVICH
0. INTRODUCTION
Let M be a
simply
connectednegatively
curvedmanifold,
aM - itssphere
atinfinity.
Then every infinitegeodesic ~
on M has twoendpoints
§± = and, conversely,
everypair
of distinctpoints
determines an infinite
geodesic ~
on M.Thus there exists a natural one-to-one
correspondence
between the Radon invariant measures of thegeodesic
flow on the unit tangent bundle SM(the
measures on the space ofparametrized geodesics
invariant with respectto the shift
along geodesics)
and the Radon measures ona2
M(the
measures on the
pairs
of theendpoints
ofgeodesics,
i. e. the measures onthe space of
non-parametrized geodesics).
If N is anegatively
curvedmanifold with the fundamental group
(N),
and M its universalcovering
space, then Radon invariant measures of thegeodesic
flow onSN
correspond
to those invariant measures of thegeodesic
flow onSM,
which are also G-invariant. Hence we get acorrespondence
betweeninvariant Radon measures of the
geodesic
flow on SN and G-invariant Radon measures ona2
M.Thus,
in order to obtain an invariant measure of thegeodesic
flow onSN,
one canproceed
in thefollowing
way. Take aquasi-invariant (with
respect toG)
finite measure v on aM. If there exists a functionf
on a2 Msuch that the measure
is G-invariant
(i. e.
the square of theRadon-Nikodym cocycle
of themeasure v is
cohomological
tozero),
then we get an invariant measure of thegeodesic
flow on SN. Forexample,
let N be a manifold of dimension(~+1)
with the constant sectional curvature -1. Then M is thehyperbolic (d + I)-space
and aM is thed-sphere.
Fix apoint
x ~ M and take thevisibility Lebesgue measure 03BBx
on aM: for a set A c aM itsmeasure Àx (A)
is the solid
angle
under which A can be seen from x. Then the measurewhere ! ~ _ 2014 ~+ L
is theangle
between thepoints ~ _ and ç
+ as seen from thepoint
x, is invariant with respect to the group of the isometries of M andcorresponds
to the natural Riemannian invariant measure of thegeodesic
flow on SM. This idea has beenextensively
used in[PI, P2, S2]
(see
also[Sl])
forstudying
invariant measures of thegeodesic
flow onnon-compact manifolds with constant
negative
curvature(in
this case thedimension d is
replaced
with the conformal dimension8).
Here we
apply
thisapproach
toarbitrary negatively
curved manifolds.In this case the
theory
is non-trivial even for compact manifolds N.Indeed,
in. the constant curvature case there exists
only
one natural measure typeAnnales oe l’Institut Henri Poincaré - Physique théorique
on the
boundary
aM(M
is the universalcovering
space ofN),
whereas ingeneral
situation we get three different measure types on aM(coinciding
for the constant
curvature):
thevisibility
type(obtained
as theimage
onlM of the
Lebesgue
measure type on the1-sphere
in the tangent space ofa certain
point x E M),
the harmonictype - the
type of thehitting
distribu-tions on aM of the Brownian motion on
M,
and the Patterson measuretype - the
type of the limits(as s
tends to the criticalvalue)
of theprobability
measures on M obtainedby norming
the measureswhere the sum is taken over all
elements g
of the fundamental group and dist is the Riemannian distance on M. The Riemannian invariant measure of thegeodesic
flowcorresponds
toonly
one of thesetypes - the visibility
type.For all these three cases the
corresponding
invariant measure of thegeodesic
flow on SN can be obtainedby
the formula(0.1) using
differentweights f
Fix apoint
x E M and take in each measure class on aM themeasure
corresponding
to thispoint (visibility
measure as seen from x, harmonic distribution with thestarting point
x, the Patterson measurewith the reference
point x, respectively).
Then it will be natural to consider theweights f
as functions on x like in the formula(0.2).
Theseweights
can be obtained as the limits
where
~.-~_~+-~+
and p is a(symmetric)
function on M.Namely,
for the
visibility
measures one should takethe determinant of the differential of the
exponential
map expx evaluated at thepoint exp-1x 1 ty) (I
owe this remark to J.-P.Otal);
for the harmonicmeasures
where G is the Green kernel of the Brownian motion on
M,
and for the Patterson measureswhere v is the
growth
of M(i.
e. the critical exponent of the Poincare series involved in the definition of the Pattersonmeasure).
All theseweights
can be considered asanalogues
of theweight (0.2),
with whichthey
coincide in the constant curvature case.Comparing
with the formula(0.2)
we see that theweights arising
fromthe formulas
(0.5), (0.6), (0.7)
should beuniformly equivalent
to the powers of certain metrics on ~M. Thecorresponding
metric for thevisibility weight
364 V. A. KAIMANOVICH
coincides with the
visibility metric,
whereas the metriccorresponding
tothe
weight (0.7)
can be written aswhere
/~_, ~+)==Hs
definedby
the conditiondist (~ _ (~), ~+ (t»= 1 (we identify here
with thecorresponding geodesic
rays issued fromx)
andE is a
sufficiently
small constant(introduced
in order tosatisfy
thetriangle inequality).
Remark that it would beinteresting
toidentify
the metriccorresponding
to the harmonicweight.
The metric
(0.8)
on aM turns out to be natural for thecorrespondence
between the invariant measures of the
geodesic
flow and the measures ona2 M. Particularly,
the metric entropy of thegeodesic
flow coincides(up
toa constant
multiplier)
with the Hausdorff dimension of thecorresponding
measure on
a2 M
withrespect
to theproduct
metric obtained from the metric(0.7).
On the otherhand,
this metric is also convenient for the estimations of the dimension of the harmonic measure type on aM .Indeed,
in the case when M is the universal
covering
space of a compact manifold(0.8)
dim =(l/E)
h(M) jl (M),
where dim is the Hausdorff dimension of the harmonic measure type with
respect
to the metric(0.8), h (M)
is the entropy of the Brownian motionon M defined in
[K]
andl (M)
is the rate of escape of the Brownian motion(cf. [L1], [K]) - this
is ananalogue
of a well knownLedrappier
formula from the
theory
of smoothdynamical
systems. Hence theproblem
of the interrelations of three different measure types on aM
(essentially
solved in
[L2], [L3])
can beexpressed
also in terms of the dimensions of thecorresponding
measure types with respect to the metric(0.8).
For theauthor this consideration was a
leading
reason forintroducing
this metric.Remark that this metric seems also more natural for the estimations of the Hausdorff dimension of the harmonic measure class for
arbitrary simply
connectednegatively
curved manifolds.Namely,
the estimates for the Hausdorff dimension can be obtained from the formula(0.9)
and theestimates for the entropy and the rate of escape
(ef [Ki], [KL]).
This paper was conceived
simultaneously
with the paper[K],
but unfor-tunately
could not beprepared
in that time.Recently
thereappeared
anumber of papers devoted to the related
problems
for the cocompact case.Mention the papers
by Ledrappier [L2], [L3]
devoted to construction of the harmonic invariant measure of thegeodesic
flow and the interrelations between three measure types and the papersby
Hamenstadt([H 1], [H2], [H3])
whereshe, particularly, identify
the maximal entropymeasure type on aM with the Hausdorff measure
corresponding
to ametric on aM similar to our metric
(0.8).
Our aim here is to describe a new
approach
to the construction of the invariant measures of thegeodesic
flow. So we don’t discuss here in detailsAnnales de l’lnstitut Henri Poincaré - Physique théorique
the
ergodic properties
of the measures obtained in this way ingeneral
situation
(for
non-compactmanifolds),
theseproperties
in the compactcase
being already
proven in the cited above papersby
Hamenstadt andLedrappier.
We shall return to theseproblems
elsewhere. Remark that thisapproach
can be also used forstudying
the invariant measures of thegeodesic
flow onhyperbolic
groups, whereonly
a definition of thegeodesic
flow
"up
to aquasification"
is known[G],
whereas invariant measures on the square of thehyperbolic boundary
can be defined without anyquasification.
The structure of the paper is the
following.
In Section 1 we
give
necessary facts and proveauxiliary
statementsabout the
negatively
curvedsimply
connected Riemannian manifolds.Particularly,
we define the metricsp~
on theboundary
aM(Section 1.3)
and show that the function
lx
onparticipating
in the definition of this metric has a cleargeometric meaning (Proposition 1.4).
In Section 2 we state a natural
correspondence
between the invariant(a-finite)
measures of thegeodesic
flow on asimply
connectednegatively
curved manifold M and the
(a-finite)
measures on a2 M("at
the square ofinfinity") -
Theorems2.1,
2.2. For the case of manifolds with compactquotients (i. e.
universalcovering
spaces of compactnegatively
curvedmanifolds)
we prove that the entropy of thegeodesic
flow case coincides(up
to a constantmultiplier)
with the dimension of thecorresponding
measure on a2 M with respect to the metric introduced in the Section 1
(Theorems 2.3, 2.4).
In Section 3 we consider the case when our manifold M has a compact
quotient
N and construct a measure class atinfinity having
the maximal dimension with respect to the metricsp~
on aM introduced in Section 1.Actually
we construct a measure which is ananalogue
of the Pattersonmeasure well known in the constant curvature case
([P2], [S2]). Then, taking
the square of this measure on a2 M andmultiplying
itby
theweight (0.7),
we get a Radon measure invariant with respect to the action of the fundamentalgroup xi (N)= G
and hence an invariant measure of thegeodesic
flow on SN.Calculating
its entropyusing
the Theorem 2.4 proves that this measure isreally
the maximal entropy measure of thegeodesic
flow. This
gives
yet another construction of the maximal entropy measure(the Bowen-Margulis measure)
for thegeodesic
flow onnegatively
curvedcompact manifolds
(cf [Bl], [Ml], [HI]).
Ourexposition
hereclosely
fol-lows the paper
[S2] by
D. Sullivan. For the sake ofsimplicity
we considerhere
only
the compactquotient
case, but thisapproach
can be alsoapplied
in the
general
situation.In Section 4 we construct an invariant measure of the
geodesic
flowon a
negatively
curved manifold N with the harmonic type conditional distributions on aM(M-universal covering
space ofN).
For the compact366 V. A. KAIMANOVICH
case the
Ledrappier’s
construction[L2]
uses the Holdercontinuity
of theGreen kernel of the Brownian motion and
strongly
relies upon thetheory
of the Gibbs measures for Anosov flows on compact manifolds. Later another and more
straightforward
construction of the harmonic invariantmeasure has been
proposed by
Hamenstadt[H3],
but alsousing
anergodic theory approach
andstrongly dependent
on the compactness of N. Our idea is based upon a directprobabilistic approach
androughly speaking
wesimply
substitute every two-sided Brownianpath
with thecorresponding geodesic joining
the limitpoints
of thispath
at 2014~ and at +00.So, excluding
the time shift(exactly
the same trick as with the invariantmeasures of the
geodesic
flow in Section2)
we get from the a-finitemeasure in the space of two-sided Brownian
paths
with one-dimensional distribution m(the
Riemannian volume onM)
a certain natural Radonmeasure
on a2
Mbelonging
to the square of the harmonic measure classon aM
(Theorem 4.1).
This construction isgeneral
and can beapplied
toany
simply
connectednegatively
curved manifold with theuniformly
bounded sectional curvatures. The obtained measure on a2 M is invariant with respect to the group of isometries of
M,
so thatby
Theorem 2.2 weget a
locally
finite invariant measure of thegeodesic
flow on anyquotient
of M.
Particularly,
for the manifolds with a compactquotient
we getexactly
the harmonic invariant measure constructed in[L2], [H3].
Remarkthat this measure can be also obtained
directly
from the harmonic measureson aM
using
theweight (0.6) - the
Nairn kernel of the Brownian motionon M
([Kol], [Ko2]).
ACKNOWLEDGEMENTS
I would like to thank the
organizers
of the conference"Hyperbolic
behavour of
dynamical systems"
for their invitation toparticipate,
andthe Universities Paris Sud
(Orsay)
and Paris-VI for their supportduring
my stay in Paris. Discussions with Alain Ancona
(who, particularly, pointed
out to me the papers[Kol], [Ko2]),
UrsulaHamenstadt, Francois Ledrappier
and Jean-Pierre Otal were very useful.This article was written down
during
my stay at the Universities of Warwick andEdinburgh.
It is apleasure
toacknowledge
mygratitude
toDavid
Elworthy
andTerry Lyons
for their warmhospitality.
Annales clo l’Institut Henri Poincaré - Physique théorique
1. NEGATIVELY CURVED BACKGROUND
1.1.
Sphere
atinfinity
Let M be a
simply
connectednegatively
curved Riemannian manifold(Cartan-Hadamard manifold)
with thepinched
sectional curvatures:As it is well
known,
for anypoint
x E M theexponential
map is adiffeomorphism
between the tangent spaceTx
M and the manifold M.By
dist we shall
always
denote the Riemannian distance on M.Say
that twogeodesic
rays on M areasymptotic
ifthey
lie within a bounded distanceone from the other and denote
by
aM the spaceof asymptotic
classesof geodesic
rays on M([BGS], [EO’N]).
For anypoint
y E 8M and any x E M there exists aunique geodesic
raystarting
from x andbelonging
to theclass y. We shall denote this ray
(x, y). By (y _ , y + )
denote theunique
infinite
geodesic belonging
to the classy - E aM
at - oo and to the class y+ at + oo.The
"sphere
atinfinity"
aM can be considered as theboundary
of Min the
visibility compactification
M - = M U 8M: a sequence(tending
toinfinity) Xn EM
is convergent in M - iff for a certain referencepoint
x ~ M the directions of the vectors
(xn)
inTx M
converge(this compactification
doesn’tdepend
on the choice of the referencepoint x).
The
resulting topology
on 9M is definedby
the coneneighbourhoods
where
Lx (y, y’)
is theangle
between thedirecting
vectors of thegeodesics (x, y)
and(x, y’)
in the tangent spaceTx M,
i. e. theangle
between thepoints
y andy’
as seen from thepoint
x E M[EO’N].
Every
linearelement ~
from the unit tangent bundle SM can be identified with the two-sided infinitegeodesic
issuedfrom ç
and endowed with theduly parametrization. Taking
theendpoints
of thisgeodesic
on ~M at+ oo and at - oo we get the maps
from SM to aM. Denote
by ~x
the restrictions of these maps toS~ M,
which are
homeomorphisms
ofSx M
and aM.Denote
by
a2 M the space 3M xlmEdiag = {(y l’ Y2):
Y 1 =I-yz}
endowed with natural
locally
compacttopology.
This space coincides with the space of all infinitegeodesics
on M(considered
as subsets ofM,
368 V. A. KAIMANOVICH
without any
parametrization)
with the usualpointwise
convergencetopol-
ogy.
Adding
the naturalparametrization along geodesics
we get the fibra- tionof SM over a2 M with the fibres R.
Slightly abusing
we shallspeak
belowabout the measures on the space a2 M as about the "measures at the square
of infinity ",
the measures on ~Mbeing
the "measures atinfinity ".
1.2.
Divergence
ofgeodesics
Below we shall use the
following
statement.ALEKSANDROV TRIANGLE COMPARISON THEOREM
[AI]. -
Let M and M’ betwo Cartan-Hadamard
mani~f’olds
with theseparated
sectional curvatures, i. e. there exists a constant 0 such thatK __
K’ _ 0for
allsectional curvatures K and K’ in
manifolds
M andM’, respectively.
Let thepoints
x; E M andx~
E M’~i = 0, 1, 2) satisfy
the conditionwhere dist and dist’ are the Riemannian metrics on M and
M’, respectively.
If
thepoints
pi andpi (i =1, 2) belong
to thegeodesic
segments(xo, xi)
andxi), respectively,
andsatisfy
the conditionthen
Let a
and P
be twogeodesic
rays with commonorigin
andComparing
M with thehyperbolic plane
with theconstant
curvature - a2
andusing
thehyperbolic
sine theorem one getsthat ’
whenever
0 _ t’
t. From theinequality (1.8)
followsPROPOSITION 1.1. - There exists a constant c
depending
on the upperbound - a2
of
the curvature on Monly,
suchthat for
any twogeodesic
rays03B1 and
03B2
with commonorigin
where t is
(uniquely)
determinedby
the relationAnnales de l’lnstitut Henri Poincaré - Physique théorique
1.3. Metric on the
boundary
For any reference
point
x~M define the functionlx
on a2 Mby
therelation
where rti are the
geodesic
rays(x, y;).
Theneighbourhoods
arising
from the function I have thefollowing simple geometrical
sense.Take the intersection of the 1-ball centered at the
point oc (t)
of thegeodesic
ray a =
(x, y)
with thet-sphere
centered at x. Then(y)
is the "shadow"of this intersection on aM if the
light
propagates from a source at thepoint
x.From the
comparison
with the constant curvature case follows that there exist constantsA,
B > 0depending
on the curvature bounds -a2,
- b2
only
such thatHence for every
point
XEM theneighbourhoods
determine thevisibility topology
on ~M.For any reference
point x
e M and E > 0 letPROPOSITION 1.2. - There exists Eo > 0
(depending
on the upper bound- a2
of
the curvature on Monly)
such thatp~
is a metric on the space aMfor
all E Eo and x E M. Thetopology
on ~M determinedby
any metricp~
coincides with the
visibility topology.
For the same valueof E
the metricsp~
and
p~ corresponding
todifferent points
x, y E M areuni.f’ormly equivalent,
i. e. 1
IC C for
a certain constant C = C(E,
x,y).
Proof -
Coincidence of thetopologies (and
even the Holderequiva-
lence of the
visibility
metric on aM andp~)
follows from the formula( 1.13).
The uniformequivalence
is acorollary
of theProposition
1.4 below.Hence we need to prove
only
thetriangle inequality.
Denoteby
ai thegeodesic
rays(x, yi) corresponding
to thepoints
~yL E aM(i =
1,2, 3)
andlet
03B3j). Suppose l13 = min{lij:
1 _ ij 3}.
Then from theProposition
1.1370 V. A. KAIMANOVICH
whence we get the desired
triangle inequality
for all E _- Eo = c.Remarks. - 1. In the definition of the metrics
pE
one could take anarbitrary
radius r instead Theresulting
metrics areuniformly equivalent
topE - see
Section 1.6 below.2. We didn’t try to find the best
possible
estimate for Eo in terms of the curvature bounds. U. Hamenstadt[HI]
has defined ananalogous
metric on the
punctured
spaceconsidering
the infinitegeodesics
issued from yo instead of the
geodesic
rays issued from apoint
x E M. Inthis case the
triangle inequality
for thecorresponding
metric is satisfiedfor
all ~ ~
a.1.4. The Busemann
cocycles
For any
point
y E aM introduce the Busemannfunction
on M[BGS]
where tr is the
geodesic
ray(xo, y) connecting
a fixed referencepoint xo e M
with y. This function is defined up to a constantdepending
on thereference
point
xo, so it will be more convenient tospeak
about theBusemann
cocycles
on Massociated with the
points
ye aM. The level sets of the Busemann functionsare the
horospheres
on M centered at y, so thatBy (x, y)
is thesigned
distance between the
horospheres passing through
thepoints x and y
andcentered at y. In other
words, By (x, y)
can be considered as a"regulariza-
tion" of the formal
expression dist (x, y) - dist (y, y)
with ybeing
a"point
at
infinity".
For any
point
x E aM define thefollowing
functionf!4 x
on a2 M:where y belongs
to thegeodesic (Y1, y~).
It is clear that theright-hand
side of the formula
( 1.18)
doesn’tdepend
on the choiceof y.
In otherwords, y2)
is thelength
of the segment cut out on thegeodesic 12) by
thehorospheres passing through
x and centered at Y1 and Y2.This function can be considered as a
"regularization"
of theexpression
with yl, y2
being points
atinfinity.
When x varies the values ofsatisfy
the
identity
Annales de l’lnstitut Henri Poincaré - Physique théorique
Hence we have
PROPOSITION 1.3. - The square
of
the Busemanncocycle
on anynegatively
curved
simply
connectedmani, f ’old
iscohomological
to zero.Remark. - The "cross Y2, Y3, on ~M introduced
by
Otal
[0]
as aregularization
of theexpression
Y 3) (1.21)
can be written in terms of the functions as
with the
right-hand
side of the formula(1.22) being independent
on x.1.5.
Negatively
curved manifold as ahyperbolic
metric space The Cartan-Hadamard manifolds with the bounded away from zerocurvature are a
particular
case ofhyperbolic
metric spaces and the notions of theboundary
aM and thecompactification
M - can be also defined inthis more
general
context([G], [GH], [CDP]).
For any reference
point
xeM the Gromovproduct
satisfies the ð-ultrametric
inequality
for a certain constant b
depending
on the upper bound - al of the sectional curvature on Monly.
The ultrametric
inequality ( 1.24)
isequivalent
to thefollowing
property, which we shall use in thesequel.
For anygeodesic triangle
with the vertices xl, x2, x~ eM take thepoints
pl, p2, p3 on the sides of thistriangle
insuch a way that for every
vertex
the distances to thepoints Pj lying
on thesides of the
triangle adjacent to xi
areequal,
i. e.pl)
= dist(xl, p3),
dist
(Xl’ Pl)
= dist(Xl’ pl),
dist(X3’ P3)
= dist(X3’ Pl) (we
assume~+1)).
We shall say that thetriangle (P1’
p2,p3)
is the innertriangle
of the initial
triangle (xl,
x2,x3).
Then there exists an absolute constant D such thati. e. the diameter
of
the innertriangle
is less than D. This statement remains true for thetriangles
with one, two or three verticesbelonging
to the372 V. A. KAIMANOVICH
boundary
aM. In this case instead of the conditiondist(y, pl)
= dist(y, p2)
with
y E aM
one should take its"regularization" Py(~i,~2)=0-
A sequence of
points Xn E M
converges in thevisibility topology
iff(xn I xm)x
tends toinfinity
as n, m oo for a certain(or, equivalently,
forevery)
referencepoint
x. Theboundary
aM can be identified with the space of theequivalence
classes of convergent sequences with respect to theequivalence
relation{~J ~ ~yn~ ~ (xn ~
Thevisibility topol-
ogy on aM coincides with the
"hyperbolic topology"
definedby
theneighbourhoods
where
and a
(resp., a’)
is thegeodesic
ray(x, y) [resp., (x, y’)].
One caneasily
see that
actually
where
£3~
is the function on a2 M introduces in Section 1.4.A metric
equivalent
toP~
from Section 1.3 also can be defined in the context ofarbitrary hyperbolic
metric spaces.Namely,
if X is ahyperbolic
metric space with the
hyperbolicity
constant8,
then for every E _ Eo(with
Eo
depending
on ðonly)
there exists ametric dE
on thehyperbolic boundary
3X
uniformly equivalent
toPe(Yl’ I Yl»’
whereI Y2)
is the Gromov
product
on 3X[GH].
1.6.
Comparison
of functionson a2
MIntroduce the last function on a2 M - the distance
dx (y l’ Y2)
from apoint
x E M to thegeodesic (Yl’ Y2)
and prove that all the three functionslx (Y 1, Y2) (Section 1. 3), (’)’1 Y2) (Sections 1.4, 1. 5)
andY2)
areessentially
coincident.PROPOSITION 1.4. - There exists a constant C
depending
on the curvaturebounds - a2, - b2
on themanifold
Monly,
such thatfor
all x E M and’)’1’
03B32 ~ ~M
thedifference
between any twoof
thequantities Y2),
(Yi ! ’Y2)
anddx (Y1, Y2)
doesn’t exceed C.Proof. -
Consider thegeodesic triangle (x,
yi,y2)
and its innertriangle
hence
Annales clo l’Institut Henri Poincaré - Physique théorique
where D is the constant from the
inequality (1.25).
The
quantity Y2) = l
is definedby
the condition = dist(al (j, (I)
= 1 with ai =(x, yi).
At the same timey2)x)
= dist(pl, p2) __
D.Hence from the Aleksandrov
comparison
theorem follows that for a certain constantC,
We have to prove now that
lx (Y1, Y2)
can’t besubstantially larger
thandx (y l’ 72)’ Let q
be thepoint
on thegeodesic (yi, Y2)
nearest to x. Then in thetriangle (x,
q, theangle
at thevertex q equals x/2,
hence all thevertices of the
corresponding
innertriangle
are close to q.Particularly,
the distance from the
point q
to the ray(x, Y 1) [as
well as to the ray(x, Y2)]
is bounded. Take the
points Yi)
such thatdist (x, Y2),
sothat
dist (q1’ ~2)~ 1-
Then the distance from thepoints
to thegeodesic (yi, Y2) is
also bounded. Hence iflx (yl, Y2)
issubstantially larger
thany2),
the short cut from y 1 to Y2going through
thepoints
piand
p2 is shorter than(y l’ Y2),
which isimpossible.
This argument can beeasily
made constructive
providing
a constant K such thatwhich in combination with the
inequalities (1.29)
and(1.30) gives
thedesired result.
2. INVARIANT MEASURES OF THE GEODESIC FLOW AND THE MEASURES "AT THE
SQUARE
OF INFINITY"2.1. General
correspondence
THEOREM 2. I. - Let M be a
simply
connectednegatively
curvedmanifold
with the
pinched
sectional curvatures: -K -_ -
a2(0
a _b).
Thenthere exists a natural convex
isomorphism
between the conesof
the Radoninvariant measures
of
thegeodesic flow
on SM and the Radon measures onalM.
Proo, f : -
Let A be a Radon measure ona 2 M,
i. e. a measure on the space of ends ofgeodesics
in M.Integrating
it with respect to theLebesgue
measure
along
thegeodesics (i.
e.lifting
it to SMusing
the fibrationx : SM ~
aM)
we get an invariant measure of thegeodesic
flow on SM.The measure X is
Radon,
since for any compact subset of SM itsimage
in a2 M is also compact as it follows from the results of Section 1.
Conversely,
let À be an invariant measure of thegeodesic
flow.Now,
in order to obtain A we have to
disintegrate
the measure Xexcluding
the374 V. A. KAIMANOVICH
action of the
geodesic
flow(the
shiftalong
thegeodesics
inM).
Let K bea compact subset of a2 M. Take the set
and consider the
dissipative decomposition
where the sets
Kn
are(mod 0) disjoint
andKn
= TnKo (T
is thegeodesic flow).
Now putIt is clear that the value of À
(Ko)
doesn’tdepend
on thedecomposition (2.2)
and that A can be extended to a measure on a2 M. We have to proveonly
thatA (K)
is finite for any compact set K c a2 M. As it follows from the results of Section1,
for any compact K c ~2 M there exists a compactset A c M such that every
geodesic
with the ends from K intersects theset A. Now we can take the
decomposition (2.2)
withwhere
is the time of the first intersection of the
geodesic ~
with the set A. Theset
Ko
has a compact closure inSM,
hence A(K)
is finite and A is Radon.If M is the universal
covering
space of anegatively
curved manifoldN,
then the invariant measures of the
geodesic
flow on SN are in naturalone-to-one
correspondence
with those invariant measures of thegeodesic
flow on SM which are also invariant with respect to the action of the fundamental group ~
(N).
Hence we get thefollowing
result.THEOREM 2.2. - Let N be a
negatively
curvedmanifold
with thepinched
sectional curvatures and M be its universal
covering manifold.
Then thereexists a natural convex
isomorphism
between the conesof the
Radon invariantmeasures
of
thegeodesic flow
on SN and the Radon measures on a2 M invariant with respect to the actionof
thefundamental
group ~cl(N).
Particu-larly,
in the case when N is compact we have anisomorphism
between thecones
of finite
invariant measuresof
thegeodesic flow
on SN andof
the1tl
(N)-invariant
Radon measures on a 2 M.Remarks. - 1. The
correspondence
constructed in the Theorem 2.2 is convex, hence it preserves theergodicity. Namely, ergodic
invariant meas-ures of the
geodesic
flow on SN are incorrespondence
withergodic (with
respect to the groupaction)
G-invariant measures on a2 M.de l’Institut Henri Poincaré - Physique théorique
2. For the more
general
situation ofarbitrary hyperbolic
metric spacesonly
a definition of thegeodesic
flow"up
to aquasification" given
in[G]
is known. Nonetheless our
approach permits
one to consider the measures on the square of thehyperbolic boundary (defined
in canonical way without anyquasification)
as natural counterparts of invariant measuresof any
reasonably
definedgeodesic
flow. It would beespecially interesting
to
study
theergodic properties
of group invariant a-finite measures onthe square of the
boundary
ofhyperbolic
groups. Ourapproach
forconstructing
the maximal entropy measure and the harmonic measure for thegeodesic
flow on Riemanniannegatively
curved manifolds can be alsoapplied
in this situation(see
below Sections 3 and4, respectively).
2.2. Measures and measure classes at
infinity
Introduce now several measures and measure classes connected with the invariant measures of the
geodesic
flow(and
with thecorresponding
measures "at the square of
infinity").
Let À be an invariant Radon measureof the
geodesic
flow on SM and A thecorresponding
Radon measureon 81 M.
We can take an
arbitrary
finite measure v on SMequivalent
to À andthen
apply
to v themaps x+
and 7r’. Denote the types of theresulting
measures
(which
areindependent
on the choiceof v)
as À + and~’, respectively.
Further, fixing
one of the coordinates(y _ , y + )
one can define for any y E aM the conditional measuresA~
andA;
of the measure A with respectto the conditions y _ = y and y + = y. Since the measure A is
a-finite,
these conditional measures are definedonly
up to a constantmultiplier.
Onecan
easily
see thatactually they
can be identified with the conditionalmeasures on the strong stable and strong unstable
horospheres
of thegeodesic
flow. The measuresA; (resp.,
aren’tmutually equivalent
ingeneral situation,
but theprojection
of a certain finite measureequivalent
to A onto the second and the first coordinates in a2
M, respectively, gives
the measure classes A + and
A’,
which coincide with the measure classes À + and~’, respectively.
Remark that if À is an invariant measure of the
geodesic flow,
then thereflected
measure03BB^
obtained from Xusing
themap 03BE ~ - 03BE
on SM isalso invariant. The measure
A
oncorresponding to ~
can beobtained from the measure A
corresponding
to Àby reversing
the orderof the coordinates on al M. For the reflected
measures
andA~
themeasures and measure classes introduced above can be obtained from the