A NNALI DELLA
S CUOLA N ORMALE S UPERIORE DI P ISA Classe di Scienze
J. J. L. V ELÁZQUEZ
Curvature blow-up in perturbations of minimal cones evolving by mean curvature flow
Annali della Scuola Normale Superiore di Pisa, Classe di Scienze 4
esérie, tome 21, n
o4 (1994), p. 595-628
<http://www.numdam.org/item?id=ASNSP_1994_4_21_4_595_0>
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Evolving by Mean Curvature Flow(*)
J.J.L.
VELÁZQUEZ
1. - Introduction
A smooth one-parameter
family
ofhypersurfaces, IT(t)l
cJRn+1
where0 t T +oo is said to evolve
by
its mean curvature if the normalvelocity VN(P)
at anypoint
P Er(t)
coincides with the mean curvature ofr(t)
atP, i.e.,
where H denotes the mean curvature of the
hypersurface r(t). Properties
of meancurvature flows
(MCF)
have beenextensively analysed,
and in recent years great attention has beenpaid
todeveloping
various theories ofgeneralized
solutions for(1.1).
Forinstance,
in the seminal workby
Brakke[B],
atheory
ofgeneralized
solutions was introduced for varifolds in
JRn+1
ofarbitrary codimension,
whichsatisfy
a weak formulation of(1.1).
Inparticular,
existence of at least one suchglobal
solution forarbitrary
initial data wasproved
there. It was also shown in[B] ]
that such solutions can benonunique.
In the case where n = 1, a
theory
ofgeneralized
solutions for curveshortening
on surfaces has beendeveloped
in[Al], [A2].
Another method to obtaingeneralized
solutions can be found in[AG].
In thehigher
dimensionalcase n > 1, an
approach
has beendeveloped
in[CGG]
and[ES]
which isbased on the
theory
ofviscosity
solutions for nonlinearelliptic
andparabolic equations.
In theseworks,
the so-called level setequation
in considered. This is ahighly degenerate parabolic equation
which arises when the level sets ofa function evolve
by
MCF. Thetheory
in[CGG]
and[ES] yields
existenceand
uniqueness
ofgeneralized
solutions for the level setequation
and alarge
class of initial values. Another weak formulation based on a
singular
limit of a~*~ Partially supported by CICYT Grant PB90-0235 and NATO Grant CRG 920196.
Pervenuto alla Redazione il 2 Agosto 1993.
reaction diffusion
equation
of the typehas been
proposed by
DeGiorgi ([DG]).
We refer to[ESS]
for a discussion of the relations between thisapproach
and thosepreviously
discussed. Wefinally
refer to another
theory
ofgeneralized
solutions of MCF that have beensuggested
in
[S].
A
question
which has deserved much attention is that of blow up,i.e.,
thedescription
of thepossible singularities
that smoothhypersurfaces
maydevelop
as
they
evolveby
mean curvature flow. One is then led todistinguish
betweenfast and slow blow up. Let a =
(ai,j)
be the second fundamental form of thehypersurface,
and letIf at a
particular
time t = T oo the evolution ofr(t)
cannot be continuedsmoothly,
then limA(t)
= oo(cf. [A4]
fordetails).
Twopossibilities
then arise.Either tTT
or
when
(1.2)
holds(resp.
when(1.3)
issatisfied)
we shall say that the solution exhibits fast blow up(resp.
slow blowup).
The fast blow up case has been consideredby
Huiskens in[H].
The author proves there thefollowing
result.For x E
r(t)
and P Er(t),
let us writeThen the rescaled
hypersurfaces
converge
sequentially (i.e.,
up to the choice of a suitablesubsequence {Tn }
withlim Tn =
oo)
to a self-similarsolution,
which ishypersurface
of the formn-~oo
where r* is a
hypersurface
inJRn+1.
One often refers to this fact in anabridged
way
by saying
that when fast blow up occurs, the behaviour near asingularity
is
(sequentially)
self-similar.When the slow blow up case
(1.4) holds,
one has thefollowing
situation(cf. [A4]).
For x er(t),
P Er(t)
and to T with-toA(to)-2
t(T - to)A(to)-2
andA(t) given
in(1.2),
we definewhere
Then there exist sequences
{tn }, {Pn }
with n-ioolim tn
= T andPn
Er(tn),
and asubsequence
such that:(1.6)
Thefamily r’j(t)
- converges to afamily of hypersurfaces
-oo t oo, whose curvatures are
uniformly
bounded. Such afamily
iscalled an eternal solution in the
terminology
of[A4].
This eternal solution satisfieswhere a = is the
corresponding
second fundamental form.In this paper, we shall describe a slow blow up mechanism for MCF.
Consider the Simons cone
(cf. [G], [S])
which has dimension d = 2n - 1. It has been
proved by Bombieri,
DeGiorgi
and Giusti in
[BGG]
thatCn
is aglobally minimizing
surface for n > 4. We shall prove here thefollowing:
THEOREM. Let n > 4. For T > 0 small
enough
there exists afamily of surfaces {r(t)},
0 t T,of
dimension d = 2n - 1 which evolveby
MCFand is such
that, as t T T, it
blows upslowly
towards asurface r(t)
which behavesasymptotically
as the Simons coneas lxl
- 0. Moreover, there exists asmooth minimal
surface
M and apositive
such that(T - approaches
to M ast T T, uniformly
on compact sets.As a matter of
fact, precise
estimates are obtained on theasymptotics
of the
family {r(t)}
ast T T.
The reader is referred to the next Section(cf.
in
particular Proposition
2.1 and Theorems 2.2 and 2.3therein)
for a detailedstatement of such results.
We shall conclude this Introduction
by remarking
on the relation between this Theorem and other known blow up results for MCF. The structure ofsingularities
is well-known for the case of convexhypersurfaces,
a situation in which there isalways
fast blow up(cf. (1.3))
and the limit surface is asphere (cf. [Hu], [GH]).
For embeddedplane
curves there isalways
evolution to aconvex curve before
collapse
to a roundpoint
occurs(cf. [Gr]).
For immersedcurves, both fast and slow blow up can
actually
occur(cf.
for instance[A4]
for a recent
survey). Finally,
forrotationally symmetric
surfaces one mayagain
have slow or fast blow up, and near the
singularities
there is convergence to self-similarspheres
orcylinders (cf. [AIAG]).
We should
point
out here that the structure ofsingularities
which arise in MCF isstrikingly
similar to thoseappearing
in the semilinear heatequation
It is well known that solutions of
(1.8)
may blow up in a finitetime, say t
= T.If x = 0 is a blow up
point
for(1.8),
it wasproved
in[GK 1 ] that,
under the additionalhypotheses
one then has that the rescaled function
converges
uniformly
forbounded I y I
towards a constant (Do, whereIt was
proved
in[GK2]
that(1.9a)
holds if(1.9b)
holds. The case 0was then ruled out in
[GK3];
see also[GP]
for anindependent proof
of theone dimensional case N = 1. We will say that a solution
v(x, t)
of(1.8)
isself-similar if it has the form
in such a case, 0 satisfies
and from the
arguments
in[GK 1 ]
itreadily
followsthat,
if(1.9a)
isassumed,
function in(1.10)
convergessequentially
to a bounded solution of(1.12).
When
(1.9b)
alsoholds,
theonly
such solutions of(1.12)
are those in(1.11),
butfor
> N + 2
there exist nonconstant,radially symmetric
solutions of(1.12)
N - 2
(cf. [BQ], [T], [L]). Roughly speaking,
when(1.9a) holds,
blow up for(1.8)
issequentially self-similar,
a case we havealready
found tohappen
in MCF when fastblow-up
occurs. As a matter offact,
one candistinctly spot deep analogies
in the argument in
[H] (where
fast blow up for MCF wasdiscussed)
and thosein
[GKl], [GK2], [GK3],
a series of papers whichopened
the road towardsa detailed
analysis
of blow up for(1.8).
Much progress has been achieved in this direction in recent years, and the subcritical case where(1.9b)
holds isby
now well understood(cf. [Bl], [B2], [FK], [FL], [HVl], [HV2], [HV3], [HV4], [HV5], [VI], [V2], [V3]
and the review[V4]
fordetails).
Inparticular,
the final
profiles
of the solutions at blow up time can becomputed ([V2]),
the
(N - 1 )-dimensional
Hausdorff measure of the blow up set is bounded incompact
sets ifu(x, t) ~ -1)(T - t)-pl l ([V3]),
andgeneric
blow up behaviour is shown tocorrespond
tosingle- point, locally
radial blow up patterns([HV4],
[HV5]).
On the other
hand,
it wasimplicit
in the arguments in[GK2] that,
if(1.9a)
does nothold,
there should be convergence of somesubsequence
of theform
towards a
global,
bounded solutionv(x, t)
of(1.8)
which is defined for x E JRn and(an
eternalsolution),
which shouldsatisfy
= 1. This isa neat
analogue
of(1.6)
for slow blow up in MCF. It was notclear, however,
whether solutions of(1.8)
which do notsatisfy (1.9a)
couldpossibly
exists.This fact has been
recently
ascertained in[HV6],
where thefollowing
resultwas
proved:
( 1.14) If
N > 11 and then for any T > 0 there existpositive,
radial solution of(1.8)
which blow up at x = 0 and t =T,
andIn
[HV6],
aprecise description
of the blow up mechanism in(1.14)
is
provided.
Inparticular,
convergence in suitable scales towards an eternal(actually stationary)
solution of(1.8)
in an innerlayer
near x = 0 is stated(cf.
[HV7]
for a sketch of the main arguments of[HV6]).
One can wonder if related
analysis
can beproduced
for MCF. We nextbriefly
describe some recent results in this direction which are relevant to our current discussion.In
[AV 1 ],
the evolutionof rotationally symmetric
surfaces under MCF wasconsidered. The authors
analysed
a situation ofcollapsing
surfaces asdepicted
in
Figures
1 and 2 below.Figure
1.
m odd : m =
3, 5, 7, ...
Figure
2m even : m =
4, 6, 8, ...
Singularities developed correspond
to a slow blow up situation. Inparti- cular,
the size of the surfaces nearcollapse,
the formation of atravelling
wavenear the
tip
and the size of this last were obtained there.On the other
hand,
in[AV2]
thecollapse
of a convex,symmetric,
immersedloop
with one self-intersection was studied(cf. Figure 3).
Figure 3
By
the results of[A3],
it is known that the internalloop
mustcollapse
at a rate described in
(1.4). Furthermore,
it was alsoproved that,
in suitablerescaled
variables,
atraveling
wave willdevelop
near thetip
of the internalloop
as blow upproceeds.
The detailed
asymptotics
of the internalloop
near blow up(and
theprecise
size of its
tip)
were then obtained in[AV2].
Wepoint
outthat,
while[AVI], [AV2]
describecollapse
oftype (1.4),
theprecise
blow up mechanisms aredifferent in both cases, even
though they
are characterizedby
thegeneration
of a
travelling
wave near atip.
The result obtainedhere,
and described in the statement of ourprevious Theorem, corresponds yet
to another blow up structure forsingularities
oftype (1.4).
2. - Preliminaries
We shall restrict our attention to
hypersurfaces (henceforth
referred to assurfaces for
short)
which are invariant under the action ofO(n)
xO(n),
whereO(n)
denotes theorthogonal
group in R~. Let T > 0 begiven,
and for 0 t Tlet {r(t)}
be any suchfamily
of surfaces. We then define a rescaledfamily
IP(-r)}
as followsA
simple
calculation revealsthat,
if{r(t)}
evolvesby
mean curvature flow(MCF),
then{r(T)} changes according
to theequation
where
VN
is the normalvelocity,
H is the mean curvature of thesurface,
N isa normal vector at y E
r(T)
and(, )
denotes the standard scalarproduct
inFrom now on, we shall
specialize
to surfaces that can beparametrized
inthe form
under suitable
assumptions
on the mapwhich is defined for W 1, and r E
(8(r), D(,r)),
where8(r),
D(T)
will bespecified presently (cf. (2.41) below)
and T > To with Tolarge
enough. Function f,
acts as followsFor
instance,
the Simons coneis indeed invariant under the group
0(n)
xO(n),
and can beparametrized
inthe form where
which
corresponds
to(2.3c) with 1/J ==
0 there. _A routine
computation
reveals that in theregion
wherer(T)
can beparametrized
in the form(2.3),
the normal vector N to such surface isgiven by
where and the normal
velocity
isso that
The metrics at the surface is then
given by
the matrixwhere is the first fundamental form in the
sphere
Theinverse matrix
(g’>I) =
is thengiven by
where
(g°~~~) _ (g~,p)-1.
The second fundamental form ofT(T)
in this coordinate system will thus begiven by
where
(aa,j3)
is the second fundamental form of thesphere Recalling
that the mean curvature H satisfies(2.8), (2.9)
thatit follows from
where we have used the fact that
= - V2 (N - 1). Taking
into account(2.2), (2.6), (2.7)
and(2.10)
wefinally
arrive at thefollowing equation
for~(r, T) (cf. (2.3c))
We shall also make use of a different
parametrization
for the kind of surfaces that we areconsidering
here.By
symmetry, any such surface is determinedby
its intersection with theplane (XI, Xn+1).
Forconvenience,
we shall writeXn+1 = v, xl = u, and assume that the surfaces
IF(t)l
may be describedby
for some smooth
enough
functionQ
such thatSince the
arguments
to bepresented
are of a local nature, we shallonly
need(2.12)
to hold for u smallenough.
In the rest of thisSection, however,
we will continue to make use of(2.12)
as stated above for the sake ofsimplicity.
Wethen can
parametrize
the surfacer(t) by
means of a functionh(U,W1,w2,t)
inthe form
We
readily
check that one now has thefollowing
formulae for normal vector, normalvelocity,
the inverse of the metrics matrix and the second fundamentalform
respectively
where
(a~,,~)
is as in(2.9)
andFrom
(2.16), (2.17)
we deduce thatwhereas
(2.13)
and(2.14) yield
We next turn our attention to
equation (2.11).
If weformally
linearize in theright-hand
sidethere,
we obtain the differentialoperator
which will
play
an essential role in what follows. A similaroperator
has beenthroughly analysed
in[HV5];
we shall therefore refer to that paper for detailsconcerning
theproperties
of A in(2.20)
which will be listed below. As in[HV5],
we define suitableweighted
spaces in thefollowing
formI
and
for
It is
readily
seen that(resp.
can be endowed with a Hilbert space structurecorresponding to
the scalarproduct
We are now
prepared
to describethe basic
spectral properties of operator
A. These are collected in thefollowing
PROPOSITION 2.1. Let n > 4. The operator A in
(2.20)
can then be extended in aunique
way to aself-adjoint
operator(also
denotedby A)
which has thefollowing properties
(2.21b)
There exists C > 0 suchthat(p, -C(cp, cpj for
any cp ED(A).
Moreover, the spectrum
of
A consistsof
a countable sequenceof eigenvalues
{-~}z~=o,i,z,....
These and thecorresponding eigenfunctions satisfying
=
ÀjCPi
aregiven by
where
M(a,
b;z)
is the standard Kummerfunction (cf. [HV6
Section2]
and[GaP]),
andfor any j
=0, l, 2, ... cj is
selected so that=
1.The
proof
ofProposition
2.1 follows with minor modifications from that of Lemma 2.3 of[HV6].
For the readersconvenience, however,
we shallmerely
sketch here one of its main
points,
which underlines the dimension restrictionn > 4. Let L > 0 be any
positive integer. Then,
as recalled in[HV6],
for any p E with L > 3 thefollowing inequalities
holdAs a matter of
fact,
when L = 3(2.25a)
reduces to the classicaluncertainty principle
Lemma(cf. [RS],
vol. II, p.169),
and(2.25b)
is an inmediateconsequence of
(2.25a).
From(2.25b)
wereadily
obtain that for any p EUQ (-R2n-1 )
it then follows that A is bounded below whenever
which
actually
holds for 2n > 5 +7/8.
?This is the crucial
startpoint
to show that A has a(unique)
Friedrichsextension which satisfies the results described in the
Proposition
above. DIt will be useful later on to recal here that the Kummer’s function
M(a,
b;z)
is ananalytic
function in thecomplex plane
whenever a, b arecomplex
numberssuch that where n =
0, 1, 2,.... Furthermore,
Recalling (2.24),
one also has thatcj
(/’ = 0,1,2,...)
andr(z)
is the standard Euler’s gamma function. 4JWe next
proceed
toanalyse
some minimal surfaceswhich
are in a sensetangent to the cone
Cn as Ixl
--~ oo. Moreprecisely,
thefollowing
result holds:PROPOSITION 2.2. Let n > 4.
Then for
any a > 0 there exists aglobally defined
minimalsurface Ma,
invariant under the actionof 0(n)
X0(n),
whichmay be parametrized
inthe form
where
is
given by
for
r > a, andthe function Ga(r)
is such thatGa(r)
0for
r > a,Ga(a) =
-a,(Ga)r(a)
= 1 andwhere a 0 is
given
in(2.24),
andko
> 0 is a constant which isindependent of
a. Moreover,if
we represent the intersectionof Ma
with the two dimensionalplane (x 1, xn+1 ) by
we have that:
PROOF. Let us write
G(r) - Ga(r)
for convenience.Recalling (2.10)
and(2.27), equation
H = 0yields
where we
impose
theboundary
conditionsAs r » 1, we shall assume that
We shall obtain a solution of
(2.30)-(2.32) by
means of classical ODEtheory.
To this
end,
we setA
quick computation
reveals now that(2.30)
is transformed intowhere
B. 11 /
Conditions
(2.31), (2.32)
read nowStandard
techniques yield
at once thefollowing phase diagram
for(2.34).
v
Figure
4: Thephase diagram
for(2.34)
in theregion
W 0.The
corresponding picture
for thesemiplane
W > 0 may now be obtainedby
reflection withrespect
to theorigin.
Notice that notrajectory
can cross fromthe
region
W -1 to that where W > -1, since the line W = -1 issingular
for
(2.34).
At thepoint (0,0),
we have twopossible asymptotic behaviours,
namely
or
where
4
We need to show that the
trajectory starting
at(-1, 2)
behaves as indicated in(2.36a).
To thisend,
we use the barrier function Z =(/3- + e)W,
where e > 0 ispositive
and small.Along
suchbarrier,
theslope
of thevelocity
field definedby (2.34)
isgiven by
if 6- > 0 is small
enough.
Thus the flow associated to(2.34) points along
theline z =
(Q-
+e)W
towards theregion
Z({3- + e)W.
This show that
(2.36a) holds,
whence(2.28)
in theoriginal
set of vari-ables. As a matter of
fact,
theprecise dependence koa-a
is obtainedby scaling:
ifGa(r) a )
is a solution of(2.30)-(2.32), ( ) ( we
weeasily
y check thato
BGa ar b
/for any b > 0. In
particular Ga(r)
=aGI (I) - klal-ara
as r ---> oo. On thea
other
hand,
sinceW(y)
isstrictly decreasing
as yincreases,
the surfacesMa
never intersect for different values of a. To derive
(2.29),
we notice that B satisfieswhence
Ba(u) - u
as u - oo andBa(u)
> 0 since G > 0. From(2.27b)
wereadily
see that for u > 0, v > 0,’
hence
Ba(u)
> u andby (2.28)
and
It follows from
(2.37)
that B’ > 0.Indeed,
if B’ 0 in someregion,
B wouldhave a
positive
maximum at some value u E[0, oo)
whereB’(u)
= 0, and since> 0,
(2.37)
wouldgive
a contradiction. On the otherhand,
oneclearly
has
B"(0)
> 0. Assume thatB"(u*)
= 0 for some u* > 0. At such apoint,
weshould have I ~ ...." I
and
by (2.37) B’(u*)
> 0. ThenB"’(u*)
> 0, but this contradicts the existence of thepoint
u* describedabove,
since B is convex near theorigin,
as well aswhen u --~ oo. This proves
(2.29). Finally,
the fact thatMa
is a minimal surface follows from standardtheory (cf.
for instance[F] 5.4.18).
DLet us fix now T > 0,
Q > 0, k > 0, p > 0, ~ = 1, 2, ...
such thatAi
> 0, 8 E(0, 1)
and 7yi, r~2 so that 0 7/2 We then define the setas the set of families of surfaces
{r(t)}
with thefollowing properties.
(2.39)
ForT - f/2
tT - r~ 1,
the familiesr(t)
are smooth embedded surfaces g : M -~JR2n,
where M is as inProposition 3.2, and g
conmutes withthe action of the group
0(n)
x0(n).
(2.40)
For x Er(t), t
E(T -
"12, T - and,~e-T ~2 ~ Ixl p,
there holds(2.41)
Let be where a is as in(2.23).
In theregion the
surfaces (may be
parametrized
as in(2.3b).
Moreover
where
J(2.42)
The surfacesr(t) (t
E(T - r~2, T - r~ 1 ))
may beparametrized
as in(2.12), 2.13 .
The functionu t
is convex foru 1 e-T ~2
andu
>(2.43)
Let be as in(2.41). For Ixl
the surface(T - t)#r(t)
is contained in the 2n-~dimensional
region
contained between andIt is
readily
seen that forlarge enough ,Q,
smallenough
p and fixedk,
theset "12,
B]
is nonempty
for any 771 ~ ’q2 2:: 0 with "11 I smallenough.
In aninformal manner,
(2.39)-(2.43)
state that thefamily
of surfacesr(t)
is very closeto the Simons cone
Cn when lxl
~ 0, and the rescaled surface(T -
is close toMk.
We are now
prepared
to state in aprecise
way the main results of this paper.THEOREM 2.1. Let us > 0, k > 0, and take
,~ large
enoug and p smallenough.
For "1 > 0sufficiently
small there exists afamily of surfaces r(t)
with t E(T - "1,0)
which evolvesby
mean curvatureflow
and is such thatr(t)
E.~(ri, 0, 1).
Clearly,
thefamily
of surfacesr(t) collapses
ast T T
to a surface which satisfiesThe
asymptotic
behaviour of thefamily r(t)
ast T T
is described in detail in thefollowing.
THEOREM 2.2. For any c > 0 there exists "1 > 0 and
k
> 0with
csuch that the
following properties
hold.i) Let 1/J
be thefunction
in(2.3c), (2.41). Then,
as T - 00in
02 uniformly
on setsu
p(r) for
anyfixed function
such that lim = 0, and i > 0r-->00
small.
ii)
Thesurface (T - approaches
toMT
ast T T, uniformly
oncompact sets.
iii)
Thesurface r(T)
is tangent to the Simons coneCn
at x = 0. Moreprecisely, if r(T)
isparametrized
as in(2.12), (2.13),
there holdswhere
Of
and c.~ arerespectively given in (2.26)
and(2.24).
3. - The
topological argument
Let us denote
by
the Green’s function associated toeAT ,
whereA is the operator defined in
(2.20)
andProposition
2.1. It has beenproved
in[HV6]
thatAssume that
r(t)
E]
where0 7?
1].Let ~ :
R - R be a cutofffunction such that
We introduce the function
where
We extend Q as zero forWe then see that Q satisfies the
equation
for where
We now argue as in
[AVI], [HV6].
Let us fix £0 > 0 smallenough (to
beprecised).
Wepick
a =(al , ... ,
EJRi-1
1 such thatFor each a
satisfiying (3.5)
we choose a smooth surfacewhere the
dependence
of is continuous in a, and wherewhere pj
is as inProposition
3.1 and k isgiven
in the definition ofA more
precise
characterization ofrq(a)
for r and r > el1-1TO will begiven
in thefollowing.
We can now solve MCF
taking
as initial value. Let us denote thefamily
of evolved surfaces asrt(a).
define the setU7J,rj
c asWe also define the function
t~,~ ( ~ , T1) :
-given by
By
standard continuousdependence
results forparabolic differential equations
we
readily
see that~(’,7-1)
is a continuous function on and also there iscontinuity
with respect to q > 7y > 0.Moreover,
if1 - ~ (1~,~,1 ...1~,~,m_ 1 )
wehave that
where at = and
It is
easily
seen that8i,i
0,uniformly
onFollowing
the standard notation we shall denote thetopological degree
of1,7,iT : Ur¡,r¡ -+ JRl-1
at a = 0 as0, U,7,-).
A standardhomotopy argument
proves that +1 if "1 is small
enough.
The
key
result in theproof
of Theorem 2.1 is thefollowing
apriori
estimate
PROPOSITION 3.1. Assume that a E solves the
equation 1~,~ (a)
= 0for
some0 ~
"1. Then,if
"1 is smallenough,
thefamily of surfaces
E
A [?7,
1j,3 /4].
The
proof
ofProposition
3.1 will begiven
in Section 4. We will provenow that
Proposition
3.1implies
Theorem 2.1.To this
end,
we claim thatFrom
(3.9)
andProposition 3.1,
Theorem 2.1readily
followsTo prove
(3.9)
we observe thatby Proposition
3.1and
continuousdependence
results forMCF,
any solution of = 0, a E isstrictly
contained at
Then,
as0,
+1, a standardhomotopy argument
shows that as far as
Set
"1*
=The compactness
ofU r¡,r¡*
and thecontinuity
ofimply
the existence of a* EU~,~*
such that = 0. If"1*
= 0,(3.9)
follows. If"1*
> 0,Proposition
3.1 and continuous
dependence
results for MCFimply
thatUr¡,r¡*+6:fØ
for some6 > 0, thus
contradicting
the definition of?7* whence q*
= 0. D4. - The main estimates
In this Section we will prove
Proposition
3.1. As a first step we have LEMMA 4.1. Assume that Õ is a solutionof
theequation for
some
0 ~
"1. For any tt > 0 there exists r~o = such thatif
"1 "10 there holdsPROOF. We can use the variation of constants formula in
(3.2)
to obtainwhere
f 1 ( ~ , T) i
=1, 2, 3
aregiven
in(3.3). Taking
into account(3.5), (3.7), (4.2)
we obtainBy (3.3a)
and(2.42)
we obtainIfi(o,,7-)l
5 / 1+6 +|03C8|1=d
+-
(re"’- By (3.3a)
and(2.42)
we obtain> 0 is
arbitrarily
small.Then,
from(2.42)
we obtainwhere 6 >
0 b
> 0 are small.By
Lemma 2.5 in[HV6]
we then obtain for 6 > 0sufficiently
smallwhere X =
X -1 ~2
is defined in the usual sense of fractional spaces withrespect
the operator A.By (2.42)
and(3.3)
we obtainfor 6, 6 > 0
small, where x
is the characteristic function of the setis
readily
bounded ase-reBT
for some r > 0, B > 0.On the other
hand,
since theeigenfunctions So2 ( ~ ) i = 1, ... , m -
1 arebounded in we then have
and
taking
into account that as q - 0,uniformly
for6oe-Alo
we obtain(4.1)
for Tolarge enough.
0As a next
step
we obtain thefollowing
LEMMA 4.2. For any ii > 0 there exists
Ao
> 0 such that,if
A >Ao,
thereexists r~o =
?70(iz, A)
small with the propertythat, for
"1 770 there holdsPROOF. The estimate for r = 0 is a
simple adaptation
of Lemma4.3,
andLemmata 4.5-4.8 in
[HV6],
that we will notrepeat
here. The estimate for thederivatives,
may be deducedby rescaling.
Indeed. We define
We
easily
check thatW(u, r)
satisfiesequation (3.2),
and forAe-~lT ~ A. ~ "
For each fixed s > To, and 0 A 1 we then set
Notice that
Taking
into account(2.42)
and(2.43),
we obtain that for ~.= o.
If r > Ae-lt’ and A is
large enough,
and we definewe
easily
obtain that(-2013~)
is small for k =0, 1, 2,
i =
1,2, 3, lul
1. Thenby
standardregularizing
effects forparabolic
9
1equations,
we have du ’ is boundedfor -
2H
1, k =0, 1
1. If s = To we obtain similar bounds
assuming
the estimates on(2.42)
as well as for the third derivatives in
1j;«(J, TO).
Wefinally
obtain(4.4)
withk =
1, 2 by coming
back to theoriginal
set of variables. 0 As a next step we will obtain the estimates on(2.42)
in theregion
LEMMA 4.3. Assume
that 1j; is
as in(2.3c)
and a eU ’7,’7 is a
solutionof 1,~,~ (ix)
= 0. Let usfcx
J-t > 0 small.If
p in(2.42) is
smallenough
A > 0 islarge enough and "1 is sufficiently
small we have thatwhere
PROOF. We can construct sub and
supersolutions
for(2.11 )
with the formwhere £
= is anarbitrary
constant different from zero andCB
is alarge (positive
ornegative)
constantdepending
on B. It is astraightforward computation
to check thatL(r, T)
defines sub andsupersolutions
for(2.11 )
forsuitable choices of
C,
p > 0small, and "1
small.Moreover,
if A islarge enough r/.u2Àt+1,
andby
Lemma4.2, 1/J
isarbitrarily
clase to , and A islarge enough.
Then
we can take in thedefinition
ofL( r T)
valuesB1 , 82, Bi
Krl82 Then,
we can take in thedefinition
of valuesB1, B2, 1 2
and construct thecorresponding
sub andsupersolutions. Taking
the initial value between them wefinally
arrive at(4.6).
DWe now
proceed
to obtain the bounds for the derivatives on(2.42).
LEMMA 4.4. Assume that
1jJ,
a are as in theprevious
Lemma.Then,
thereholds
(i)
Thefunction Q(u, t)
has theconvexity
indicated in(2.42) for
To T Tland
|y |>
A as well asfor |y| _ 1 A
Aif
A islarge enough.
(ii)
We have the estimateswhere it, p, "1 are as in Lemma 4.3.
PROOF. Part
i)
followsby comparison. Taking
into account(2.15)
and(2.19)
wereadily
obtain thatWithout loss of
generality
we can assume thatQ(u, t)
> u forpeT/2.
Moreover
by
Lemma 4.2 and(2.42)
we can assume thatQ
is convexfor
A,T > To and A
Iyl ~ peT/2,
T = To.Differentiating (4.8)
withrespect
to u we obtainwhere
L1
is aparabolic operator satisfying LI(c,u,7-) =
0 for any c E R.Selecting
the initial values in a suitable way, we haveby comparison
thatA new differentiation of
(4.8a) yields
where
L2
is aparabolic operator satisfying L2(0, U, T)
= 0.Arguing again by comparison
we arrive at 0Quu
forI peT/2,
T > To andpart i)
ofLemma 4.4 follows. The case
Q(u, t) u
for T > To is similar.From the
convexity
orconcavity
of the surface we obtain(4.7a)
fromLemma 4.3.
To derive
(4.7b)
we need a more careful argument.Let us
parametrize
the surfacer(t)
aswhere
for some
Taking
into account(2.6), (2.10)
weeasily
obtain that Z satisfies theparabolic equation
and
taking
into account(2.2), (2.3c)
we have that, I
We define
where i . and
It is
easily
seen thatBy (4.6)
and(4.10)
we have thatwith >
small if andby
we havefor
If s = ~ we can assume that the initial value
~(~, TO)
to be close to well as its first three derivatives. Thisgives
for j = 0, 1, 2, 3,
1 rpe/.
On the otherhand, taking
into account(4.10)
and
(4.11 )
we obtainwhence:
where A is
large enough and q
smallenough.
DefineBy (4.12)
we obtain thatR,(-y, A)
satisfies theequation
where
Clearly
for i =1,2,
Alarge enough,
q smallenough.
We now canuse
(4.13)
and interior estimates forquasilinear equations (cf. [LSU],
Theorem5.4,
p.449,
as well as(4.14)
and Theorem6.1,
p. in[LSU]
to prove that,
1 (R.~),y-i 1, 1 (R,),,), I
areuniformly
bounded.Then,
we have thatR,
satisfiesan
equation
of the form(R,)),
=as(¡,
+b.~ (-i, B)(R,,)-i
+Cs(~, A)R.,,
wherea,,
bs,
c, and their derivatives are bounded.By
standard Schauder estimates weobtain 1
-1 ~ , 1
for s q,
111 I 1,
0 A 1 andtaking
into account(4.10) (4.11 )
we canprove that in the
original
set of variables this estimateimplies
thatfor 1
This concludes the
proof
of Lemma 4.4. DAs a next
step
we obtainprecise
estimates for theregion jyj
« 1.LEMMA 4.5. Let J.l > 0 be small
enough
and let a as inProposition
3.1. Thesurface
is contained betweenMk-J1.’ Mk+p,for T -r~
tT-"1, and Ixi C(T - t)1/2+ul
whereM,,
isdefined
inProposition
2.2. Moreover,if
we
parametrize rt(ix)
as in(2.13)
we have that the derivativesof
thefunction L(p, T) defined by
are
uniformly
bounded in each compact setof
pif
"1 is smallenough.
PROOF. The surface defined
by
therescaling (T -
and the newtime variable s
= 1
evolvesaccording
to theequation
2(Jf
g qwhere