A NNALES DE L ’I. H. P., SECTION C
F ELIPE L INARES G USTAVO P ONCE
On the Davey-Stewartson systems
Annales de l’I. H. P., section C, tome 10, n
o5 (1993), p. 523-548
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On the Davey-Stewartson systems
Felipe
LINARESInstitute for Pure-Appl. Math., Rio de Janeiro, Brazil
Gustavo PONCE
Department of Mathematics, University of California, Santa Barbara, CA 93106, USA
Vol. 10, n° 5, 1993, p. 523-548. Analyse non linéaire
ABSTRACT. - We
study
the initial valueproblem
for theDavey-Stewartson systems.
This model arisesgenerically
in bothphysics
and mathematics.Using
the classification in[15]
we consider theelliptic-hyperbolic
andhyperbolic-hyperbolic
cases. Under smallnessassumption
on the data it is shown that the IVP islocally wellposed
inweighted
Sobolev spaces.Key words : Initial value problem, smoothing effect, local well-posedness.
RESUME. - Nous etudions le
probleme
deCauchy
pour lessystemes
deDavey-Stewartson.
Ce modele sepresente
defagon generique
en mathe-matiques
et enphysique.
Nous utilisons la classification de[15]
et consi-derons les cas
elliptique-hyperbolique
ethyperbolique-hyperbolique.
Sousdes conditions
(de petites tailles)
sur les donnees nous montrons que leprobleme
est bienpose
sur les espaces de Sobolev apoids.
1. INTRODUCTION
Consider the initial value
problem
IVP for theDavey-Stewartson (D-S)
svstem
where
u = u (x,
y,t)
is acomplex-valued function,
y,t)
is a real-valued function
at
=a/at, ax
=ay
=~/~y
and co, ..., c3 are real para-meters.
A
system
of this kind was first derivedby Davey
and Stewartson[11] ]
in their work on two-dimensional
long
waves over finitedepth liquids (see
also
[12]). Independently
Ablowitz and Haberman[1] obtained
aparticular
form of
( 1. 1 )
as anexample
of acompletely integrable
model whichgeneralizes
the two-dimensional nonlinearSchrodinger equation.
Sincethen several works have been devoted to
study special
forms of thesystem ( 1. 1 ) using
the inversescattering approach.
In fact when(co,
CI’ C2,e3) _ ( - l, 1, - 2, 1)
or(1, -1, 2, -1)
thesystem
in(1.1)
isknown in inverse
scattering
as the DSI and DSIIrespectively.
In thesecases several remarkable results
concerning
the associated IVP have been established(see [2]-[5], [10]
and theirbibliography).
On the other hand the abovesystem
arises in water waves,plasma physics
and nonlinearoptics.
Moreover,
it has been shown that underappropriate asymptotic
consider-ations a
large
class of nonlineardispersive
models in two dimensions canbe reduced to the
system ( 1.1 ) (see [13], [29]
and referencestherein).
In
[15] Ghidaglia
and Saut studied the existenceproblem
for solutionsof the IVP
( 1. 1 ). They
classified thesystem
aselliptic-elliptic, elliptic- hyperbolic, hyperbolic-elliptic
andhyperbolic-hyperbolic according
to therespective sign of (co, c3): ( + , + ), ( + , - ), ( - , + )
and(-, -).
For theelliptic-elliptic
andhyperbolic-elliptic
casesthey
obtained aquite complete
set of results
concerning
local andglobal properties
of solutions to the IVP( 1 . 1 )
inL2, H2.
Their main tools were the LP - L~ estimates of Strichartztype [24] (see [6], [16], [19], [26])
and thegood continuity
proper- ties of theoperator ( - 0) -1
I(and
itsderivatives).
Also in theelliptic- hyperbolic
casethey
established theglobal
existence of a weak solution of the IVP( 1.1 ) corresponding
to "small" data(see
also[25]).
In this case
(elliptic-hyperbolic)
as well as thehyperbolic-hyperbolic
caseone has to assume that (p
( . )
satisfies the radiation condition i. e.[without
loss ofgenerality
we have taken C3 = -1 in(1.1)].
Thisguarantees
that forF ELl ([R2), .%-1 F is
well defined wherelinéaire
Thus the IVP
(1.1)
isequivalent
towith
Co> 0 (resp. Co 0) corresponding
to theelliptic-hyperbolic
case(resp.
hyperbolic-hyperbolic case).
As was remarked in
[15]
and[25]
no existence results were known for thehyperbolic-hyperbolic
case.Our main purpose here is to established local
well-posedness
results forthe
IVP ( 1. 2) (with (i. e.
theelliptic-hyperbolic
andhyperbolic- hyperbolic cases)
for "small" data. Our notion of wellposedness
includesexistence, uniqueness, persistence [i. e.
the solutionu ( . )
describes a con-tinuous curve in the function space X whenever uo
eX].
Theproblem (1. 2)
can be seen as a nonlinear
Schrodinger equation involving
derivatives anda nonlocal term in the
non-linearity.
It isinteresting
to remark thatprevious approaches
used in nonlinear evolutionequation (LP -
Lq estima-tes, energy
inequality, L2-theory, etc.)
do notapply
in this case.In
[22] Kenig, Ponce,
andVega
studied the IVP for nonlinear Schrodin- gerequation
of the formwith ...,
a/axn)
anddenoting
apolynomial
having
no constant or linear terms. Theirarguments rely heavily
onsharp
versions(see [21], [22])
of thehomogeneous
andinhomogeneous smoothing
effect first establishedby
Kato[18]
in solutions of theKorteweg-de
Vriesequation.
This allows them to obtain conditions whichguarantee
that for "small" data the IVP( 1 . 3)
is localwellposed.
Here weshall extend this
approach
to treat theequation
in(1.2)
whichpresents
amore
complicated
nonlinear term(i.
e. nonlocal terminvolving
anoperator
with badcontinuity properties)
than that considered in( 1. 3).
In the
hyperbolic-hyperbolic
case(i. e. Co 0)
after rotation in the xy-plane
andrescaling
thesystem ( 1. 2)
can be written aswhere Jf cp =
~2xy
cp(with
cpsatisfying
theappropriate
radiationcondition)
and cl, c2, c3 are
arbitrary
constants.To
explain
our results(in
thehyperbolic-hyperbolic case)
it is convenient to consider first the associated linearproblem
to(1.4)
It will be shown
(see
Theorem2.1)
that there exists c > 0 such that forany y~R
denotes the group associated to the IVP
(1.5),
DX~2 v (x, y, t) = c (~ ~ ~ 1 ~2 v~x~ (~, y, t)) "
withdenoting
the Fouriertransform in the x-variable. Notice that
( 1. 6)
is aglobal (in
space andtime)
estimate which involves theLy L~
Previous resultsonly provide
thegain
of half-derivatives in(~3) (see [9], [27], [28]). Roughly speaking (1.6) corresponds
to thesharp
one dimensional version of the Katosmoothing
effect obtained in[21] (Theorem 4 .1 ).
Also theestimate
( 1. 6)
illustrates one of thekey arguments
in theproof
of thehyperbolic-hyperbolic
case(see
Theorem Abelow),
i. e. the use of differentLP-norms for the x
and y
variables. This kind of estimate also appears in theinhomogeneous
version of(1 . 6) (see
Theorem2. 3)
and wheninverting
the
operator
3i[see
estimate(2. 20)
inProposition 2.7].
Our results in the
hyperbolic-hyperbolic
case are contained in the follow-ing
theorem.THEOREM A. - There exists ~ > 0 such that
for
anywith s >_ 6 and
there exist T = T
(~o)
> 0[with
T(bo)
- oo as60 - 0]
and aunique
classicalsolution u
( . ) of
the IVP( 1 . 4) satisfying
and
Moreover for
any T’ E(0, T)
there exists aneighborhood Vuo of
uo inYS
such that the map
50 - u (t) from Vuo
into the classdefined by ( 1 . 7)-( 1 . 9)
with T’ instead
of T
isLipschitz.
-In Theorem A
(and
Theorem Bbelow)
we shall notoptimize
the lowerbound for the Sobolev
exponents given
in thehypothesis.
linéaire
In the
elliptic-hyperbolic
case(i. e. co =1)
after a rotation in the xy-plane
andrescaling, ( 1 . 2)
becomeswhere 3i cp =
aXy
cp and c~, c2, c3arbitrary
constants.As was remarked above in this case
Ghidaglia
and Saut[15]
established theglobal
existence of a weak solutioncorresponding
to "small" data.Also in
[25]
M. Tsutsumi studied theasymptotic
behavior of this weaksolution. Our results show that the IVP
(1.10)
is localwellposed
for smalldata uo.
THEOREM B. - There exists 6 > 0 such that
for
anywith
s >_ 12
andthere exist T = T
(bo)
> 0[with
T(bo)
- oo as~o -~ 0]
and aunique
classicalsolution u
( . ) of
the IVP(1. 10) satisfying
and
Moreover
for
any T’ E(0, T)
there exists aneighborhood Vu of uo
inYS
such that the map
io - u (t) from u0
into the classdefined by ( 1. 11 )-( 1.12)
with T’ instead
of T
isLipschitz.
-This paper is
organized
as follows: in section 2 we shall deduce all linear estimates needed in theproof
of TheoremsA,
B. Section 3 contains the essentialarguments
in theproof
of our nonlinear results. Here all the nonlinear estimates to be used in sections4,
5 are carried out in details.Finally
in sections 4 and 5 we prove Theorems A and Brespectively.
2. LINEAR ESTIMATES
In this section we shall deduce several estimates
concerning
the linearIVP
First we consider the
hyperbolic-hyperbolic
case, L e. 8 = 2014 1. In thiscase after
changing
variable andrescaling (2 .1 )
can be written asWe
begin by establishing
thefollowing sharp
versions of the Katosmoothing
effect in thegroup ( e‘t
~ commented in the introduction.THEOREM 2. 1. - There exists c > 0 such that
if
uo EL2 ((~2)
thenfor
any y E R the solution u( . , . , . ) of
the IVP(2. 2) satisfies
thatIt is clear that the same estimate holds with the roles of x
and y interchanged.
Proof - By
Fourier transform it follows thatHence
performing
thechange
of variables a =03BE~
and b =03BE, using
Plan-cherel’s theorem in the
(x, t)-variables, returning
to theoriginal
variablesand
using again
Plancherel’s theorem one obtains thatCOROLLARY 2 . 2. - Let F ~
Ly (R :
t~(f~2)).
ThenAnnales de l’lnstitut Henri Poincaré - linéaire
Proof -
It follows from(2. 3) by duality.
Next we deduce the
inhomogeneous
version of the estimate(2. 3).
Thuswe consider the
inhomogeneous
IVPwhich solution u
( . )
isgiven by
the formulaTHEOREM 2. 3. -
If
u( . )
is the solutionof
the IVP(2. 5)
thenProof. -
We shall follow theargument
in[22].
Using
Fourier Transform in the time and space variables oneformally
has that
Hence
applying
Plancherel’s theorem it follows thatwhere
and t~ denotes the Fourier transform of F in the x, t variables.
By comparison
with the kernel of the Hilbert transform(or
itstranslated)
itis easy to see that K E L~
(f~3).
Thuscombining (2. 8),
Minkowski’sintegral
inequality
and Plancherel’s theorem we find that for any y e RUsing
Parseval’sidentity
we find(formally)
that the solutiont)
satisfies the
following
dataBy (2 . 4)
we can infer thatD;/2 U (x,
y,0)
EL 2 (1R2). Finally
sincecombining (2. 9), (2. 3)
and the above remark we obtain(2.7).
The aboveformal
computation
can bejustified (and
theproof stays essentially
thesame) by using
theargument given
in[23] (section 3).
Next we recall some estimates
concerning
the Katosmoothing
effect inthe
group {~}~.
.It is convenient to introduce the notation:
thus
{Q~ p}~,p 6 ~
forms afamily
of cubes of side one withnonoverlapping
00
interiors such that
[f~
=U
p.Q[,P=-00
’
THEOREM 2.4. - Then
where G
(x,
y,t) _ (, (~, ~1) ~ 1 ~2 (~,
.~,t )) " .
Then
and
where
Vx,
y=
(ax, ly) .
-’ °
Annales de l’lnstitut Henri Poincaré - Analyse linéaire
Proof. -
The estimate(2.10)
wasbasically
proven in[9], [27]
and[28].
(2 .11 )
is the dual version of(2 .10). Finally (2 .12)
was established in[22].
To
complement
theprevious
estimates in theproof
of our nonlinearresults in section 3 we shall use the
following
theorems.LEMMA 2. 5. - Let uo E
H4 (~2) (~ H3 (~2 : r2
dxdy).
Thenwhere
with r=
(x2
+y2)1/2.
-Proof -
Forsimplicity
in theexposition,
it will be carried outonly
the details for T > o.
For
(y, t)
fixed Sobolev’s theorem tells us that_ .. _ _~ ... _~ ..
Similarly for y
fixednow
using
theinequality
together
with Minkowski’sintegral inequality
and theidentity (see [17])
we find that
and
The same
argument applied
to the last two terms on theright
handside of
(2.15) yields (2.13).
Using
the notation introduced before the statement of Theorem 2.4 and in(2.14)
one has thecorresponding
result for the group{~~}~.
LEMMA 2.6. - Then
Proof (see [22], Proposition
3.7).
Next we deduce some estimates
concerning
the secondequation
in( 1.1 ).
Thus after a
change
of variable we need to consider theproblem
with F E
L1 (f~2)
and w( . , . ) satisfying
the radiation conditionUnder the above
hypotheses
theequation (2. 17)
has aunique
solutiongiven by
the formulaePROPOSITION 2. 7. - then and
In
addition, if
F ELy (R : Lx ((1~))
thenWe recall the notation
As was commented in the introduction we observe that the estimates
(2. 3)-(2. 7)
and(2.20)
use different LP-norms for the xand y
variables.Proof. - (2.19)
followsdirectly
from(2.18).
To obtain(2.20)
from(2.18)
one sees thatThus
computing
theL2-norm
in x,using
Minkowski’sintegral inequality
and
taking
supremum in they-variable
we obtain(2. 20).
3. NONLINEAR ESTIMATES
In this section we shall obtain all the nonlinear estimates needed in the
proofs
of TheoremsA,
B. First we have thefollowing inequalities
concern-ing
fractional derivatives.THEOREM 3 . 1. - Let
s > 0, 0 a 1, [0, a]
with a = 03B11 + oc2.oo) with 1 + 1 , =1 oo).
Thenfor
anyf,
gp
P (Schwartz class)
and when n =1
(not essential)
+ 2014 = - 00 L
~~~1 ~2 ~
Proof -
The estimate(3 . 1 )
was proven in[20] (Appendix). (3 . 2)
follows
by combining Galiardo-Nirenberg,
H61der andYoung inequalities.
Finally,
for(3 . 3)
and(3 . 4)
we refer to Theorems A. 12 and A. 13 in[23]
respectively.
As was remarked in[20]
and[23]
theproof
of(3 . 1), (3. 3)- (3. 4)
relies on ideas of Coifman andMeyer ([7]-[8]).
The
following
estimates form the essentialsteps
in theproof
ofTheorems
A,
B.They
combine the linear results obtained in section 2 with theinequalities
in Theorem 3 . 1.Propositions
3.2-3.5 concerned withPROPOSITION 3. 2. -
If
k =s -1 /2
E 7~ with k >_ 3 thenProof -
Tosimplify
the notation we assume(without
loss ofgenerality)
that c
== c~ = ~3 = 1.
ThusUsing
thehomogeneous
version of the Katosmoothing
effect in thegroup described in
(2. 3) together
with Minkowski’sintegral inequality
and the estimate in(3 .1 )
it follows thatTo bound
A2
we first observe thatsince
aXy ~ -1--_ identity.
Annales de I’Institut Henri Poincaré - Analyse linéaire
Hence
(2. 3)
and Minkowski’sintegral inequality
lead toThe estimate for the second term on the
right
hand side of(3 . 8)
is thesame as that in
(3 . 7).
To handle the first term on theright
hand side of(3 . 8)
we use(3 . 3), (3.4), (2.19)
and(3.2)
to obtainFinally
we consider the termA3
in(3 . 6).
SinceFrom
(2. 3)
and(2. 7)
we have thatCombining
Minkowski’sintegral inequality
and the estimates(2.20), (3 . 2),
it is not hard to obtain thefollowing string
ofinequalities
A similar
argument
shows thatOn the other
hand, using (3.3), (2. 19), (3.4)
and(3.2)
we obtainfor j
fixed in
B2
thatTherefore
Combining (3.10)-(3.14)
one has a bound forA3. By inserting
thisbound and those in
(3.7)-(3.9
forAi, A2 respectively
in(3.6)
weobtain
(3 . 5).
Annales de I’Institut Henri Poincaré - Analyse linéaire
PROPOSITION 3 . 3. - with
k >_- 3
thenProof -
Theargument
forhighest
derivatives is the same as thatgiven
in the
previous proof
where instead of(2 . 3)
and(2. 7)
one uses the groupproperties
and(2.4).
Theproof
for the lowest derivatives issimpler
andsimilar to that to be used in
coming propositions,
hence it will be omitted.PROPOSITION 3.4:
We recall the notation for the
with
r==(~+~)~.
Proof. - Combining
Minkowski’sintegral inequality,
theidentity (see [17])
and the one obtained
by reversing
the roles of xand y together
with thegroup
properties
and the estimates(2. 19)-(2.20)
and(3.2)
it is not hardto see that
for ~a ~
3which
yields (3 .16).
PROPOSITION 3.5.
Proof. - Using
Minkowski’sintegral inequality, (2.13), (3 . 1 ), (3 . 2)
and Sobolev’s theorem it follows that
From
(3 . 2)
and(2 .19)
it is not hard to see thatand
Inserting (3 .19)-(3 . 20)
in(3 .18)
andusing
Sobolev’s theorem we obtain the desiredinequality (3 .17).
PROPOSITION 3. 6. -
If k = s -1 /2 E 7L with k >_
3 thenWe recall the notation:
with a,
(3
E 7~.Proof. -
Without loss ofgenerality
we can assume cl = c2 == 1.Thus
From the
homogeneous
version of the Katosmoothing
effect in(2 .10),
the Minkowski’sintegral inequality
and the estimate(3 .1 )
it follows thatTo bound
A2
we notice thatUsing
anargument
similar to thatgiven
in(3.23) [based
in estimate(2.10)] together
with theinequality (2.19)
oneeasily
sees thatwhere
Hx
denotes the Hilbert transform in the x-variable.To handle the first term on the
right
hand side of(3 . 24)
we use(2.12)
to see that
Annales de l’Institut Henri Poincaré - Analyse linéaire
Combining
theargument
used in theproof
of(2. 20)
with thecorrespond- ing
version of(3 . 2)
for bounded domains it follows thatInserting (3.27)
in(3 . 26)
we obtain the bound for the first term on theright
hand side of(3 . 24j.
Theproof
for the second term follows the sameargument.
Finally,
to boundA3,
we notice thatThen the
smoothing
effect(2.10) together
with similararguments
as those in(3 . 23)
and(3. 25) yield
Collecting
all these bounds weget (3.21).
PROPOSITION 3 . 7. -
If h = S - 1 /2 E ~L
withk >_ 3
thenwhere D was
defined
in(3 . 21 ).
Proof. -
Thepart
of theproof
of(3 . 29) involving
thehighest
deriva-tives is similar to that used to obtain
(3 . 21 )
where instead of(2.10)
and(2.12)
one needs the groupproperties
and(2 . 11 ).
Theargument
for the lowest derivatives is astraight application
of the groupproperties.
PROPOSITION 3.8: 1
Proof. -
From Minkowski’sintegral inequality
and(2.16)
it followsthat
From
(3 . 2)
one has thatand
Similarly
from(2 .19)
and(3 . 2)
it is easy to tind thatand
Inserting (3.32)-(3.35)
in(3.31)
and thenusing
Sobolev’s theorem weobtain
(3.30).
PROPOSITION 3.9 : 1
Proof. -
Theproof
is similar to thatprovided
in detail for(3.16) (Proposition 3.4).
Hence it will be omitted.4. PROOF OF THEOREM A
To
simplify
ourexposition
we fix s such thatBy hypo-
For v~L~
([0, T] :
HS(!R2)
defineand
For uo E HS
(!R2) U H3 (!R2 : r2
dxdy)
we denoteby (v)
= u the solution of the linear IVPwhere v E
XT = ~
v(v) _ a ~ .
We shall prove that there exists ~ > 0 such that if
then there exist T > 0 and a > 0
[with T = T (80)
--~ oo asbo -~ 0]
such thatif v~XaT
then andis a contraction. For this purpose we
rely
on theintegral equation
versionof
(4. 6)
to writeThus
combining (2.3), (3. 5)
and Sobolev’s theorem we find thatSimilarly,
from the groupproperties
and(3.15)
it follows thatfrom
(3.16)
and from
(2.13), (3.17)
Annales de l’lnstitut Henri Poincaré - linéaire
Thus
(4 . 8)-(4 .11 ) yield
theinequality
Choosing a = 2 c ( 1 + T2) bo
with Tsatisfying
The same
argument
shows thatand that for
ToE (0, T)
when
I I I uo - uo I I I = I I uo - uo
+i I uo - uo ~H3xy
(r2> issufficiently
small.Therefore c
XT
for a and T as above and is a contraction.Thus there exists a
unique
u EXT
such that(u)
= u, i. e.(4 .16)
u(t)
=eit~2xy
uoInserting
theargument
used for(4. 8)
in(4.16)
we obtain thatSince as T --~ 0
by (4.13)
it follows that~, i (u) - o ( 1 )
as T - 0.
Combining
this result with thearguments,
in(4.9)-(4.10)
and the inte-gral equation (4.16)
we conclude thatNow
using
thecontinuity properties
is not hard to extend theuniqueness
result to the class
XT n
C([0, T] :
HS(I~2) (~ H3 (~2 : r2
dxdy)) (see [22]).
This observation
completes
theproof
of Theorem A.5. PROOF OF THEOREM B
As in Theorem A we fix s
satisfying
withk >__
12. It willbe clear from our
proof
below that this does notrepresent
a loss ofgenerality.
For v e L~
([0, T] :
HS((~2))
defineand
For uo
(~ H6 (~2) : r6 dx dy)
we denoteby (v)
= u the sol-ution of the IVP
It will be established that there exists ~ > 0 such that if
then there exist t > 0 and a > 0
[with
T(bo)
-~ oo as~o ~ 0]
such that ifv E
ZT
then u =(v)
EZT
andis a contraction. As in the
proof
of Theorem A werely
on theintegral
form p
(5 . 6)
trom
(2 . 10)
and(3 . 21 )
it follows thati ~ ~. ~ .... T ._ _ ... _ - _ -
Similarly,
trom the groupproperties
and(3 . 29)
ana Irom ana tj. ~U)
Annales de l’lnstitut Henri Poincaré -
Collecting
the information in(S . 8)-(5 . 11 )
andusing
the notation in(5.5)
one finds that(5.12) QT (v)) ~
c(1
+ + c(1
+T8) (QT (v))3.
Once that the estimate
(5.12)
has been established the rest of theproof
of Theorem B follows an
argument
similar to that used for Theorem A.Hence it will be omitted.
ACKNOWLEDGEMENTS
The authors would like to thank C. E.
Kenig,
J.-C. Saut and L.Vega
for fruitful conversations and
suggestions.
This work wassupported
inpart by
aNSF-grant.
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( Manuscript received November 27, 1992.)
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