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Controls insensitizing the observation of a quasi-geostrophic ocean model

Abstract

We consider a linear quasi-geostrophic ocean model with partially known initial conditions. We search for controls that make the observation locally insensitive to the perturbations of the initial data. Their existence is equivalent to the null controllability property for an associated cascade Stokes-like system. Thanks to the presence of the Coriolis term, we are able to prove the existence of such controls. Our strategy is the following. First, we prove a unique continuation property for the adjoint of the state system that leads to approximate controllability; then, under certain assumptions, an observability inequality is established for the adjoint. The proof is inspired by the arguments leading to the unique continuation property. This inequality leads to the desired null controllability result.

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Controls insensitizing the observation of a quasi-geostrophic ocean model

Author: Fernández Cara, Enrique; García Mókina, Galina Cristina; Osses Alvarado, Axel
Publisher: Society for Industrial and Applied Mathematics
Year: 2005
DOI: 10.1137/S0363012903433607
Source: https://idus.us.es/bitstreams/72c907ea-b029-4dc7-ae68-f7fe3f1ebee1/download
SIAM J. CONTROL OPTIM.c
2005 Socie y o Indus ial and Applied Ma hema ics
Vol. 43, No. 5, pp. 1616–1639
CONTROLS INSENSITIZING THE OBSERVATION OF A
QUASI-GEOSTROPHIC OCEAN MODEL∗
ENRIQUE FERN´
ANDEZ-CARA†, GALINA C. GARCIA‡,AND AXEL OSSES§
Abs ac . We conside a linea quasi-geos ophic ocean model wi h pa ially known ini ial
condi ions. We sea ch o con ols ha make he obse a ion locally insensi i e o he pe u ba ions
o he ini ial da a. Thei exis ence is equi alen o he null con ollabili y p ope y o an associa ed
cascade S okes-like sys em. Thanks o he p esence o he Co iolis e m, we a e able o p o e he
exis ence o such con ols. Ou s a egy is he ollowing. Fi s , we p o e a unique con inua ion
p ope y o he adjoin o he s a e sys em ha leads o app oxima e con ollabili y; hen, unde
ce ain assump ions, an obse abili y inequali y is es ablished o he adjoin . The p oo is inspi ed
by he a gumen s leading o he unique con inua ion p ope y. This inequali y leads o he desi ed
null con ollabili y esul .
Key wo ds. insensi izing con ols, Ca leman inequali ies, unique con inua ion, null con olla-
bili y, ocean model
AMS subjec classifica ions. 93B05, 35B37, 35B60, 35Q30
DOI. 10.1137/S0363012903433607
1. In oduc ion and main esul s.
1.1. Incomple e ini ial da a ocean model. Le Ω be a nonemp y open
bounded and connec ed subse o R2, wi h bounda y Γ o class C2and ou wa ds uni
no mal ec o ν=ν(x). Le ωbe a nonemp y open subse o Ω, T>0, Q=Ω×(0,T),
and Σ = Γ ×(0,T). In his pape , we will conside a linea quasi-geos ophic ocean
model [1, 15, 16] desc ibed by he ollowing equa ions:
⎧
⎪
⎪
⎪
⎪
⎨
⎪
⎪
⎪
⎪
⎩
u −A∆u+γu +( 0+βx2)k∧u+1
ρ0
∇p=T+h1ωin Q,
di u=0 inQ,
u= 0 on Σ,
u(0) = u0+τu0in Ω,
(1.1)
whe e u(x, ) and p(x, ), espec i ely, deno e he eloci y and he p essu e o he
fluid a (x, )=(x1,x
2, )∈R2×R+. In his model, A ep esen s he ho izon al eddy
iscosi y coefficien , γis he bo om ic ion coefficien , ρ0is he fluid densi y, and
( 0+βx2)k∧uis he Co iolis e m, wi h k∧u=(−u2,u
1). In he igh -hand side, 1ω
deno es he cha ac e is ic unc ion o ωand Tis a gi en sou ce in L2(Q)2. The e m
∗Recei ed by he edi o s Augus 22, 2003; accep ed o publica ion (in e ised o m) July 1, 2004;
published elec onically Ma ch 11, 2005.
h p://www.siam.o g/jou nals/sicon/43-5/43360.h ml
†Depa amen o de Ecuaciones Di e enciales y An´alisis Num´e ico, Uni e sidad de Se illa, Ap do.
1160, 41080 Se illa, Spain (ca a@nume .us.es). This au ho ’s wo k was pa ially suppo ed by
D.G.E.S. (Spain) g an s BFM2000-1317 and BFM2003-06446.
‡Facul ad de Ingenie ´ıa, Uni e sidad Ca ´olica de la San ´ısima Concepci´on, Casilla 297, Con-
cepci´on, Chile ([email p o ec ed]). This au ho ’s wo k was suppo ed by FONDAP in Applied Ma he-
ma ics, CONICYT Ph.D. g an s, and CONICYT-INRIA coope a ion ag eemen s (Chile).
§Depa amen o de Ingenie ´ıa Ma em´a ica, Uni e sidad de Chile, Casilla 170/3 Co eo 3, San-
iago, Chile, and Cen o de Modelamien o Ma em´a ico, UMI 2807/Uni e sidad de Chile-CNRS,
San iago, Chile ([email p o ec ed]hile.cl). This au ho ’s wo k was pa ially suppo ed by FONDAP
in Applied Ma hema ics, FONDECYT-CONICYT 1030808-7030059, and ECOS-CONICYT C01E02
g an s (Chile).
1616
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CONTROLS INSENSITIZING AN OCEAN MODEL 1617
τu0, whe e τ∈R, ep esen s a small unknown pe u ba ion o he ini ial eloci y field
u0, and h=h(x, ) is a con ol unc ion o be de e mined.
No ice ha he Co iolis o ce is ep esen ed by a ze o o de coupling e m in he
equa ions. I in oduces a diffe en beha io o he sys em depending on he di ec ion
in space. To simpli y he p esen a ion o he esul s, we will assume ha A=1,γ=1,
0=1,β= 1, and ρ0=1.
We in oduce he ollowing spaces, which a e usual in he analysis o S okes sys-
ems:
H={ ∈L2(Ω)2: di = 0 in Ω, ·ν= 0 on Γ},
V={ ∈H1
0(Ω)2: di = 0 in Ω},W=H2(Ω)2∩V.
Recall ha
W→V→H≡H→V→W,
whe e he embeddings a e dense and compac .
Fo any gi en u0,τu0∈Hwi h u00,Ω=1,anyT∈L2(Q)2, and any h∈
L2(ω×(0,T))2, he linea sys em (1.1) possesses a unique solu ion (u, p), wi h u∈
L2(0,T;V)∩H1(0,T;V) and p∈W−1,∞(0,T;L2(Ω)). (pis unique up o an addi i e
dis ibu ion only depending on .) This is easily p o ed by adap ing he a gumen s o
[17] o he p esence o a skew-symme ic Co iolis e m in he equa ions. No ice ha i
we had u0+τu0∈V, hen he couple (u, p) would sa is y u∈L2(0,T;W)∩H1(0,T;H)
and p∈L2(0,T;H1(Ω)).
We will be conce ned wi h he sea ch o con ols such ha he eloci y measu e-
men s o e an obse a ion se a e ei he insensi i e o almos insensi i e o small
a ia ions o he ini ial condi ions. To do his, we will use insensi izing con ol heo y.
1.2. Insensi izing con ols and con ollabili y. Le Obe an open nonemp y
subse o Ω and le us in oduce he ollowing unc ional, defined on he amily o
solu ions o (1.1):
Φ(u)=1
2T
0O
|u(x, )|2dx d .(1.2)
The no ion o insensi izing con ols was in oduced by Lions [13]. In he con ex
o (1.1)–(1.2), i eads as ollows.
De ini ion 1.1. We say ha he con ol h∈L2(ω×(0,T))2is Φinsensi izing
i
d
dτ Φ(u)τ=0 =0 ∀u0∈Hwi h u00,Ω=1.(1.3)
On he o he hand, we say ha h∈L2(ω×(0,T))2is Φε-insensi izing i

d
dτ Φ(u)τ=0≤ε∀u0∈Hwi h u00,Ω=1.(1.4)
O cou se, in (1.3) and in (1.4) uis, oge he wi h p, he solu ion o (1.1).
The Φ insensi izing ( esp., Φ ε-insensi izing) con ols hmus be in e p e ed as
hose leading o an obse a ion Φ(u) ha is locally independen ( esp., almos inde-
penden ) a he ini ial pe u ba ion τu0. The exis ence o such con ols is a pe inen
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1618 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
ques ion, since i is ealis ic o assume ha he ue ini ial condi ions o (1.1) a e
unknown. In ac , as no iced in [13], i would be mo e con enien o sea ch o Ψ
insensi izing (o Ψ ε-insensi izing) con ols, whe e
Ψ(u)=1
2T
0O
|cu l u(x, )|2dx d ,
bu his is beyond he scope o his a icle and will be he subjec o u u e wo k.
I is easy o cha ac e ize he insensi i i y ( esp., ε-insensi i i y) p ope y in e ms
o exac null con ollabili y ( esp., app oxima e con ollabili y) o a ela ed cascade
sys em. Indeed, le (¯u, ¯p) and (q, ) be he solu ions o he ollowing sys ems:
⎧
⎪
⎪
⎨
⎪
⎪
⎩
¯u −∆¯u+¯u+(1+x2)k∧¯u+∇¯p=T+h1ωin Q,
di ¯u=0 inQ,
¯u= 0 on Σ,
¯u(0) = u0in Ω,
(1.5)
⎧
⎪
⎪
⎨
⎪
⎪
⎩
−q −∆q+q−(1 + x2)k∧q+∇π=¯u1Oin Q,
di q=0 inQ,
q= 0 on Σ,
q(T)=0 inΩ.
(1.6)
Then he con ol his Φ insensi izing ( esp., Φ ε-insensi izing ) i and only i
q(0) = 0 ( esp., q(0)0,Ω≤ε).(1.7)
Indeed, in iew o (1.2), condi ion (1.3) is equi alen o
T
0O
¯u·uτdx d =0  esp., (1.4) is equi alen o T
0O
¯u·uτdx d ≤ε,
whe e ¯uis he solu ion o (1.5) and uτis he solu ion o (1.1) diffe en ia ed wi h
espec o τ. Using he defini ion o (q,π) and in eg a ing by pa s, we ob ain
Ω
q(0) ·u0dx =0  esp., Ω
q(0) ·u0dx≤ε∀u0∈Hwi h u00,Ω=1.
This is equi alen o (1.7). See [18] o mo e de ail.
No ice ha since ¯u∈L2(0,T;V), we also ha e q∈L2(0,T;W)∩H1(0,T;H) and
π∈L2(0,T;H1(Ω)).
We a e hus in he p esence o a null con ollabili y p oblem ( esp., an app oxima e
con ollabili y p oblem) o a cascade sys em, whe e he con ol his no ac ing di ec ly
in he sys em sa isfied by q( he unc ion we wan o d i e o ze o a e a ime in e al
o leng h T) bu indi ec ly, h ough ¯u1O.
1.3. Main esul s. The e ha e been se e al ecen esul s conce ning he exis-
ence o insensi izing and ε-insensi izing con ols o pa abolic p oblems.
Thus, in [2] he exis ence o ε-insensi izing con ols o linea hea equa ions
wi h pa ially known ini ial and bounda y condi ions was es ablished. The same
was also ob ained o semilinea hea equa ions wi h globally Lipschi z-con inuous
nonlinea i ies. Since hen, i has been p o ed in [18] ha insensi izing con ols exis
o he same equa ions comple ed wi h ze o ini ial da a, unde sui able assump ions
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CONTROLS INSENSITIZING AN OCEAN MODEL 1619
on he sou ce e m. In [3], he au ho s ex ended hese esul s o o he mo e gene al
(sligh ly supe linea ) nonlinea i ies.
In his pape , we deal wi h he insensi izing and ε-insensi izing p oblems o he
case o he S okes- ype equa ions (1.1). Ou esul s we e ske ched in [7]. These a e
he fi s insensi i i y esul s in he li e a u e o equa ions o his ype, as a as we
know.
We will assume ha he ollowing geome ical hypo hesis is sa isfied, as in he
p e ious e e ences:
ω∩O=∅.(1.8)
Ou main esul s a e he ollowing.
Theo em 1.2. Le T>0and assume ha (1.8) is sa isfied. Then, o each
ε>0 he e exis s a con ol h∈L2(ω×(0,T))2which is Φε-insensi izing.
Theo em 1.3. Unde he assump ions o Theo em 1.2, i we also ha e u0=0
and T
0Ω
exp M −4T2dx d < +∞(1.9)
o an app op ia e cons an Mdepending on Ω,ω,O, and T, hen he e exis s a
con ol h∈L2(ω×(0,T))2which is Φinsensi izing.
I was p o ed in [18] o he linea hea equa ion ha , in gene al, we canno
expec he exis ence o insensi izing con ols o non anishing ini ial da a in L2(Ω)
when Ω ω=∅. The p oo o his esul is based on a coun e example o which
he app op ia e obse abili y inequali y ails when he ini ial da a belong o L2(Ω).
Simila a gumen s could be used o S okes sys ems. In iew o his, i is easonable
o impose in Theo em 1.3 ha u0=0.
This pape is o ganized as ollows. In sec ion 2, we p o e Theo em 1.2, whe e
we ob ain a unique con inua ion esul o an adjoin cascade sys em hanks o he
p esence o he Co iolis e m. In sec ion 3, we p o e Theo em 1.3. In his sec ion,
we show ha insensi izing con ols do exis i an app op ia e obse abili y inequali y
holds. We deduce his obse abili y inequali y in sec ion 3.2 by means o an app o-
p ia e global Ca leman inequali y o he same adjoin cascade sys em. The p oo o
his global Ca leman inequali y is gi en in sec ion 3.1 and ollows a chain o es ima es
based on he s eps o he unique con inua ion p oo . A he end o his sec ion and
o be sel -con ained, we gi e he p oo o a s anda d global Ca leman es ima e o
S okes-like sys ems ha is needed in sec ion 3.1. Finally, in sec ion 4, we summa ize
he key poin s o his a icle in some final ema ks.
2. P oo o Theo em 1.2. We can assume wi hou loss o gene ali y ha T=0
and u0= 0 in (1.5)–(1.6). I is well known ha he exis ence o ε-insensi izing con ols
o (1.5)–(1.6) is equi alen o a unique con inua ion p ope y o he associa e adjoin
sys em ⎧
⎪
⎪
⎨
⎪
⎪
⎩
φ −∆φ+φ+(1+x2)k∧φ+∇θ=0 inQ,
di φ=0 inQ,
φ= 0 on Σ,
φ(0) = φ0in Ω,
(2.1)
⎧
⎪
⎪
⎨
⎪
⎪
⎩
−z −∆z+z−(1 + x2)k∧z+∇ =φ1Oin Q,
di z=0 inQ,
z= 0 on Σ,
z(T)=0 inΩ
(2.2)
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1620 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
o a gi en φ0∈H. This coupled sys em possesses a unique solu ion (φ, θ), (z, ),
wi h a leas φ, z ∈L2(0,T;V)∩H1(0,T;V) and θ, ∈W−1,∞(0,T;L2(Ω)). (Again,
θand a e unique up o a dis ibu ion depending only on .)
Using (1.5)–(1.6) and (2.1)–(2.2) he ollowing duali y iden i y is easily deduced:
T
0ω
h·zdxd =Ω
q(0) ·φ0dx ∀h∈L2(ω×(0,T))2.
I is clea om his las iden i y ha he se {q(0) : h∈L2(ω×(0,T))2}is dense in
Hi he ollowing unique con inua ion esul holds.
Lemma 2.1. Assume (1.8).Le (φ, θ),(z, )be he solu ion o (2.1)–(2.2) wi h
φ0∈H. Then, i z=0in ω×(0,T), we necessa ily ha e z≡φ≡0and ∇ ≡∇θ≡0
in Q.
P oo . This is a di ec consequence o a mo e gene al unique con inua ion esul .
To s a e his esul p ecisely, le ω=ω∩O=∅and le us se
C1(ω)={(x1,x
2)∈Ω:∃x0
1s. . (x0
1,x
2)∈ω},Σ1(ω)=(Γ∩C1)×(0,T).(2.3)
(C1(ω) is he ho izon al componen o ω.) We will p o e ha i φ=(φ1,φ
2)is
oge he wi h θ,z, and a solu ion o
⎧
⎨
⎩
φ −∆φ+φ+(1+x2)k∧φ+∇θ=0 inQ,
di φ=0 inQ,
φ1= 0 on Σ1,
(2.4)
−z −∆z+z−(1 + x2)k∧z+∇ =φ1ωin Q,
di z=0 inQ,
and z=0inω×(0,T), hen φ≡0.
To p o e his asse ion, we di ide he p oo in o wo s eps. Wi hou loss o
gene ali y, we can assume ha ωis connec ed; o he wise we would eplace ωby one
o i s connec ed componen s.
In a fi s s ep, we deduce om he ac ha z=0inω×(0,T) ha φ2= 0 and
φ1is cons an i hey a e es ic ed o ω×(0,T). Thus, since z=0inω×(0,T)we
no ice ha cu l φ=0inω×(0,T) by applying he cu l ope a o in he equa ion o
zin (2.4). Using his ac , i we now apply he cu l ope a o o he fi s equa ion in
(2.4), hanks o he p esence o he Co iolis e m we ob ain ha
cu l ((1 + x2)k∧φ)=φ2+ di φ=φ2=0
in ω×(0,T). Now, since di φ= 0 and cu l φ=0inω×(0,T), we ha e ∇φ1=0in
ω×(0,T). The e o e φ1is cons an in ω×(0,T) and we ce ainly ob ain φ= (Cons .,0)
in ω×(0,T).
In a second s ep, le us in oduce
ψ=∂φ
∂x1
,π=∂θ
∂x1
(2.5)
and he coefficien ma ix:
a=1−(1 + x2)
(1 + x2)1
∈L∞
loc(Q).(2.6)
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CONTROLS INSENSITIZING AN OCEAN MODEL 1621
Then we ha e ψ −∆ψ+aψ +∇π=0 inQ,
di ψ=0 inQ,
(2.7)
(ψ,π)∈L2
loc(Q)2×D
(Q)(2.8)
wi h ψ=0inω×(0,T). He e, we use a sha p uniqueness p ope y o he S okes
sys em (2.7) p o ed in [5] ha says ha , unde he egula i y de e mined by (2.6)
and (2.8), one has ψ≡0inQ. Now, om (2.5) we ob ain ∂φi/∂x1≡0 o i=1,2in
Q. Since di φ=0inQwe also ha e ∇φ2=0inQand, om he ac ha φ2=0in
ω×(0,T), we deduce ha φ2≡0inQ( ecall ha Ω is connec ed).
On he o he hand, since ∂φ1/∂x1=0inQand φ1= 0 on Σ1, we see ha φ1=0
in C1×(0,T). Finally we ha e φ=(φ1,φ
2)=0inC1×(0,T), which is an open
subse o Q. We can conclude ha φ≡0inQusing again he uniqueness p ope y
o [5]. (We can also use he e he weake esul p o ed in [4].)
Rema k 1. The me hod used in he second pa o he p oo o Lemma 2.1 leads
o he ollowing uniqueness p ope y in any dimension n. Le (φ, θ) be he solu ion o
⎧
⎨
⎩
φ −∆φ+aφ+∇θ=0 inQ,
di φ=0 inQ,
φ= 0 on Σ1(ω),
(2.9)
whe e Q=Ω×(0,T), Ω is a nonemp y open bounded connec ed subse o Rn,ωis
an open nonemp y subse o Ω, Σ1and C1a e as defined in (2.3), and a∈L∞(Q). I
ais a unc ion independen o x1in Qand φis independen o x1in ω×(0,T), hen
φ anishes in Q. Indeed, le us in oduce ψ=∂φ/∂x1,π=∂θ/∂x1, which sa is y
a S okes p oblem simila o (2.9), and his p oblem does no in ol e φexplici ly
since ais independen o x1. Now, om he uniqueness p ope y in [5], ψ≡0inQ.
Consequen ly ∂φ/∂x1=0inQand φ= 0 on Σ1,soweha eφ=0inC1×(0,T).
Using he unique con inua ion p ope y in [5] once again, we ob ain ha φ≡0inQ.
Rema k 2. The p e ious ema k shows ha he Co iolis e m plays a c ucial
ole only in he fi s pa o he p oo o Lemma 2.1. In ac , he p esence o he
Co iolis e m allows us o p o e ha cu l φ=0inω×(0,T) implies ha he second
componen o φ anishes in ω×(0,T). This will also be impo an in he deduc ion
o he Ca leman inequali y la e .
Rema k 3. In he p oo o he p e ious lemma, i is no possible o use he
esul s o [4] conce ning uniqueness p ope ies o he S okes sys em when one o he
componen s o φ anishes in ω×(0,T). This is because he esul s in [4] equi e ha
he coefficien a, in oduced in (2.6), sa is y a12 =0.
3. P oo o Theo em 1.3. The p oo o he exis ence o insensi izing con ols
o (1.1), i.e., he exac null con ollabili y o (1.5)–(1.6), elies on he ollowing
obse abili y esul o he cascade adjoin sys em (2.1)–(2.2).
P oposi ion 3.1. Assume ha ω∩O =∅. The e exis posi i e cons an s Mand
K, depending only on Ω,ω,O, and T, such ha he inequali y
T
0Ω
exp −M −4|z|2dx d ≤KT
0ω
|z|2dx d (3.1)
holds o e e y solu ion o (2.1)–(2.2) wi h φ0∈H.
The p oo o his esul is based on a global Ca leman inequali y (see Theo-
em 3.3), as will be seen in sec ion 3.2. This Ca leman inequali y will be p o ed in
sec ion 3.1.
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1622 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
Le us now gi e he p oo o Theo em 1.3 using P oposi ion 3.1. Thus, le us
assume ha (1.8) is sa isfied, u0= 0, and (1.9) holds wi h Mbeing he cons an
u nished by P oposi ion 3.1.
The app oxima e con ol ho minimal no m in L2(ω×(0,T))2co esponding o
u0= 0, a sou ce e m Tsa is ying (1.9), and ole ance ε>0 can be ob ained by
minimizing in L2(Ω)2 he ollowing con ex unc ional [6, 14]:
Jε(φ0)=1
2T
0ω
|z|2dx d +T
0Ω
T·zdxd +εφ00,Ω.(3.2)
Thus, he minimum o Jεis a ained a some 
φ0ε∈L2(Ω)2. We deno e by (
φε,
θε),
(zε, ε) he co esponding solu ion o (2.1)–(2.2) wi h φ0=
φ0ε; hen he con ol
unc ion defined as
hε=zε1ω
(3.3)
is such ha he associa ed solu ion (¯uε,¯pε), (qε,π
ε) o (1.5)–(1.6) wi h u0= 0 sa isfies
qε(0)0,Ω≤ε.
I is no difficul o see ha
lim in
φ00,Ω→∞
Jε(φ0)
φ00,Ω
≥ε.
The p oo o his inequali y is classical; see [6]. I is implied by he unique con inua ion
p ope y o he cascade adjoin sys em ha we p esen ed abo e (see Lemma 2.1).
Fu he mo e, he ollowing op imali y condi ion mus be sa isfied a 
φ0ε:
T
0ω
|zε|2dx d +T
0Ω
T·zεdx d +ε
φ0ε0,Ω=0.(3.4)
By eplacing (3.3) in (3.4), in oducing he weigh eM −4, and using (3.1) and Young’s
inequali y, we easily deduce ha
T
0ω
|hε|2dx d ≤K2T
0Ω
exp(M −4)|T |2dx d .
Since {hε}is uni o mly bounded in L2(ω×(0,T))2, hen up o a subsequence, s ill
deno ed {hε},weha e
hεh weakly in L2(ω×(0,T))2,
¯uε→¯us ongly in L2(Q)2,and
qε→qs ongly in L2(Q)2,
as ε→0. O cou se, we ha e deno ed he e by (¯uε,¯pε), (qε,π
ε) and (¯u, ¯p), (q,π)
he solu ions o (1.5)–(1.6) associa ed wi h hεand h, espec i ely. No ice ha
qε(0)0,Ω≤εand consequen ly we ha e q(0) = 0. This ends he p oo o Theo-
em 1.3.
3.1. A global Ca leman es ima e. The goal o his sec ion is o p esen an es-
ima e o he Ca leman kind o he solu ions o he adjoin cascade sys em (2.1)–(2.2).
As men ioned abo e, his es ima e will be c ucial o he p oo o P oposi ion 3.1.
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CONTROLS INSENSITIZING AN OCEAN MODEL 1623
Le us fi s in oduce an open ball B0such ha B0⊂⊂ ω∩O and an auxilia y
unc ion η0∈C
2(Ω) sa is ying
η0(x)>0∀x∈Ω,η
0=0 on∂Ω,|∇η0(x)|>0∀x∈Ω B0.(3.5)
The exis ence o such a unc ion is p o ed in [9].
Le us also in oduce he weigh unc ions
α(x, )=e2λη0∞−eλη0
4(T− )4,α( ) = min
Ω
α(x, ),α
∗( ) = max
Ω
α(x, ),
ϕ(x, )= eλη0
4(T− )4,ϕ( ) = max
Ω
ϕ(x, ),ϕ
∗( ) = min
Ω
ϕ(x, ).
The ollowing p ope y o he unc ions α∗and αwill be needed la e .
Lemma 3.2. Fo any a>1 he e exis s λa>0such ha
aα( )>α
∗( )∀λ>λ
a,∀ ∈(0,T).
P oo . The p oo is elemen a y. I suffices o no ice ha we ha e a(e2x−ex)>
e2x−1i a>1 and xis sufficien ly la ge.
The main esul in his sec ion is he ollowing.
Theo em 3.3. Assume ha ω∩O=∅and le he unc ions α,ϕ,α, and ϕbe
as abo e. Fo each γ∈(0,1), he e exis cons an s s,
λ, and 
Cdepending on Ω,ω,
O,T, and γsuch ha one has
T
0Ω
e−2sα 1
sϕ(|z |2+|∆z|2)+sλ2ϕ|∇z|2+s3λ4ϕ3|z|2dx d
+T
0Ω
e−2sα 1
sϕ(|φ |2+|∆φ|2)+sλ2ϕ|∇φ|2+s3λ4ϕ3|φ|2dx d
≤
CT
0ω
e−(1+γ)sαs63λ32 ϕ67|z|2dx d (3.6)
o any s>sand λ>
λand o e e y solu ion (φ, θ),(z, ) o (2.1)–(2.2) associa ed
wi h ini ial da a φ0∈H.
The p oo will be di ided in se e al s eps and will be gi en in he ollowing
subsec ions. Fi s , we will apply a global Ca leman es ima e o he S okes sys em o
(2.1) and (2.2). This will lead o he es ima e (3.10). Then, o deduce (3.6), we will
ha e o es ima e he in eg al in he igh -hand side o (3.10) con aining φin e ms
o z. To his end, we will ollow he s eps o he p oo o Lemma 2.1 in e e se o de .
3.1.1. S ep 1: A fi s di ec Ca leman es ima e. Le I(s, λ; ) s and o
he quan i y
I(s, λ; )=T
0Ω
e−2sα 1
sϕ(| |2+|∆ |2)+sλ2ϕ|∇ |2+s3λ4ϕ3| |2dx d (3.7)
o any posi i e sand λand any sufficien ly egula unc ion = (x, ). We hen
ha e he ollowing.
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1624 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
Lemma 3.4. Fo each γ1∈(0,1) he e exis posi i e cons an s s1,λ1, and C1,
depending on Ω,ω,O,T, and γ1, wi h he ollowing p ope ies:
I(s, λ;z)≤C1T
0B0
e−(1+γ1)sαs7λ4ϕ15/2|z|2dx d
+T
0B0
e−2sα(sλϕ)2|φ|2dx d (3.8)
+T
0O
e−2sα (sϕ)1/2|φ|2+1
s3ϕ7/2|φ |2dx d 
and
I(s, λ;φ)≤C1T
0B0
e−(1+γ1)sαs7λ4ϕ15/2|φ|2dx d (3.9)
o any s>s
1and λ>λ
1and o e e y solu ion o (2.1)–(2.2) wi h φ0∈H.
The p oo o Lemma 3.4 is simila o he p oo o o he ecen global Ca leman
inequali ies o he S okes sys em. The main ideas a e due o Imanu ilo [10, 11];
also see [8] o o he ela ed esul s. The p oo is p esen ed in he appendix.
Le us fix γ, wi h 0 <γ<1. We a e now going o deduce se e al es ima es ha
hold o “sufficien ly la ge sand λ.” By his we mean ha hey a e sa isfied o any
s>¯sand any λ>¯
λ, whe e ¯sand ¯
λa e (la ge) posi i e cons an s depending only on
Ω, ω,O,T, and γ.
In wha ollows, Cdeno es a gene ic cons an , no necessa ily he same a each
occu ence, depending on Ω, ω,O,T, and (possibly) γ.
Le γ1be gi en in (γ,1). In iew o Lemma 3.4 applied o γ1,wege
I(s, λ;z)+I(s, λ;φ)≤CT
0B0
e−(1+γ1)sαs7λ4ϕ15/2(|z|2+|φ|2)dx d (3.10)
o sand λla ge enough.
Indeed, he las wo in eg als in (3.8) can be abso bed by he le -hand side o
I(s, λ;φ), since
Cs−3ϕ−7/2≤1
2(sϕ)−1and C(sϕ)1/2≤1
2s3ϕ3
o sufficien ly la ge s.
3.1.2. S ep 2: An es ima e o φin e ms o cu l φ.To simpli y he no a-
ion, le us se a= 7 and b=15/2. Then
I(s, λ;z)+I(s, λ;φ)≤CT
0B0
e−(1+γ1)sαsaλ4ϕb(|z|2+|φ|2)dx d .(3.11)
We will deno e by B1,B
2,... a sequence o balls cen e ed a he same poin as
B0and sa is ying
B0⊂⊂ B1⊂⊂ · · · ⊂⊂ ω∩O.
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CONTROLS INSENSITIZING AN OCEAN MODEL 1631
Le us fi s p o e ha he e exis posi i e cons an s M,C1such ha
T/2
0Ω
exp(−M −4)|z|2dx d +T
T/2Ω
|φ|2dx d ≤C1T
0ω
|z|2dx d .(3.31)
Fo his es ima e, le us fi s no ice ha o some cons an s Mand C, one has
e−2sα(x, )ϕ(x, )3≥Ce−M −4∀(x, )∈Ω×(0,T/2);
his is easy o see, in iew o he defini ions o αand ϕ. Now, using (3.6), we ge
T/2
0Ω
exp(−M −4)|z|2dx d ≤1
s3λ4I(s, λ;z)
≤CK T
0ω
e−(1+γ)sαs63 ϕ67|z|2dx d ,
and since he weigh e−(1+γ)sαϕ67 is bounded, we can es ima e he fi s e m in he
le -hand side o (3.31). On he o he hand, o ob ain an es ima e o φin e ms o z,
le us ecall he inequali y (3.6). Since e−2sα −12(T− )−12 is bounded om below
a om = 0 and =T, in iew o (3.30), we ha e
T
T/2Ω
|φ|2dx d ≤3T/4
T/4Ω
|φ|2dx d
≤C3T/4
T/4Ω
e−2sαs3λ4ϕ3|φ|2dx d ≤CT
0ω
e−(1+γ)sαϕ67|z|2dx d .
As be o e, om he ac ha e−(1+γ)sαϕ67 is bounded, we a e able o es ima e he
second e m in he le -hand side o (3.31).
Finally, he desi ed obse abili y inequali y (3.1) is ob ained using he ene gy
es ima e (3.29) and (3.31):
T
0Ω
exp(−M −4)|z|2dx d ≤T/2
0Ω
exp(−M −4)|z|2dx d +T
T/2Ω
|z|2dx d
≤CT/2
0Ω
exp(−M −4)|z|2dx d +T
T/2Ω
|φ|2dx d

≤CT
0ω
|z|2dx d .
Appendix. P oo o Lemma 3.4. Le us ecall ha his p oo is gi en o
he sake o comple eness, bu i is essen ially an adap a ion o ou amewo k o he
a gumen s p esen ed in [8] and [11]. Le us conside he sys em
⎧
⎪
⎪
⎨
⎪
⎪
⎩
−z −∆z+z−(1 + x2)k∧z+∇ =φ1Oin Q,
di z=0 inQ,
z= 0 on Σ,
z(T)=0 inΩ,
(3.32)
whe e φ∈L2(0,T;W)∩H1(0,T;H).
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1632 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
Recall ha B0is an open ball sa is ying B0⊂⊂ ω∩O and he auxilia y unc ion
η0sa isfies η0∈C
2(Ω),
η0(x)>0∀x∈Ω,η
0=0 on∂Ω,|∇η0(x)|>0∀x∈Ω B0.
We will need an addi ional open ball B00 ⊂⊂ B0, such ha we s ill ha e
|∇η0(x)|>0∀x∈Ω B00 .
We will di ide he p oo o Lemma 3.4 in o se e al s eps.
S ep 1. Following [8], we apply some well-known Ca leman es ima es o he hea
equa ion o (3.32). Thus, he e exis cons an s s0,λ0, and C>0 depending on Ω,
ω, and Tsuch ha o e e y λ>λ
0and s>s
0, he ollowing es ima e holds:
I(s, λ;z)≤CT
0B00
e−2sαs3λ4ϕ3|z|2dx d
+T
0Ω
e−2sα |∇ |2+|(1 + x2)k∧z|2+|φ1O|2dx d .(3.33)
Recall ha he defini ions o I(s, λ;z) and he weigh s αand ϕa e gi en in sec ion 3.1.
O cou se, we can choose sla ge enough o abso b he p e ious e m |(1+x2)k∧z|2
wi h he le -hand side (3.33). We hen ha e
I(s, λ;z)≤CT
0B00
e−2sαs3λ4ϕ3|z|2dx d
+T
0Ω
e−2sα|∇ |2dx d +T
0O
e−2sα|φ|2dx d 
(3.34)
o any λ>λ
0and any s>s
01 .
S ep 2. To es ima e he p essu e g adien ∇ in (3.34), we fi s apply he di e -
gence ope a o o (3.32), i.e., we w i e
∆ ( ) = di ((1 + x2)k ∧z)( )inΩ, ∈(0,T),(3.35)
and hen we use he ollowing esul by Imanu ilo and Puel [12], which is sa isfied
by weak solu ions o second o de ellip ic equa ions.
Lemma 3.5. Le usse β(x)=eλη0(x)and le ∈H1(Ω) be a solu ion o
∆ = di hin Ω,(3.36)
whe e h∈L2(Ω)2. Then he e exis posi i e cons an s τ2,λ01, and Csuch ha
Ω
e2τβ|∇ |2dx ≤CτΩ
e2τββ|h|2dx +τ1/2e2τg2
1/2,∂Ω
+τ2λ2B00
e2τββ2| |2dx +B00
e2τβ|∇ |2dx
(3.37)
o any τ>τ
2and any λ>λ
01 , whe e g= |∂Ω.
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CONTROLS INSENSITIZING AN OCEAN MODEL 1633
In pa icula , we ha e he ollowing o ( ) and g( )= ( )|∂Ω:
Ω
e2τβ|∇ ( )|2dx ≤CτΩ
e2τββ|(1 + x2)k∧z( )|2dx
+τ1/2e2τg( )2
1/2,∂Ω+τ2λ2B00
e2τββ2| ( )|2dx
+B00
e2τβ|∇ ( )|2dx.(3.38)
To es ima e he las in eg al in (3.38), le us in oduce an open se B01 such ha
B00 ⊂⊂ B01 ⊂⊂ B0and a unc ion ξ01 ∈C
2
0(B01) such ha
0≤ξ01 ≤1 and ξ01 =1inB00 .
In eg a ing by pa s, i ollows om (3.35) ha
B00
e2τβ|∇ ( )|2dx ≤B01
e2τβξ01|∇ ( )|2dx
=−B01
e2τβξ01 di ((1 + x2)k ∧z)( ) ( )dx
−1
2B01
e2τβ∇ξ01 ·∇| ( )|2dx −B01
ξ01∇e2τβ ·∇| ( )|2dx.
In eg a ing again by pa s, applying Young’s inequali y, and aking in o accoun ha
|∆(e2τβξ01)|≤Cτ2λ2β2e2τβ o some posi i e cons an C, a e some s aigh o wa d
compu a ions we deduce ha
B00
e2τβ|∇ ( )|2dx ≤Cτ2λ2B01
e2τββ2| ( )|2dx +B01
e2τβ|z( )|2dx.
Replacing his inequali y in (3.38), we ob ain he ollowing o each ∈(0,T):
Ω
e2τβ|∇ ( )|2dx ≤CτΩ
e2τββ|z( )|2dx
+τ1/2e2τg( )2
1/2,∂Ω
+τ2λ2B01
e2τββ2| ( )|2dx.
Now, le us pu τ=s/( 4(T− )4) and le us choose s>s
02 = max(s01 ,τ
2(T/2)8).
Then τ>τ
2. Le us mul iply by exp(−2sexp(2λη0∞)/( 4(T− )4)) he p e ious
inequali y and le us in eg a e wi h espec o in (0,T). This leads o he es ima e
T
0Ω
e−2sα|∇ |2dx d ≤CT
0Ω
e−2sαsϕ|z|2dx d
+T
0
e−2sα∗(sϕ∗)1/2g( )2
1/2,∂Ωd
+T
0ω1
e−2sα(sλϕ)2| |2dx d ,(3.39)
whe e α∗and ϕ∗we e in oduced in sec ion 3.1.
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1634 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
The fi s e m in he igh -hand side o (3.39) can be abso bed by he le -hand
side I(s, λ;z) in (3.33) o sla ge enough. Hence, we ob ain
I(s, λ;z)≤CT
0ω0
e−2sαs3λ4ϕ3|z|2dx d +T
0
e−2sα∗(sϕ∗)1/2g( )2
1/2,∂Ωd
+T
0ω1
e−2sα(sλϕ)2| |2dx d +T
0O
e−2sα|φ|2dx d 
(3.40)
o any λ>λ
01 and any s>s
03 .
S ep 3. S ep 3 es ima es he no m o he ace o he p essu e on he bounda y.
To his end, we in oduce h ee new unc ions:
χ( )=e−sα∗( )(sϕ∗( ))1/4,˜z=χ( )z, ˜ =χ( ) .
F om (3.32), we see ha (˜z, ˜ ) sa isfies
⎧
⎪
⎪
⎨
⎪
⎪
⎩
−˜z −∆˜z+˜z+∇˜ =−χz+χ(1 + x2)k∧z+χφ1Oin Q,
di ˜z=0 inQ,
˜z= 0 on Σ,
˜z(T)=0 inΩ.
Using he con inui y o he ace ope a o and s anda d a p io i es ima es o he
p essu e, we deduce ha
T
0
˜ ( )2
1/2,∂Ωd ≤T
0
˜ ( )2
1,Ωd
≤CT
0Ω
e−2sα∗s5/2(ϕ∗)3|z|2dx d
+T
0O
e−2sα∗(sϕ∗)1/2|φ|2dx d .
We ha e used he e ha |χ( )|2≤Ce−2sα∗s5/2(ϕ∗( ))3 o all ∈(0,T). We hus
ob ain a new es ima e om (3.40):
I(s, λ;z)≤CT
0B00
e−2sαs3λ4ϕ3|z|2dx d +T
0B01
e−2sα(sλϕ)2| |2dx d
+T
0O
e−2sα(sϕ)1/2|φ|2dx d 
(3.41)
o any λ>λ
01 and any s>s
04 .
S ep 4. I emains o es ima e he local e m in he igh -hand side o (3.41)
con aining | |2in e ms o zand φ.
Assume ha he p essu e has been no malized in such a way ha
B01
( )dx =0 ∀ ∈(0,T).
Then he e exis s C>0 such ha
B01
| ( )|2dx ≤CB01
|∇ ( )|2dx ∀ ∈(0,T)
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CONTROLS INSENSITIZING AN OCEAN MODEL 1635
and also
T
0B01
e−2sα(sλϕ)2| |2dx d ≤CT
0B01
e−2sα(sλϕ)2|∇ |2dx d ,
whe e he unc ions α=α( ) and ϕ=ϕ( ) we e in oduced in sec ion 3.1.
F om (3.32), we see ha
T
0B01
e−2sα(sλϕ)2|∇ |2dx d ≤CT
0B01
e−2sα(sλϕ)2(|z|2+|φ|2)dx d
+T
0B01
e−2sα(sλϕ)2(|z |2+|∆z|2)dx d .
The e o e, in iew o (3.41), we ob ain
I(s, λ;z)≤CT
0B01
e−2sαs3λ4ϕ3|z|2+(sλϕ)2|φ|2dx d
+T
0B01
e−2sα(sλϕ)2(|z |2+|∆z|2)dx d
+T
0O
e−2sα(sϕ)1/2|φ|2dx d .(3.42)
S ep 5. The es o he p oo deals wi h he es ima es o he local in eg als
con aining |∆z|2and |z |2. Fi s , we will be conce ned wi h |∆z|2.
Le us in oduce a unc ion ξ0∈C
4
0(B0) such ha
0≤ξ0≤1 and ξ0=1inB01 .
Le us se z(x, )=e−sαϕξ
0∆z(T− ). We wan o es ima e he no m zL2(B01×(0,T ))2.
Following he a gumen s in [8] (see S ep 4), we can deduce ha
T
0B01
e−2sα(sλϕ)2|∆z|2dx d =T
0B01
s2λ2|z|2dx d
≤CT
0B0
e−2sαs4λ2ϕ9/2|z|2dx d +T
0B0
e−2sα(sλϕ)2|φ|2dx d .
(3.43)
Thus, om (3.42) we ha e
I(s, λ;z)
≤CT
0B0
e−2sαs4λ4ϕ9/2|z|2dx d +T
0B0
e−2sα(sλϕ)2|φ|2dx d
+T
0B01
e−2sα(sλϕ)2|z |2dx d +T
0O
e−2sα(sϕ)1/2|φ|2dx d .(3.44)
S ep 6. Now we wan o es ima e |z |2. Due o he egula i y p ope ies o φ,we
can use he e a mo e s aigh o wa d a gumen han in [8], whe e he igh -hand side
belongs only o L2(Q)2.
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1636 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
Fi s , no ice ha
T
0B01
e−2sα(sλϕ)2|z |2dx d ≤δT
0B01
e−2sα 1
sϕ|z |2dx d
+δT
0B01
e−2sα∗1
s3(ϕ∗)7/2|z |2dx d
+CδT
0B01
e−4sα∗+2sα∗s7λ4ϕ15/2|z|2dx d .
This is easily ob ained by in eg a ing by pa s in ime. We will la e choose δ>0
small enough.
We ha e he ollowing auxilia y esul .
Lemma 3.6. Le (z, )be he solu ion o (3.32). Then he ollowing es ima e
holds:
T
0Ω
e−2sα∗1
s3(ϕ∗)7/2|z |2dx d
≤CI(s, λ;z)+T
0O
e−2sα∗1
sϕ∗|φ|2+1
s3(ϕ∗)7/2|φ |2dx d .(3.45)
P oo . Mul iply (3.32) by e−2sα∗s−2(ϕ∗)−9/4z and in eg a e in Q. No icing ha
(e−2sα∗(ϕ∗)−9/4) ≤Ce−2sα∗s(ϕ∗)−1,
a e some compu a ions we deduce ha
T
0Ω
e−2sα∗1
s2(ϕ∗)9/4|∇z |2dx d
≤CT
0Ω
e−2sα∗1
sϕ∗(|z|2+|z |2)dx d
+T
0Ω
e−2sα∗s(ϕ∗)1/4|∇z|2dx d +T
0O
e−2sα∗1
sϕ∗|φ|2dx d 
+1
2T
0Ω
e−2sα∗1
s3(ϕ∗)7/2|z |2dx d .(3.46)
On he o he hand, i we compu e he ime de i a i e o (3.32) and hen we
mul iply he esul by e−2sα∗s−3(ϕ∗)−7/2z , we find ha
T
0Ω
e−2sα∗1
s3(ϕ∗)7/2|z |2dx d
≤T
0Ω
e−2sα∗1
s2(ϕ∗)9/4|∇z |2dx d (3.47)
+CT
0Ω
e−2sα∗1
sϕ∗|z |2dx d +T
0O
e−2sα∗1
s3(ϕ∗)7/2|φ |2dx d .
F om (3.46) and (3.47), we see ha (3.45) holds.
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CONTROLS INSENSITIZING AN OCEAN MODEL 1637
In iew o his lemma, we ha e
T
0B01
e−2sα(sλϕ)2|z |2dx d
≤CδI(s, λ;z)+T
0O
e−2sα∗1
sϕ∗|φ|2+1
s3(ϕ∗)7/2|φ |2dx d 
+CδT
0B01
e−4sα∗+2sα∗s7λ4ϕ15/2|z|2dx d .
I we assume ha γ1<1, hen (3−γ1)/2>1, and om Lemma 3.2 we deduce ha
(3 −γ1)α/2>α
∗ o sufficien ly la ge λ,say,λ>λ
02 . Consequen ly, −4α+2α∗<
−(1 + γ1)αand
T
0B01
e−2sα(sλϕ)2|z |2dx d
≤CδI(s, λ;z)+T
0O
e−2sα∗1
sϕ∗|φ|2+1
s3(ϕ∗)7/2|φ |2dx d 
+CδT
0B01
e−(1+γ1)sαs7λ4ϕ15/2|z|2dx d
o any λ>λ
02 and any s>s
04 .
F om (3.44) and his es ima e, choosing δ>0 small enough, we find
I(s, λ;z)
≤CT
0B0
e−(1+γ1)sαs7λ4ϕ15/2|z|2dx d +T
0B0
e−2sα(sλϕ)2|φ|2dx d
+T
0O
e−2sα (sϕ)1/2|φ|2+1
s3(ϕ∗)7/2|φ |2dx d 
o all λ>λ
02 and s>s
04 .
Ob iously, his yields (3.8). The p oo o (3.9) is e y simila and in ac much
simple , since he le -hand side o (2.1) is ze o.
Thus, we ha e p o ed Lemma 3.4 o λ1=λ02 and s1=s04 ( wo pa ame e s
depending on Ω, ω,O, and T).
4. Some final ema ks. The geome ical hypo hesis ω∩O=∅is equi ed o
p o e he exis ence o bo h ε-insensi izing and insensi izing con ols. In he fi s case,
his assump ion is used o p o e a unique con inua ion p ope y (Lemma 2.1). In
he case o insensi izing con ols, i is used o p o e an obse abili y inequali y. The
p oblem is comple ely open when ω∩O=∅(see [18]).
The exis ence o insensi izing con ols is gua an eed by he null con ollabili y
p ope y o a cascade sys em o quasi-geos ophic equa ions (1.5)–(1.6). In his case,
he con ol ac s indi ec ly on one a iable h ough he o he one. O cou se, his
con ollabili y p ope y is s onge han he null con ollabili y o a single quasi-
geos ophic sys em.
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1638 E. FERN´
ANDEZ-CARA, G. C. GARCIA, AND A. OSSES
To p o e he null con ollabili y p ope y o he cascade sys em, he e a e wo
main difficul ies.
Fi s is he need o a unique con inua ion esul o he adjoin sys em
(2.2)–(2.1). The p esence o he Co iolis e m pe mi s us o ela e he second compo-
nen o he eloci y and i s associa ed o ici y, and his is a key poin in he p oo
o uniqueness (see Rema k 2).
The second p oblem is he need o an obse abili y inequali y o he adjoin .
This inequali y comes om an app op ia e (global) Ca leman es ima e. The main
idea is o es ima e φin e ms o cu l φin a ball con ained in ω∩Oin he igh -hand
side o (3.10). This is possible again due o he p esence o he Co iolis e m (in ac ,
ou me hod does no wo k in he case o he usual S okes equa ions). We ew i e he
sys em using he s eam unc ion and he o ici y and we see ha he Co iolis e m
leads o an exp ession o he ho izon al de i a i e o he s eam unc ion in e ms o
he o ici y. In his way, we a e able o a oid es ima es o p essu e e ms, which
a e in gene al e y ha d o deduce (see he appendix in sec ion 3). Mo eo e , he
weigh in he igh -hand side o (3.10) is la ge han he weigh in he le -hand side.
Acco dingly, he e ms in he igh canno be abso bed di ec ly as in he case o he
hea equa ion (see [18]) and his ac equi es some addi ional wo k.
Acknowledgmen s. The au ho s wish o hank J.-P. Puel o he Labo a oi e de
Ma h´ema iques Appliqu´ees, Uni e si ´e Ve sailles/Sain Quen in-en-Y elines (F ance)
and S. Gue e o o he Depa amen o de Ecuaciones Di e enciales y An´alisis Num´e ico,
Uni e sidad de Se illa (Spain), o e y use ul discussions.
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