On the Non-Homogeneous Stationary Kuramoto-Sivashinsky Equation

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1 On the Non-Homogeneous Stationary Kuramoto-Sivashinsky Equation A. Cheskidov and C. Foias Department of Mathematics, Indiana University, Rawles Hall, Bloomington, IN, 4745, USA Abstract In this note we give some explicit estimates for the L -norm of the periodic solutions of the time-independent non-homogeneous Kuramoto-Sivashinsky equation. In particular, we give an estimate of the Michelson s upper bound of all periodic solutions of the time-independent homogeneous Kuramoto-Sivashinsky equation. Key words: Kuramoto-Sivashinsky Equations; Global attractor; Michelson s constant 1 Introduction The Kuramoto-Sivashinsky equation t U + 4 U + U + 1 U = (1.1) has been independently discovered by Kuramoto and Tsuzuki [11], and by Sivashinsky [15] in the study of a reaction diffusion system and flame front propagation respectively as well as in the study of D Kolmogorov fluid flows [16]. Corresponding author. acheskid@indiana.edu. Preprint submitted to Physica D 1 December

2 In fact in [16], one considered a slightly modified Kolmogorov flow U =(v, w) given by the equations v t + vv x + wv y = p x + R 1 v µr 1 v R 1 sin y w t + vw x + ww y = p y + R 1 w µr 1 w (1.) v x + v y =, where R stands for the Reynolds number and µ>isasmallfrictioncoefficient, under the rescaling µ = λɛ 4, ξ = ɛx, τ = ɛ 4 t with a constant λ. The stream function Ψ(x, y) is assumed to have the form Ψ(x, y) =cosy + A(ξ + cη, τ)+o(ɛ) with another constant c. Then it is shown that U(ζ,s) = satisfies the equation c A( 6ζ,6 s) U s + U ζζζζ + (( (3c) Uζ )U ζ ) ζ Uζ + λ U =. (1.3) 6 This remarkable equation becomes the one dimensional version of (1.1) in case c, λ. In this case it can be written in the following way u t + u xxxx + u xx + uu x =, (1.4) where u = U. As argued in [16], this equation provides a good model for the weak turbulent effects observed for the flow in (1.). The equation (1.4) turned out to be a very fruitful subject of research. Periodic boundary conditions for (1.1) yield periodic boundary conditions for (1.4), i.e. u(x, t) =u(x + L, t), x, t, (1.5) where L is the period in the space variable and the supplementary condition L u(x)dx =. (1.6) Under these conditions the equation (1.4) has, once the period L is large enough, a very complicated global attractor A L which seems to be amenable to computer based investigations. The complexity of A L was observed in [8] and later in low-dimensional approximate inertial forms in [1]. This approach

3 allowed the study of several global bifurcations of A L [4]. Moreover, the mathematical study of the equation, initiated in [13] also leads to some very interesting results in [13], [5], [6], [], [1], [7], [9] as well as challenging conjectures in [14], [3], [7]. For instance: Does there exist a universal constant K such that for any u A L one has u(x) K, x R. (1.7) An affirmative answer to this question would give immediate positive answers to the conjectures that the fractal dimension of the A L scales as L [14] and (via [7]) that all elements of A L are analytic functions in x with convergence radius everywhere larger that an absolute positive constant [3]. Both these conjectures have strong computational support. In the remarkable paper [1], Michelson has taken a first step in proving (1.7) for all u A L, namely he has proven that there exists a constant K M such that (1.7) holds for all stationary solutions of (1.4) with K = K M. The next step would be to prove that the set { ū = } uµ(du); µ = invariant probability measure on A L, L > (1.8) is bounded in L (R). To solve this problem one must study the non-homogeneous Kuramoto-Sivashinsky equation. In this note we extend Michelson s result to this latter equation and give a positive partial answer to the preceding problem. In fact, we study the non-homogeneous stationary Kuramoto-Sivashinsky equation u (x)+u (x)+u(x)u (x) =f(x) x R (1.9) with the periodic boundary conditions (1.5) and the supplementary condition (1.6). Our main objective is to study the periodic solutions of (1.9) and their dependence on f. We will prove that the existence of periodic solutions puts some constraints on the function f. Our method is based on elementary estimates and is more direct than Michelson s. In particular, it yields an explicit estimate for the Michelson constant K M,namelyK M 9. (see Theorem 5.3 below). 3

4 Integral Representation Integrating equation (1.9), we get u + u + 1 u = 1 F, (.1) where x F (x) = f(y)dy +const. (.) Periodicity of u implies that F is also periodic with the same period L. Integrating over the period one more time, we obtain L F (x)dx = L u (x)dx. (.3) Let F min =min x F (x), F max =maxf (x). (.4) x Equation (.3) implies F max. Let c F max, (.5) p(x)= c F (x), x R. (.6) Then the equation (.1) can be written as u + u + 1 u + 1 p = 1 c, (.7) where p(x) is periodic. Let y := u c. Then we have that y + y + cy = 1 ( y + p ). (.8) The solutions of the homogeneous part y + y + cy =are y 1 = e bx, y = e b x cos βx, and y 3 = e b x sin βx, 4

5 where b is the positive solution of b 3 + b = c and β = 3 4 b +1. By the change of variables v(ξ) = 1 ( ) ξ c u, q(ξ) = 1 ( ) ξ β c p, w(ξ) =v(ξ) 1, (.9) β the equation (.7) becomes v + 1 β v = 1 δ(1 v q ), (.1) where δ = c β 3. The equation (.8) can be written for w as w + 1 β w + δw = φ(ξ) := 1 δ(w + q ). (.11) Note that due to periodicity all functions in (.1) and (.11) are bounded on R. Therefore we will first consider solutions of (.1) and (.11) which are bounded on R but not necessarily periodic. The general solution for this equation is given by w(ξ) =A(a)e b β (ξ a) + B(a)e b β (ξ a) cos(ξ a) + C(a)e b β (ξ a) sin(ξ a) (.1) + A a [ ξ where A = e b β (ξ y) e b β (ξ y) cos(ξ y)+ 3b β e b β (ξ y) sin(ξ y) β 3b +1 and ξ a. Multiplying (.1) by e b β (ξ a) and letting ξ,weobtain ] φ(y)dy, A(a) = A ψ(a) := A a e b β (a y) φ(y)dy, (.13) with φ defined in (.11). We can now prove that w satisfies also the following equation: w b β w + b +1 β w = ψ, (.14) 5

6 where ψ was defined in (.13). Indeed, w(a)=a(a)+b(a), w (a)= b β A(a)+ b B(a)+C(a), and β ( ) w (a)= b b β A(a)+ 4β 1 B(a)+ b β C(a), whence solving for B(a) andc(a) weobtain ( A(a) =A w (a) b ) β w (a)+ b +1 w(a). β This and the definition of ψ gives (.14). The general solution for (.14) is w(ξ)=a 1 (a)e b β (ξ a) cos(ξ a)+b 1 (a)e b β (ξ a) sin(ξ a) ξ a e b β (ξ y) sin(ξ y)ψ(y)dy. (.15) Letting a, we finally obtain the following: Lemma.1 Any solution w of the equation (.11) bounded over all R is given by the following integral representation: w(ξ) = e b ξ β (ξ y) sin(ξ y)ψ(y)dy, (.16) where w and ψ are defined in (.9) and (.13) respectively. In the next section we will show how this representation (.16) leads to some global estimates for the bounded solution of the equations (.1) and (.11). 3 Global Estimates We start by proving that the first derivative of the bounded solution w of (.11) is also bounded. 6

7 Lemma 3.1 For all ξ R we have b β w(ξ)+ 1 ( w ξ + π ) w (ξ) b γ β w(ξ) ( γw ξ π ), (3.1) where γ(β) =e bπ β. PROOF. Recall that ψ(y), y R. Therefore, from (.16) we obtain and w (ξ)= ξ [ ] β b (ξ y) sin(ξ y)+cos(ξ y) ψ(y)dy β e b = b β w(ξ)+ + e bπ 4β w (ξ)= ξ+ π ξ+ π b β w(ξ)+ 1 γ w ξ e b ξ e b β (ξ y) cos(ξ y)ψ(y)dy e b β (ξ+π/ y) cos ((ξ + π/) y π/) ψ(y)dy ( ξ + π ), [ ] β b (ξ y) sin(ξ y)+cos(ξ y) ψ(y)dy β = b β w(ξ) + e bπ 4β ξ π ξ ξ π b β w(ξ) γw e b β (ξ y) cos(ξ y)ψ(y)dy e b β (ξ π/ y) cos ((ξ π/) y + π/) ψ(y)dy ( ξ π ). This lemma immediately implies the following global estimates for v. Theorem 3. Any bounded solution of (.1) satisfies v(ξ), ξ R. (3.) γ 1 7

8 PROOF. From Lemma 3.1 it follows that ( γw ξ π ) ( + w ξ + π ), (3.3) or, in terms of v, ( γv ξ π ) ( + v ξ + π ) 1+γ, ξ R. (3.4) Consider v 1 (ξ) = v( ξ), q 1 (ξ) =q( ξ). Since (.1) is valid if we replace {v, q} with {v 1,q 1 },wealsohave ( γv ξ + π ) ( + v ξ π ) (1 + γ), ξ R. (3.5) Relations (3.4) and (3.5) imply (3.). Note that γ+1 is bounded by 7, which implies the following: γ 1 5 Corollary 3.3 Any bounded solution u of (.7) satisfies u(x) 7 c. (3.6) 5 Combining Lemma 3.1 and Theorem 3. we can now obtain L bounds for the first and second derivatives of v. Lemma 3.4 For v as in Theorem 3. we have γ ( b γ 1 β + 1 ) v g(β) := ( ) b γ γ 1 β + γ γ (3.7) and v b β g(β)+b +1 β γ γ 1. (3.8) PROOF. Relation (3.7) follows from Theorem 3. and Lemma 3.1. For (3.8) we apply (.14), Theorem 3. and (3.7) to obtain 8

9 v b β v b +1 (v 1) β b +1 γ β g(β)+b β γ 1. Using again the fact that {v 1,q 1 } defined in the proof of Theorem 3. is a solution of (.1), we get v b β g(β) b +1 β γ γ 1. 4 Universal Bounds After the preparation done in the preceding sections we can now proceed to our main result. Lemma 4.1 Let [ξ 1,ξ ] be an interval such that v (ξ) > for ξ (ξ 1,ξ ), v (ξ 1 )=v (ξ )=.Leth be an absolutely continuous non-negative function on the interval [v 1,v ],wherev 1 := v(ξ 1 ), v := v(ξ ).Then v v 1 v h(v)dv ( 1 q g(β) δβ ) v v 1 ξ h(v)dv + (v ) v h (v)dξ, (4.1) δ ξ 1 where q =max ξ q(ξ). PROOF. Multiplying (.1) by h(v)v and integrating over the interval [ξ 1,ξ ], we obtain ξ ξ v h(v)v dξ + (v ) h(v)dξ β ξ 1 ξ 1 = δ ξ ξ ξ h(v)v dξ v h(v)v dξ v h(v)q dξ ξ 1 ξ 1 ξ 1 δ v v v h(v)dv v h(v)dv q h(v)dv. v 1 v 1 Since v (ξ) g(β) for any ξ, wehave v 1 9

10 ( 1 q g(β) δβ ) v v 1 h(v)dv v v 1 v h(v)dv ξ v h(v)v dξ δ ξ 1 = ξ ξ (v ) h(v)dξ + (v ) v h (v)dξ δ ξ 1 ξ 1 ξ (v ) v h (v)dξ. δ ξ 1 Lemma 4. Let v be any bounded solution of (.1), and let max q (ξ) <G(β) :=1 g(β) ξ β δ 1 6 ( ). (4.) γ 1 Let also [ξ 1,ξ ], ξ 1 <ξ, be an interval such that v (ξ) > for ξ (ξ 1,ξ ), v (ξ 1 )=v (ξ )=.Then v 1 v > and (4.3) max{ v 1, v } > 1 6 γ 1, (4.4) where v 1 = v(ξ 1 ), v = v(ξ ). PROOF. First, consider the case when v 1 <v.set h(v) :=v v for v [v 1,v ]. (4.5) Note that ξ ξ 1 (v ) v h (v)dξ = 1 3 ξ ξ 1 ( (v ) 3) h (v)dξ ξ = 1 (v ) 3 h (v)dξ =. 3 ξ 1 1

11 Denote a = a(β,q ):=1 q g(β) β δ. (4.6) UsingLemma4.1weobtain v v a (v v)dv v (v v)dv, v 1 v 1 ( a v (v v 1 ) 1 ) (v v1) 1 3 v (v 3 v1) (v4 v1). 4 So, we have a v +v 1 v +3v1. 6 Thus, by the assumption (4.), ( ) v +v 1v +3v1 >. (4.7) γ 1 Therefore, v 1 by virtue of (3.). Moreover, 6max{v 1,v } v +v 1 v +3v 1 > ( ), γ 1 which implies max{ v 1, v } > 1 6 γ 1. (4.8) Inthecasewhenv 1 <v we define h on the interval [v 1,v ]as h(v) :=v v 1. (4.9) As in the previous case we get that v and ( ) v1 +v 1v +3v >. (4.1) γ 1 11

12 Therefore, max{ v 1, v } > 1 6 γ 1. (4.11) In the remaining case when v 1 v < we have to get a contradiction. Define the function h on the interval [v 1,v ] as follows. h(v) := v v 1 v 1 when v 1 v<, v v v when v v. (4.1) Let ξ (ξ 1,ξ ) be the point where v vanishes. Then notice that ξ ξ (v ) v h (v)dξ = 1 (v ) v dξ 1 (v ) v dξ v 1 v ξ 1 ξ 1 ξ By the Lemma 4.1, ξ = 1 v (v (ξ )) v 1 3 (v (ξ )) 3 >. Thus, v v 1 a dv + a v 1 v 1 a v v v dv < v (v v 1 ) v v (v v) dv + dv, v v 1 v v 1 ) + v < 1 ( v4 1 v 1 v v v v 3 ) ( v 3 a ( v 1 + v ) < 1 1 ( v v). 3 ( v 1 a< 1 v v 3. 6 v 1 + v v4 4 + v v 3 3 ), So, by virtue of (4.), v v 3 v 1 + v > ( ). (4.13) γ 1 Finally, v 1 v 1 ( ) + v v γ 1 ( ) >, γ 1 1

13 which contradicts (3.). Theorem 4.3 Let v be any periodic solution of (.1) with zero mean. Then the function q from equation (.1) must satisfy max q (ξ) G(β), (4.14) ξ for G defined in Lemma 4.. PROOF. Suppose, to the contrary, that max q (ξ) <G(β). ξ Since v has zero mean, but is not identical zero (since q can not reach one), there exists ξ with the property that v(ξ )=andthatforanyɛ>there exists ξ ɛ >ξ such that ξ ɛ ξ <ɛand v (ξ ɛ ) >. Given ɛ>, consider the maximal interval (ξɛ L,ξR ɛ ) such that ξ ɛ (ξɛ L,ξR ɛ )andv (ξ) >, ξ (ξɛ L,ξR ɛ ). If ξ [ξɛ L,ξR ɛ ]thenwegetv(ξl ɛ )v(ξr ɛ ) which contradicts the previous lemma. Thus, ξ <ξɛ L.Choosenowξ [ξ,ξɛ L ) such that v (ξ ) >. Consider again the maximal interval (ξ L,ξR ) such that ξ (ξ L,ξR )andv (ξ) >, ξ (ξ L,ξR ). Notice that ξ R ξ <ɛ. As above, ξ <ξ L also implies that by virtue of the previous lemma. Moreover, that lemma v(ξ R ) > 1 6 γ 1. Since this is valid for any ɛ, wehavedestroyedthecontinuityofv at ξ. 5 Explicit Estimates Theorem 4.3 can be stated in a more explicit way. For this consider the following equation: q = G(β). (5.1) 13

14 Note that the right hand side is bounded G(β) <q := lim τ G(τ), β >. For q <q we can solve (5.1) numerically. Let us define β (q )asthelargest positive solution of (5.1). The graph of β (q ) is shown in Figure 1. Then Theorem 4.3 has the following corollary: Theorem 5.1 If there exists a periodic solution of (.1) with zero mean and q := max q(ξ) <q.68, then β β (q ). (5.) q * β.4.3 H 6. 4 q q * c Fig. 1. Graph of β (q ) Fig.. Graph of H(c) Let us reformulate this theorem in terms of equation (.7). Recall that β was defined as a function of c in the following way: β(c) := 3 4 b +1, where b is the positive solution of b 3 + b = c. Then equality (5.1) can be written as q = H(c) :=G(β(c)). (5.3) From Theorem 4.3 we see that max q(x) H(c). x We solve (5.3) numerically for c and define C(q ) to be the largest positive solution. Let also K(q):= γ(β(c(q ))) + 1 γ(β(c(q))) 1 C(q ). (5.4) 14

15 The graphs of C(q )andk(q ) are shown in Figures 3 and 4 respectively. Then using Theorem 3. and the definition (.9) for q we get the following corollary: Corollary 5. If there exists a periodic solution of (.7) with zero mean, then max x p(x) H(c) and u(x) c γ 1 c<7 c, x. (5.5) 5 In particular, if maxx p(x) c q <q.68, then c C(q ) and u(x) K(q ), x R. (5.6) The graphs of H(c), C(q ),andk(q ) are shown in Figures, 3, and C 1 K q q * Fig. 3. Graph of C(q ) q q * Fig. 4. Graph of K(q ) Consider (.7) with p =: u + u + 1 u = 1 c. (5.7) As a particular case of Corollary 5., we obtain an explicit estimate for the Michelson constant K M.Forthis,defineC := C(), K := K(). Then we have Theorem 5.3 Let u be any periodic solution of (5.7) with zero mean. Then c C 64.7 (5.8) 15

16 and u(x) K M K 9., for all x R. (5.9) Choosing c = F max, the theorem can be reformulated in terms of F.Namely, let u be a periodic solution of (1.9) and let F max and F min be defined as in (.4). Then Theorem 4.3 has also the following consequence: Corollary 5.4 If there exists a periodic solution u of (1.9) with zero mean, then ) F max F min H ( F max and u(x) F max < 7 F max γ 1 5 c, x.(5.1) In particular, if Fmax F min F max q <q.68, then F max C(q ) and u(x) K(q ), x R. 6 Universal Bounds on Averages of Solutions In this section we apply the results obtained thus far to time averages of periodic solutions of the non-stationary Kuramoto-Sivashinsky equation (1.4). In order to define the average, we have to use a functional Lim which is an extension of the ordinary limit to the Banach space B(, ) of all bounded functions on (, ). Thanks to the Hahn-Banach theorem, there exists a functional Lim satisfying the following conditions: (1) Lim t f(t) f. () Lim t f(t) = lim t f(t) if this limit exists in the classical case. Let u(x, t) be a solution of (1.4) satisfying the conditions (1.5), (1.6). Denote by ū(x) the time average t 1 ū(x) :=Lim t u(x, τ)dτ (6.1) t As in [1] one can prove that there exists an invariant probability measure µ on A L such that ū(x) = u(x)µ(du) (6.) 16

17 Henceforth we let an upper bar denote the average with respect to such an invariant probability measure µ. It is then easy to show using equation (1.4) that ū satisfies ū +ū + ( 1 u ) =, (6.3) where u (x) = u (x)µ(du). Set ũ(x) = u(x) ū(x) andletp(x) be the positive square root of p (x) =ũ (x) = ũ (x)µ(du). Since u =ū + p,wehave ū +ū +ūū + 1 (p ) =. (6.4) Integrating this equation, we get ū +ū + 1 ū + 1 p = c 1. Since u is periodic, ū is periodic also. Thus, after integrating one more time over the period, we get c 1 L. Denote c = c 1.So,wehave ū +ū + 1 ū + 1 p = 1 c. (6.5) Thus, ū(x) satisfies equation (.7) with c = 1 L L u(x) dx and p (x) = u(x) ū(x). (6.6) 17

18 So, Corollary 5. implies Corollary 6.1 Let u(x, t) be any periodic solution of (1.4) with zero mean. Then (1) ū(x) 1 L u(x) γ 1 L dx () Moreover, if for some q <q,then u(x) ū(x) q 1 L L 1, x R. u(x) dx, x R, (6.7) L 1 u(x) L dx C(q) and ū(x) K(q), x R, where C( ) and K( ) are the functions in the Corollary 5.. For example, in the particular case of (6.7) when u(x) ū(x) <.5 1 L L u(x) dx, x, we have 1 L u(x) L dx 3545 and ū(x) 678.7, for all x R. Acknowledgements We would like to thank Prof. Michael S. Jolly for helpful discussions and constructive comments.this work was supported in part by the National Science Foundation Grant Number DMS References [1] H. Bercovici, P. Constantin, C. Foias, O. P. Manley, Exponential decay of the power spectrum of turbulence, Journal of statistical Physics 8 (1995)

19 [] P. Collet, J.-P. Eckmann, H. Epstein, J. Stubbe, A global attracting set for the Kuramoto-Sivashinsky equation, Communication in Mathematical Physics 15 (1993) [3] P. Collet, J.-P. Eckmann, H. Epstein, J. Stubbe, Analyticity for the Kuramotu- Sivashinsky equation, Phys. D 67 (1993) [4] S. P. Dawson, A. M. Mancho, Collections of heteroclinic cycles in the Kuramoto- Sivashinsky equation, Phys. D 1 (3-4) (1997) [5] C. Foias, B. Nicolaenko, G. R. Sell, R. Temam, Inertial manifolds for the Kuramoto-Sivashinsky equation and an estimate of their lowest dimension, J. Math. Pures Appl. (9) 67 (3) (1988) [6] J. Goodman, Stability of Kuramoto-Sivashinsky and related systems, Comm. Pure Appl. Math. 47 (1994) [7] Z. Grujic, I. Kukavica, Space analyticity for the Navier-Stokes and related equations with initial data in L p, Journal of Functional Analysis 15 () (1998) [8] J. M. Hyman, B. Nicolaenko, The Kuramoto-Sivashinsky equation: a bridge between PDEs and dynamical systems, Phys. D 18 (1-3) (1986) , solitons and coherent structures (Santa Barbara, Calif., 1985). [9] J. S. Il yashenko, Global analysis of the phase portrate for the Kuramoto- Sivashinsky equation, J. Dynamics Diff. Eqn 4 (199) [1] M. S. Jolly, I. G. Kevrekidis, E. S. Titi, Approximate inertial manifolds for the Kuramoto-Sivashinsky equation: analysis and computations, Phys. D 44 (1-) (199) [11] Y. Kuramoto, T. Tsuzuki, Persistent propagation of concentration waves in dissipative media far from thermal equilibrium, Prog. Theor. Phys. 55 (1976) [1] D. Michelson, Steady solutions of the Kuramoto-Sivashinsky equation, Phys. D 19 (1986) [13] B. Nicolaenko, B. Scheurer, R. Temam, Some global dynamical properties of the Kuramoto-Sivashinsky equation: Nonlinear stability and attractors, Phys. D 16 (1985) [14] Y. Pomeau, P. Manneville, Stability and fluctuations of spatially periodic flow, Physique Lett. 4 (1979) [15] G. Sivashinsky, Nonlinear analysis of hydrodynamic instability in laminar flame, I. derivation of basic equations, Acta Astronautica 4 (1977) [16] G. Sivashinsky, Weak turbulence in periodic flows, Phys. D 17 (1985) [17] R. Temam, Infinite-Dimensional Dynamical Systems in Mechanics and Physics, Vol. 68 of Applied Mathematical Sciences, Springer-Verlag,

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