On nonlinear conservation laws with nonlocal diffusion term Franz - - PowerPoint PPT Presentation
On nonlinear conservation laws with nonlocal diffusion term Franz - - PowerPoint PPT Presentation
On nonlinear conservation laws with nonlocal diffusion term Franz Achleitner 1 Sabine Hittmeir 1 Christian Schmeiser 2 1 Vienna University of Technology 2 University of Vienna Padova, June 2012 financial support by the Austrian Science Fund
- utline
1 examples in physics 2 nonlocal operator 3 partial integro-differential equations 4 traveling wave solutions
existence of traveling wave solutions asymptotic stability of traveling wave solutions
5 outlook 6 References
shallow water flow
boundary conditions at free surface incompressible Navier-Stokes equations no-slip boundary conditions at rigid bottom Assumptions (Kluwick, Cox, Exner and Grinschgl (2010))
1 Froude number 1 <
U0 √gH << 2
2 length scales H << L 3 Reynolds number 1 << Re = L√gH
ν H2 L2
⇒ viscous effects only important in boundary layer
incompressible Navier-Stokes equation
ux + vy = 0 , ut + uux + vuy = −px + 1 Re H2 L2 uxx + uyy
- ,
vt + uvx + vvy = − L2 H2 (py + 1) + 1 Re H2 L2 vxx + vyy
- .
x, y ...coordinates, u, v ...velocity components, t ...time, p ...pressure no-slip boundary condition y = s(x, t) : u = 0 , v = st . boundary conditions at free surface y = h(x, t) : ht + uhx − v = 0 , p = −Thxx
- 1 + H2
L2 (hx)2 −3/2 .
triple-deck structure: lower deck
matching conditions lim
Y →∞ U(X, Y ) = Y + A ,
lim
X→−∞ U(X, Y ) = Y .
no-slip b.c. at Y = 0: U = 0 , V = 0 . governing equations for (U, V , P) with X ∈ R, Y ∈ R+ and t ∈ R+ ∂XU + ∂Y V = 0 , U∂XU + V ∂Y U = −∂XP + ∂2
Y U ,
∂tP + ∂XP − P∂XP = K1∂XA + K2∂3
XP .
linear flow response
interaction equation for pressure P ∂tP + ∂XP = K1∂XD1/3P + K2∂3
XP,
X ∈ R, t ∈ R+, with constants K1 and K2 related to K1 streamline curvature and boundary displacement effects K2 detuning and surface tension and a nonlocal operator Dα with 0 < α < 1 defined as (DαP)(X) := 1 Γ(1 − α) X
−∞
P′(ξ) (X − ξ)α dξ .
Fowler equation: model for dune formation
∂tu + 1 2∂xu2 = −∂xD1/3u + ∂2
xu,
x ∈ R, t ∈ R+, where u(x, t) represents dune amplitude. no maximum principle (Alibaud, Azerad and Is` ebe (2010)) bore-like traveling wave solutions
nonlocal operator ∂xDα
For 0 < α < 1, the operator (∂xDαu)(x) = ∂x 1 Γ(1 − α) x
−∞
u′(y) (x − y)α dy is a Fourier multiplier operator F(∂xDαu)(ξ) = 1 √ 2π
- R
e−iξx(∂xDαu)(x) dx = Λ(ξ)Fu(ξ) with u ∈ S(R) and symbol Λ(ξ) = −
- sin
- απ
2
- − i sgn(ξ) cos
- απ
2
- |ξ|α+1 ,
ξ ∈ R .
Fourier multiplier operator (FTf )(ξ) = −ψ(−ξ)(Ff )(ξ)
Id −H −Id H ∂x −∂xH −∂x ∂xDαu ∂2
x
−H∂2
x
∂3
x
1 − α 1 + α a θ 2 1 −1 3 2 1 Riesz-Feller operator T ψ(ξ) = |ξ|a exp
- i sgn(ξ)θπ
2
- real-valued parameters
a index of stability 0 < a ≤ 2 θ skewness parameter |θ| ≤ min(a, 2 − a) Hilbert transform Hf := p.v. 1 π ∞
−∞
f (y) x − y dy
Fourier multiplier ψa,θ(ξ) := |ξ|a exp
- i sgn(ξ)θ π
2
- −1
i sgn(ξ) 1 −i sgn(ξ) iξ |ξ| −iξ −(iξ)a |ξ|2 −(iξ)3 1 − α 1 + α a θ 2 1 −1 3 2 1 real-valued parameters a index of stability 0 < a ≤ 2 θ skewness parameter |θ| ≤ min(a, 2 − a)
fractional diffusion equation
∂tu = ∂xDαu , x ∈ R , t ∈ R+ , for some fixed α with 0 < α < 1. strongly continuous, convolution semigroup Tt : Lp(R) → Lp(R) , u0 → Ttu0 = u(t, x) = K(t, ·) ∗ u0 , with 1 ≤ p < ∞ and kernel K(t, x) = F−1(exp(Λ(.)t))(x). Properties of K(t, x): for all x ∈ R, t > 0 and m ∈ N, non-negative K(t, x) ≥ 0 integrable K(t, .)L1(R) = 1 scaling K(t, x) = t−
1 1+α K(1, xt− 1 1+α )
smooth K(t, x) is C∞ smooth bounded there exists Bm ∈ R+ such that |∂m
x K|(t, x) ≤ t− 1+m
1+α
Bm 1 + t−
2 1+α |x|2
L´ evy strictly stable distributions on R
L C H N 1 − α 1 + α a θ 2 1 −1 3 2 1 random variable X E[exp(iξX)] = exp(−ψ(ξ)) ψ(ξ) = |ξ|a exp
- i sgn(ξ)θ π
2
- distributions
L L´ evy-Smirnov PDF x−3/2
2√π exp
- − 1
4x
- ,
x > 0. C Cauchy(-Lorentz) PDF 1
π 1 1+x2
H Holtsmark N Normal (Gaussian) PDF
1 √ 2πσ2 exp
- − x2
2σ2
approximate identity
Theorem (Stein, Weiss)
Suppose φ ∈ L1(Rn) with
- Rn φ(x)dx = 1 and for ǫ > 0 let
φǫ(x) = ǫ−nφ(x/ǫ). If f ∈ Lp(Rn), 1 ≤ p < ∞, or f ∈ C0 ⊂ L∞(Rn), then f ∗ φǫ − f p → 0 as ǫ → 0.
Theorem (Lieb, Loss)
Let j be in L1(Rn) with
- Rn j = 1. For ǫ > 0, define jǫ(x) := ǫ−nj(x/ǫ), so
that
- Rn jǫ = 1 and jǫ1 = j1. Let f ∈ Lp(Rn) for some 1 ≤ p < ∞ and
define the convolution fǫ := jǫ ∗ f . Then fǫ ∈ Lp(Rn) and fǫp ≤ j1f p . fǫ → f strongly in Lp(Rn) as ǫ → 0 . If j ∈ C ∞
c (Rn), then fǫ ∈ C ∞(Rn) and Dαfǫ = (Dαjǫ) ∗ f .
Theorem (L´ evy process)
For every 0 < α < 1, there exists a L´ evy process {Xt | t ≥ 0} such that the probability distribution µt of Xt has probability density function K(t, x). Moreover, the associated transition semigroup {Pt} is a strongly continuous semigroup on C0(R) with Pt = 1. The infinitesimal generator Lα of {Pt} is given for f ∈ C 2
0 (R) by
Lαf (x) = cos
- (1 − α)π
2 ∞ f (x + y) − f (x) − yf ′(x) y2+α dy and has core C ∞
c (R).
transition function Pt(x, B) = µt(B − x) for t ≥ 0, x ∈ R, B ∈ B(R) transition semigroup Define for f ∈ C0(R) (Ptf )(x) =
- R
Pt(x, dy)f (y) =
- R
f (x + y)K(t, y) dy = E[f (x + Xt)] , then Ptf ∈ C0(R) by the Lebesgue convergence theorem.
scalar conservation law with nonlocal diffusion
∂tu + ∂xf (u) = ∂xDαu, x ∈ R, t ∈ R+, (1) where f (u) is a smooth flux function.
Theorem (Droniou, Gallou¨ et and Vovelle (2003))
The Cauchy problem of (1) with initial datum u0 ∈ L∞(R) has a unique global solution u(t, x), in the sense that u ∈ L∞((0, ∞) × R) satisfies u(t, x) = (K(t, .) ∗ u0)(x) − t
- K(t − τ, .) ∗ ∂xf (u(τ, .))
- (x)dτ
(2) almost everywhere. Moreover,
1 u ∈ C ∞((0, ∞) × R) and u ∈ C ∞
b ((t0, ∞) × R) for all t0 > 0.
2 u satisfies equation (1) in the classical sense. 3 for all t > 0, u(t, .)∞ ≤ u0∞ and, in fact, u takes its values
between the essential lower and upper bounds of u0.
4 u(t) t→0
− − → u0 in L∞(R) weak-∗ and in Lp
loc(R) for all p ∈ [1, ∞).
sketch of proof
Droniou, Gallou¨ et and Vovelle established the result in case of a nonlocal diffusion operator with symbol −|ξ|1+α for 0 < α < 1. existence Suppose u0 ∈ C ∞
c (R).
Construct approximate solution uδ, δ > 0, by a splitting method: Define uδ(0, .) = u0 Define uδ(t, x) on (t, x) ∈ (2nδ, (2n + 1)δ] × R, n ∈ N0, as the solution of ∂tu = 2∂xDαu with initial condition uδ(2nδ, .). Define uδ(t, x) on (t, x) ∈ ((2n + 1)δ, (2n + 2)δ] × R, n ∈ N0, as the solution of ∂tu + 2∂xf (u) = 0 with initial condition uδ((2n + 1)δ, .). For δ0 > 0 sufficiently small, any compact set Q ⊂ R and T > 0, {uδ | δ ∈ (0, δ0]} is relatively compact in C([0, T]; L1(Q)). limit function u ∈ C([0, T]; L1(R)) satisfies mild formulation (2).
scalar conservation law with vanishing nonlocal diffusion
∂tuǫ + ∂xf (uǫ) = ǫ∂xDαuǫ, x ∈ R, t ∈ R+, (3) where f (u) is a smooth flux function.
Theorem (Droniou (2003))
Suppose 0 < α ≤ 1 and u0 ∈ L∞(R). The solution uǫ of ∂tuǫ + ∂xf (uǫ) = ǫ∂xDαuǫ , uǫ(0, x) = u0(x) , converges as ǫ → 0 in C([0, T]; L1
loc(Rn)) for all T > 0 to the entropy
solution of the Cauchy problem ∂tu + ∂xf (u) = 0 , u(0, x) = u0(x) . Moreover, if u0 ∈ L∞(R) ∩ L1(R) ∩ BV (R), then uǫ − uC([0,T];L1(R)) = O
- ǫ1/(1+α)
.
traveling wave solutions of equation (1)
Consider wave speed s ∈ R and traveling wave variable ξ := x − st.
Definition
A traveling wave solution of (1) is a solution of the form u(t, x) = ¯ u(ξ), for some function ¯ u that connects different endstates limξ→±∞ ¯ u(ξ) = u±. traveling wave equation h(u) := f (u) − su −
- f (u−) − su−
- = Dαu =
1 Γ(1 − α) x
−∞
u′(y) (x − y)α dy (4) properties of specific traveling wave solutions Rankine-Hugoniot condition f (u+) − f (u−) = s(u+ − u−) For convex flux function f (u) and a monotone solution, standard entropy condition u− > u+.
existence of traveling wave solution
Theorem (A., Hittmeir and Schmeiser (2011))
Suppose f ∈ C ∞(R) is a convex function and (u−, u+, s) satisfy the Rankine-Hugoniot condition as well as the entropy condition u− > u+. Then there exists a traveling wave solution of (1), which is decreasing and unique (up to translations) among all functions u ∈ {u− + v | v ∈ H2(−∞, 0) ∩ C 1
b (R)}.
traveling wave equation linearized at u = u− h′(u−)v(ξ) = Dαv(ξ) := 1 Γ(1 − α) ξ
−∞
v′(y) (ξ − y)α dy, ξ ∈ R−, has solutions of the form v(ξ) := b exp(λξ) with λ := h′(u−)1/α and b ∈ R.
local existence + uniqueness
Lemma
For every sufficiently small ǫ > 0, ξǫ := log ǫ
λ
and Iǫ = (−∞, ξǫ], there exists an ǫ-independent δ > 0, such that the equation (4) has solutions uup,ǫ, udown,ǫ ∈ u− + H2(Iǫ), which satisfy uup,ǫ(ξǫ) = u− + ǫ , udown,ǫ(ξǫ) = u− − ǫ (5) and are unique among all functions {u | u − u−H2(Iǫ) ≤ δ}. Moreover, uup,ǫ − u− − eλξH2(Iǫ) ≤ Cǫ2 , udown,ǫ − u− + eλξH2(Iǫ) ≤ Cǫ2 holds with an ǫ-independent constant C and λ := h′(u−)1/α. proof Consider ¯ u = udown,ǫ(ξ) − u− + exp(λξ) which satisfies a BVP
- Dα−h′(u−)
- ¯
u = h(u−−exp(λξ)+¯ u)+h′(u−)
- exp(λξ)−¯
u
- ,
¯ u(ξǫ) = 0. Cast BVP as a fixed point problem + use Banach’s fixed point theorem.
local monotonicity
Lemma
For all ξ ∈ Iǫ, the solution udown,ǫ(ξ) is bounded (udown,ǫ(ξ) < u−) and monotone (u′down,ǫ(ξ) < 0). proof Due to Sobolev imbedding H2(Iǫ) ֒ → C 1
b (Iǫ),
|udown,ǫ − u− − eλξ| ≤ Cǫ2 for all ξ < ξǫ . There exists ξ⋆ < ξǫ, such that udown,ǫ(ξ⋆) = u− − 2Cǫ2 and the solution is bounded from above by u− for all ξ ∈ (ξ⋆, ξǫ). For ǫ2 = 2Cǫ2
1 with ǫ1 = ǫ,
the translated function udown,ǫ(ξ − ξǫ2 + ξ⋆) is the unique solution udown,ǫ2. Iteration of the argument produces a sequence {ǫn}, determined by ǫn+1 = 2Cǫ2
n, such that the unique solution satisfies udown,ǫ(ξ) < u− for
all ξ ∈ (ξǫn, ξǫ) and n ∈ N. Similar argument proves monotonicity.
continuation of solution
Lemma
Let u ∈ C 1
b (−∞, ξ0] be a solution of (4). For sufficiently small δ > 0, the
solution has a unique continuation in the function space C 1
b (−∞, ξ0 + δ).
proof For monotone functions u ∈ C 1
b (R), equation (4) is equivalent to
u(ξ) − u− = 1 Γ(α) ξ
−∞
h(u(y)) (ξ − y)1−α dy . (6) Rewrite equation (6) as a Volterra integral equation on a bounded interval u(ξ) = f (ξ) + 1 Γ(α) ξ
ξ0
h(u(y)) (ξ − y)1−α dy , where f (ξ) = u− + 1 Γ(α) ξ0
−∞
h(u(y)) (ξ − y)1−α dy . Local existence of a smooth solution is a standard result.
global properties
Lemma
Let u ∈ C 1
b (−∞, ξ0] be (a continuation of) the solution udown(ξ) of (4).
Then for all ξ ∈ (−∞, ξ0], u(ξ) is nonincreasing and bounded by u+ < u(ξ) < u−.
Proof of Theorem.
global existence boundedness+local continuation ⇒ The solution u(ξ) exists for all ξ ∈ R and satisfies limξ→+∞ u(ξ) = u+. global uniqueness Let u ∈ {u− + v | v ∈ H2(−∞, 0) ∩ C 1
b (R)} be a
solution of (4). Then the restriction of the solution to an interval (−∞, ξ0] is, up to a shift in ξ, the continuation of uup or udown, or the constant function u ≡ u−.
asymptotic stability of traveling wave φ
Theorem (A., Hittmeir and Schmeiser (2011))
Suppose f is a convex function, φ is a traveling wave solution of (4), and u0 is such that W0(ξ) = ξ
−∞(u0(η) − φ(η)) dη satisfies W0 ∈ H2(R).
If W0H2 is small enough, then the Cauchy problem for ∂tu + ∂ξ(f (u) − su) = ∂ξDαu with initial datum u0 has a unique global solution converging to the traveling wave solution φ in the sense that lim
t→∞
∞
t
u(τ, ·) − φH1 dτ = 0 .
idea of proof
Perturbation U = u − φ satisfies ∂tU + ∂ξ
- f (u) − f (φ) − sU
- = ∂ξDαU .
The energy estimate 1 2 d dt U2
L2+1
2
- R
f ′′(φ)φ′U2 dξ−1 2
- R
f ′′(φ+ϑU)U2∂ξU dξ = −aαU2
˙ H
1+α 2
holds for some 0 < ϑ < 1 and leads to 1 2 d dt U2
L2 − C0U2 L2 − L(UL∞)UL∞U2 H1 ≤ −aαU2 ˙ H
1+α 2
, for a positive nondecreasing function L and positive constants C0 and aα.
The primitive of the perturbation
W (t, ξ) := ξ
−∞
U(t, η) dη satisfies for some 0 < ϑ < 1 ∂tW + (f ′(φ) − s)∂ξW + 1 2f ′′(φ + ϑU)(∂ξW )2 = ∂ξDαW (7) and the energy estimate 1 2 d dt W L2 − L(UL∞)W L∞∂ξW 2
L2 ≤ −aαW 2 ˙ H
1+α 2
.
Lemma
Suppose W0 ∈ H2(R). Then there exists T > 0 such that the Cauchy problem for (7) with initial data W0 has a unique solution W (t) ∈ H2(R) for all t ∈ [0, T).
Lyapunov functional
J(t) = 1 2(W 2
L2 + γ1U2 L2 + γ2∂ξU2 L2)
with positive constants γ1 and γ2. Linear combination of energy estimates yields d dt J + aα
- W 2
˙ H
1+α 2
+ γ1W 2
˙ H
3+α 2
+ γ2W 2
˙ H
5+α 2
- − γ1C0U2
L2 − γ2C1U2 H1 − L(W H2)W H2U2 H(5+α)/4 ≤ 0
Choose γ1, γ2 > 0 such that γ1C0U2
L2 +γ2C1U2 H1 ≤ aα
2
- W 2
˙ H
1+α 2
+ γ1W 2
˙ H
3+α 2
+ γ2W 2
˙ H
5+α 2
- and get the final estimate
d dt J ≤ −γ∗ aα 2 − L γ∗ W H2 W 2
˙ H
1+α 2
+ γ1W 2
˙ H
3+α 2
+ γ2W 2
˙ H
5+α 2
fractional Korteweg-de Vries-Burgers equation
∂tu + u∂xu = ǫ∂xDαu + δ∂3
xu,
x ∈ R, t ∈ R+, (8) for some fixed α with 0 < α < 1 and ǫ, δ ∈ R.
Theorem (Molinet and Ribaud (2001))
global well-posedness of the Cauchy problem for the Kortweg-de Vries-Burgers equation with fractional Laplacian and initial datum in Hs(R) for s > − 3
4.
existence of traveling wave solutions
Theorem (A., Cuesta and Hittmeir (2012))
Suppose (u−, u+, s) satisfy the Rankine-Hugoniot condition as well as the entropy condition u− > u+. Then there exists a traveling wave solution ¯ u ∈ C 2
b (R) of (8), such that limξ→−∞ ¯
u(ξ) = u−.
references
- F. Achleitner, S. Hittmeir and Ch. Schmeiser. On nonlinear conservation
laws with nonlocal diffusion term J. Diff. Equ., 250: 2177–2196, 2011.
- J. Droniou, T. Gallou¨
et and J. Vovelle. Global solution and smoothing effect for a non-local regularization of a hyperbolic equation.
- J. Evol.
Equ., 3: 499–521, 2003.
- J. Droniou Vanishing non-local regularization of a scalar conservation law.
Electronic J. Diff. Equ., 117: 1–20, 2003.
- A. Kluwick, E. A. Cox, A. Exner and C. Grinschgl On the internal
structure of weakly nonlinear bores in laminar high Reynolds number flow. Acta Mech., 210: 135–157, 2010.
Thank you for your attention.
Riemann-Liouville fractional derivative
For a finite interval [a, b] ⊂ R, α ∈ C\N0 with ℜα ≥ 0 and n = ⌊ℜα⌋ + 1 (Dα
a+f )(x) =
1 Γ(n − α) dn dxn x
a
f (y) (x − y)α−n+1 dy , x ∈ [a, b] properties: For α = n ∈ N0 (Dn
a+f )(x) = f (n)(x)
For α, β ∈ C with ℜα ≥ 0 and ℜβ > 0 (Dα
a+(. − a)β−1)(x) =
- Γ(β)
Γ(β−α)(x − a)β−α−1
for α − β / ∈ N0 for α − β ∈ N For α ∈ C\N0 with ℜα ≥ 0 and f ∈ AC n[a, b] (Dα
a+f )(x) = n−1
- k=0
f (k)(a) Γ(1 + k − α)(x−a)k−α+ 1 Γ(n − α) x
a
f (n)(y) dy (x − y)α−n+1
Caputo fractional derivative on finite interval
For a finite interval [a, b] ⊂ R, α ∈ C\N0 with ℜα ≥ 0 and n = ⌊ℜα⌋ + 1 (CDα
a+f )(x) = Dα a+
- f (.) −
n−1
- k=0
f (k)(a) k! (. − a)k
- (x) ,
x ∈ [a, b] properties: alternative representation (CDα
a+f )(x) =
- 1
Γ(n−α)
x
a f (n)(y) (x−y)α−n+1 dy
for α / ∈ N0 f (n)(x) for α ∈ N0 For α, β ∈ C with ℜα ≥ 0 and ℜβ > 0 (CDα
a+(. − a)β−1)(x) =
- Γ(β)
Γ(β−α)(x − a)β−1
for α − β / ∈ N0 for α − β ∈ N For α / ∈ N0 and f ∈ C n[a, b] (CDα
a+f )(a) = 0
Liouville fractional derivative
For α ∈ C\N0 with ℜα ≥ 0 and n = ⌊ℜα⌋ + 1 (Dα
+f )(x) =
1 Γ(n − α) dn dxn x
−∞
f (y) (x − y)α−n+1 dy , x ∈ R properties: For α = n ∈ N0 (Dn
+f )(x) = f (n)(x)
For α, λ ∈ C with ℜα ≥ 0 and ℜλ > 0 (Dα
+ exp(λ.))(x) = λα exp(λx)
For α ∈ C with ℜα > 0 and f ∈ S(R) (FDα
+f )(ξ) = (−iξ)α(Ff )(ξ)
where (−iξ)α = exp(−απi sgn(ξ)/2).
Caputo fractional derivative on R
For α ∈ C\N0 with ℜα > 0 and n = ⌊ℜα⌋ + 1 (CDα
+f )(x) =
1 Γ(n − α) x
−∞
f (n)(y) (x − y)α−n+1 dy , x ∈ R properties: For α = n ∈ N0 (CDα
+f )(x) = f (n)(x)
For α ∈ C with ℜα > 0 and λ > 0 (CDα
+ exp(λ.))(x) = λα exp(λx)
For α ∈ C with ℜα > 0 and f ∈ S(R) (FCDα
+f )(ξ) = (−iξ)α(Ff )(ξ)
where (−iξ)α = exp(−απi sgn(ξ)/2).
Cauchy problem with fractional derivative
For a finite interval [a, b] ⊂ R and α ∈ C\N0 with ℜα ≥ 0 (Dα
a+y)(x) = f (x, y(x))
with n = ⌊ℜα⌋ + 1 initial conditions (Dα−k
a+ y)(a+) = bk ,
bk ∈ C , k = 1, . . . , n
Theorem (Kilbas et al (2006))
For an open set G ⊂ C and a function f : (a, b] × G → C with f (x, y) integrable w.r.t. x for all y ∈ G and f (x, y) Lipschitz continuous in y uniformly w.r.t. x ∈ (a, b]. Then there exists a unique solution y(x) for Cauchy type problem in the space { y ∈ L1(a, b) | Dα
a+y ∈ L1(a, b) }.
Step 1: Cauchy type problem is equivalent to Volterra integral equation y(x) =
n
- j=1
bj Γ(α − j + 1)(x − a)α−j + 1 Γ(α) x
a
f (t, y(t)) (x − t)1−α dt , x ∈ [a, b] Step 2: Banach fixed point theorem
Cauchy problem with Caputo fractional derivative
For a finite interval [a, b] ⊂ R and α ∈ R\N0 with α > 0 (CDα
a+y)(x) = f (x, y(x))
with n = ⌊α⌋ + 1 initial conditions y(k)(a+) = bk , bk ∈ C , k = 0, . . . , n − 1
Theorem (Kilbas et al (2006))
For an open set G ⊂ C and a function f : (a, b] × G → C with f (x, y) continuous w.r.t. x for all y ∈ G and f (x, y) Lipschitz continuous in y uniformly w.r.t. x ∈ (a, b]. Then there exists a unique solution y(x) for Cauchy type problem in the space { y ∈ C ⌊α⌋[a, b] | CDα
a+y ∈ C[a, b] }.
Step 1: Cauchy type problem is equivalent to Volterra integral equation y(x) =
n−1
- j=0
bj j! (x − a)j + 1 Γ(α) x
a
f (t, y(t)) (x − t)1−α dt , x ∈ [a, b] Step 2: Banach fixed point theorem
L´ evy strictly α-stable distributions on R
A random variable is said to be strictly stable (or to have a strictly stable distribution), if it has the property that linear combinations of two independent copies of the variable have the same distribution, up to a scaling. random variable X with L´ evy strictly stable distribution characteristic function E[exp(iξX)] = exp(ψ(ξ)) characteristic exponent ψ(ξ) := −c0|ξ|α exp
- − i sgn(ξ)θα π
2
- parameters
α index of stability 0 < α ≤ 2 θ skewness parameter |θ| ≤ min 2−α
α , 1
- c0 scaling parameter c0 > 0
L´ evy α-stable distributions on R
A random variable is said to be stable (or to have a stable distribution), if it has the property that linear combinations of two independent copies of the variable have the same distribution, up to location and scale parameters. random variable X with L´ evy stable distribution characteristic function E[exp(iξX)] = exp(ψ(ξ)) characteristic exponent ψ(ξ) =
- −c|ξ|α
1 − iβ(sgn ξ) tan απ
2
- + iτξ
for α = 1 , −c|ξ|
- 1 − iβ 2
π(sgn ξ) log |ξ|
- + iτξ
for α = 1 . parameters α index of stability 0 < α ≤ 2 β skewness parameter −1 ≤ β ≤ 1 c scaling parameter 0 < c τ location parameter τ ∈ R
L´ evy operator
Theorem (Sato (1999) Theorem 31.5)
Suppose {Xt} is a L´ evy process on Rd with generating triplet (A, ν, γ), whereat A = (Ajk) ∈ Rd×d and γ = (γj) ∈ Rd. The associated family of
- perators {Pt | t ≥ 0} is a strongly continuous semigroup on C0(Rd) with
norm Pt = 1. Let L be its infinitesimal generator. Then C ∞
c (Rd) is a
core of L, C 2
0 (Rd) ⊂ D(L), and
Lf (x) = 1 2
d
- j,k=1
Ajk ∂2f ∂xj∂xk (x) +
d
- j=1
γj ∂f ∂xj (x)+ +
- Rd
- f (x + y) − f (x) −
d
- j=1
yj ∂f ∂xj (x)1D(y)
- ν( dy)
(9) for f ∈ C 2
0 (Rd) and D = {x ∈ Rd | |x| ≤ 1}.
L´ evy operator: examples for d = 1
1 Any non-trivial α-stable distribution with 0 < α < 2 has absolutely
continuous L´ evy measure ν(dx) =
- c1x−1−α
- n (0, ∞) ,
c2|x|−1−α
- n (−∞, 0) ,
with c1 ≥ 0, c2 ≥ 0, c1 + c2 > 0.
2 If the L´
evy measure ν is non-singular, then
- R
- f (x + y) − f (x) − y ∂f
∂x (x)1D(y)
- ν( dy) = (K ∗ f − µf )(x)