Mathematical Models of the Evolution of Surface Waves on...

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Mathematical Models of the Evolution of Surface Waves on Deep Water Crystal Lee Derivation of 1D NLS Numerical Solutions of 2D NLS Solitary Waves Perturbed Solitary Wave Unperturbed vs Perturbed Solitary Wave Mathematical Models of the Evolution of Surface Waves on Deep Water Crystal Lee University of Washington May 15, 2008

Transcript of Mathematical Models of the Evolution of Surface Waves on...

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Mathematical Models of the Evolution ofSurface Waves on Deep Water

Crystal Lee

University of Washington

May 15, 2008

Page 2: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

1 Derivation of 1D NLS

2 Numerical Solutions of 2D NLS

3 Solitary Waves

4 Perturbed Solitary Wave

5 Unperturbed vs Perturbed Solitary Wave

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Derivation of 1D NLSGoverning Equations

z

x

Φzz+∆2Φxx = 0

z = 0

z = 1+¶Ζ

φzz + δ2φxx = 0 on 0 < z < 1 + εζ

φz = δ2(ζt + εφxζx) on z = 1 + εζ

φt + ζ+ε

2

( 1

δ2φ2

z + φ2x

)=

T ζxx

(1 + ζ2x )3/2

on z = 1 + εζ

φz = 0 on z = 0

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Derivation of 1D NLS

Introduce the transformation

ξ = x − cp(k)t η = ε(x − cg (k)t) τ = ε2t

k =2π

λ

Look for an asymptotic solution of the form

φ ∼∞∑

n=0

εnφn(ξ, η, τ, z) ζ ∼∞∑

n=0

εnζn(ξ, η, τ)

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Derivation of 1D NLS

Solution takes the form

φ0 = f0(η, τ) + F0(z , η, τ)e ikξ + F ∗0 (z , η, τ)e−ikξ

ζ0 = A0(η, τ)e ikξ + A∗0(η, τ)e−ikξ

and

φn =n+1∑

m=0

Fnm(z , η, τ)e ikmξ + F ∗nm(z , η, τ)e−ikmξ

ζn =n+1∑

m=0

Anm(η, τ)e ikmξ + A∗nm(η, τ)e−ikmξ.

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Derivation of 1D NLS

Finally,−2ikcpAτ + αAηη + β|A|2A = 0,

whereα = c2

g − (1− δktanh δk)sech2δk

and

β =k2

c2p

(1

2(1 + 9coth2δk − 13sech2δk − 2tanh4δk)

− (2cp + cg sech2δk)2(1− c2g )−1

)

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Numerical Solutions of 2D NLS

Determine the numerical solution to

iuτ + αuξξ + βuηη + γ|u|2u = 0

with ICu(ξ, η, 0) = f (ξ, η)

and periodic BCs in ξ and η on [0, L].

Page 8: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Numerical Solutions of 2D NLSPDE

iuτ + αuξξ + βuηη + γ|u|2u = 0

u = u(ξ, η, τ) = uR(ξ, η, τ) + iuI (ξ, η, τ)

Re: − uIτ + αuRξξ+ βuRηη + γu3

R + γu2I uR = 0

Im: uRτ + αuIξξ+ βuIηη + γuIu

2R + γu3

I = 0

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Numerical Solutions of 2D NLSIC

u(ξ, η, 0) = f (ξ, η)

u(ξ, η, 0) = uR(ξ, η, 0) + iuI (ξ, η, 0)

Re: uR(ξ, η, 0) = Re(f (ξ, η))

Im: uI (ξ, η, 0) = Im(f (ξ, η))

Page 10: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Numerical Solutions of 2D NLSBCs

u(0, η, τ) = u(L, η, τ)

u(ξ, 0, τ) = u(ξ, L, τ)

Re: uR(0, η, τ) = uR(L, η, τ)

uR(ξ, 0, τ) = uR(ξ, L, τ)

Im: uI (0, η, τ) = uI (L, η, τ)

uI (ξ, 0, τ) = uI (ξ, L, τ)

Page 11: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Numerical Solutions of 2D NLSCOV

Letτ = ε2

√gkt

ξ = εk(x − g + 3k2T

2√

gk + k3Tt)

η =εky

b.

Then, the surface displacement is given by

ζ(x , y , t) =−2ε

√gk

k√

k(g + k2T )

(uR(ξ, η, τ)sin(kx −

√k(g + k2T )t)

+ uI (ξ, η, τ)cos(kx −√

k(g + k2T )t))

Page 12: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary Waves

A soliton solution of the 1D NLS equation is given by

u(ξ, τ) = ±√

γsech(ξ)e iατ .

-10 -5 5 10

0.2

0.4

0.6

0.8

1sechHΞL

-10 -5 5 10Ξ

-1

-0.5

0.5

1

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MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary WavesSolitary Wave IC

Page 14: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary WavesSolitary Wave IC

0 50 100 150 200 250 3000

25

50

75

100

125

150

175

x cm

y cm t=5sec

Page 15: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary WavesSolitary Wave IC

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=22.86 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=22.86 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=22.86 cm

Page 16: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary WavesSolitary Wave IC

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=32.107 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=32.107 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=32.107 cm

Page 17: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary WavesSolitary Wave IC

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=34.29 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=34.29 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=34.29 cm

Page 18: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Solitary WavesSolitary Wave IC

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=36.473 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=36.473 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=36.473 cm

Page 19: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

-10 -5 5 10Ξ

-3-2-1

123

Re@UHΞLD,Im@UHΞLD-10 -5 5 10

Ξ

-4

-2

2

4

Re@VHΞLD,Im@VHΞLD

Page 20: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

Consider the following IC.

pertsoln(ξ, η, 0, eps) =

r2α

γsech ξ

+ eps((<[U(ξ)] + i=[U(ξ)])e iρ(η−π2

) + (<[U(ξ)]− i=[U(ξ)])e−iρ(η−π2

))

+ ieps((<[V (ξ)] + i=[V (ξ)])e iρ(η−π2

) + (<[V (ξ)]− i=[V (ξ)])e−iρ(η−π2

))

Page 21: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

Re@pertsolnD

-10-5

05

10

x

-10

-5

0

5

10

y

-5

0

5

-10-5

05

10

x

Im@pertsolnD

-10-5

05

10

x

-10

-5

0

5

10

y

-50

5

-10-5

05

10

x

Page 22: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

Page 23: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

0 50 100 150 200 250 3000

25

50

75

100

125

150

175

x cm

y cm t=4.6sec

Page 24: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=22.86 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=22.86 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=22.86 cm

Page 25: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=32.107 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=32.107 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=32.107 cm

Page 26: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=34.29 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=34.29 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=34.29 cm

Page 27: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Perturbed Solitary Wave

-3 -2 -1 1 2 3t sec

-0.2

-0.1

0.1

0.2

0.3

x=0 cm y=36.473 cmΖHx,y,tL

2 4 6 8 10t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=150 cm y=36.473 cm

11 12 13 14 15 16 17t sec

-0.2

-0.1

0.1

0.2

ΖHx,y,tL x=300 cm y=36.473 cm

Page 28: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Unperturbed vs Perturbed Solitary Wave

At x = 0 cm, y = 22.86 cm,

-3 -2 -1 1 2 3t sec

-0.02

-0.01

0.01

0.02

0.03

x=0 cm y=22.86 cmΖ-Ζ0

Page 29: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Unperturbed vs Perturbed Solitary Wave

At x = 300 cm, y = 22.86 cm,

11 12 13 14 15 16 17t sec

-0.02

-0.01

0.01

0.02

Ζ-Ζ0 x=300 cm y=22.86 cm

Page 30: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Unperturbed vs Perturbed Solitary Wave

At x = 0 cm, y = 34.29 cm,

-3 -2 -1 1 2 3t sec

-0.00002

0.00002

0.00004

x=0 cm y=34.29 cmΖ-Ζ0Ζ-Ζ0

Page 31: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Unperturbed vs Perturbed Solitary Wave

At x = 300 cm, y = 34.29 cm,

11 12 13 14 15 16 17t sec

-0.02

-0.01

0.01

0.02

Ζ-Ζ0 x=300 cm y=34.29 cm

Page 32: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

Results

The soliton solution is not stable with respect to theperturbation.

Page 33: Mathematical Models of the Evolution of Surface Waves on ...depts.washington.edu/amath/wordpress/wp-content/uploads/2014/0… · Mathematical Models of the Evolution of Surface Waves

MathematicalModels of theEvolution of

Surface Waveson DeepWater

Crystal Lee

Derivation of1D NLS

NumericalSolutions of2D NLS

Solitary Waves

PerturbedSolitary Wave

Unperturbedvs PerturbedSolitary Wave

References

Ablowitz, Mark and Segur, Harvey. Solitons and theInverse Scattering Transform. Philadelphia: SIAMPublishing, 1981.

Byrd, P.F. and Friedman, M.D. Handbook of EllipticIntegrals for Engineers and Scientists, Second Edition.New York: Springer-Verlag, 1971

Dr. John Carter, Department of Mathematics, SeattleUniversity.

Johnson, R.S. A Modern Introduction to theMathematical Theory of Water Waves. Cambridge:Cambridge University Press, 1997.