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/centre for analysis, scientific computing and applications Water Waves Ekeoma Rowland Ijioma Supervisor : Dr. J.H.M. ten Thije Boonkkamp 16 December 2009

Water Waves - Faculteit Wiskunde en Informatica · PDF fileOutline Introduction Equations for water waves Linear wave theory Classification of water waves Behavior near the front

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  • /centre for analysis, scientific computing and applications

    Water Waves

    Ekeoma Rowland IjiomaSupervisor : Dr. J.H.M. ten Thije Boonkkamp

    16 December 2009

  • /centre for analysis, scientific computing and applications

    Outline

    IntroductionEquations for water wavesLinear wave theoryClassification of water wavesBehavior near the front of the wavetrainSolution through the dispersion relationConclusion

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    Introduction

    The general idea of dispersive waves originated from theproblems of water waves. The problems are of great interest inthe Maritime and Offshore settings.

    Figure: http://weblogs.sun-sentinel.com

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    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

  • /centre for analysis, scientific computing and applications

    Equations of water waves

    Basic Assumptionswe consider an inviscid incompressible fluidconstant density the spatial domain is given in (x1, x2, y) andthe components of the velocity vector u by (u1,u2, v)F = gj be an external force on the fluid.assume the flow to be irrotational, = u = 0introduce a velocity potential such that u =

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    Linear wave theory

    Plot of velocity potential with the velocity field

    (velocity.avi)

    velocity.aviMedia File (video/avi)

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    Equations of water waves

    then, the inviscid incompressible equations are

    .u = 0

    DuDt

    =ut

    + (u.)u = 1p gj

    so thatut

    +(

    12

    u2)

    + u = 1p gj

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    Equations of water waves

    on integrating foru =

    we havep p0

    = t 12||2 gy

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    Equations of water waves

    Boundary conditions

    Figure: sketch of the flow domain and its boundaries

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    Equations of water waves

    Define an interfacef (x1, x2, y , t) = 0

    or for convenience as

    y = (x1, x2, t) such that f (x1, x2, y , t) (x1, x2, t) y

    Kinematic free surface condition

    DDt

    = t + u1x1 + u2x2 = v

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    Equations of water waves

    and we obtainDynamic free surface condition

    p = p0

    Boundary conditions at the free surface

    t + x1x1 + x2x2 y = 0, on y = ,

    t +12||2 + g = 0, on y =

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    Equations of water waves

    Consider the bottom

    y = h0(x1, x2)

    we obtain Kinematic bottom boundary condition

    x1h0x1 + x2h0x2 + y = 0, on y = h0

    and for a horizontal flat bottom,

    y = 0, on y = h0

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    Linear wave theory

    the linearized free surface conditions are

    t = y , on y = ,t + g = 0, on y = .

    tt + gy = 0, on y = 0

    the surface elevation is

    = 1gt(x1, x2,0, t)

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    Linear wave theory

    The linearized formulation

    x1x1 + x2x2 + yy = 0, on h0 < y < 0,tt + gy = 0, on y = 0,

    x1h0x1 + x2h0x2 + y = 0, on y = h0

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    Linear wave theory

    Analytic solution of the wave problemForm of solution for water waves

    = A exp {i(x t)}

    where A is the Amplitude of the wave

    = Y (y) exp {i(x t)}

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    Linear wave theory

    The Laplace equation

    xx + yy = 0

    Method:Separation of VariablesIn 2-D, we define

    (x , y , t) = X (x)Y (y)T (t)

    divide by X(x)Y(y)T(t) such that

    X

    X= Y

    Y= 2

  • /centre for analysis, scientific computing and applications

    Linear wave theory

    The Laplace equation

    xx + yy = 0

    Method:Separation of VariablesIn 2-D, we define

    (x , y , t) = X (x)Y (y)T (t)

    divide by X(x)Y(y)T(t) such that

    X

    X= Y

    Y= 2

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    Linear wave theory

    The Laplace equation

    xx + yy = 0

    Method:Separation of VariablesIn 2-D, we define

    (x , y , t) = X (x)Y (y)T (t)

    divide by X(x)Y(y)T(t) such that

    X

    X= Y

    Y= 2

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    Linear wave theory

    where 2 is the separation constant.We obtain

    X + 2X = 0

    Y 2Y = 0

    solving these equations, we obtain

    X = B cosx + D sinxY = Eey + Gey

    The solution is given by

    (x , y , t) = (B cosx + D sinx)(Eey + Gey )T (t)

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    Linear wave theory

    We choose for T (t)

    cost or sint

    where =

    2T

    and arrive at 4 possible solutions, periodic in x and t

    1 = A1Y (y) cosx cost2 = A2Y (y) sinx sint3 = A3Y (y) sinx cost4 = A4Y (y) cosx sint

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    Linear wave theory

    The first equation gives the following solution

    1 =gA

    cosh(h0 + y)coshh0

    cosx cost and

    1 = A cosx sint

    The dispersion relation is

    W () = 2 = g tanhh0

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    Classification of water waves

    Water waves are classified into three main categories:Shallow water or long waves, if

    h0

    12

    Intermediate water waves, if

    120