Variable Depth Shallow Water Wave Equation

Introduction

We consider here the problem of waves reflected by a region of variable depth in an otherwise uniform depth region assuming the equations of Shallow Depth.

Equations

We begin with the shallow depth equation

[math]\displaystyle{ \rho(x)\partial_t^2 \zeta = \partial_x \left(h(x) \partial_x \zeta \right). }[/math]

subject to the initial conditions

[math]\displaystyle{ \zeta_{t=0} = \zeta_0(x)\,\,\,{\rm and}\,\,\, \partial_t\zeta_{t=0} = \partial_t\zeta_0(x) }[/math]

where [math]\displaystyle{ \zeta }[/math] is the displacement, [math]\displaystyle{ \rho }[/math] is the string density and [math]\displaystyle{ h(x) }[/math] is the variable depth (note that we are unifying the variable density string and the wave equation in variable depth because the mathematical treatment is identical).

Waves in a finite basin

We consider the problem of waves in a finite basin [math]\displaystyle{ 0\lt x\lt 1 }[/math]. At the edge of the basin the boundary conditions are

[math]\displaystyle{ \left.\partial_x \zeta\right|_{x=0} = \left.\partial_x \zeta\right|_{x=1} =0 }[/math]

.

We solve the equations by expanding in the modes for the basin which satisfy

[math]\displaystyle{ \partial_x \left(h(x) \partial_x \zeta_n \right) = -\lambda_n \zeta_n , }[/math]

normalised so that

[math]\displaystyle{ \int_0^1 \zeta_n \zeta_m = \delta_{mn}. }[/math]

The solution is then given by

[math]\displaystyle{ \zeta(x,t) = \sum_{n=0}^{\infty} \left(\int_0^1 \zeta_n(x^\prime) \zeta_0 (x^\prime) dx^\prime \right) \zeta_n(x) \cos(\sqrt{\lambda_n} t ) }[/math] [math]\displaystyle{ + \sum_{n=1} ^{\infty} \left(\int_0^1 \zeta_n(x^\prime) \partial_t\zeta_0 (x^\prime) dx^\prime \right) \zeta_n(x) \frac{\sin(\sqrt{\lambda_n} t )}{\sqrt{\lambda_n}} }[/math]

where we have assumed that [math]\displaystyle{ \lambda_0 = 0 }[/math].

Calculation of [math]\displaystyle{ \zeta_n }[/math]

We can calculate the eigenfunctions [math]\displaystyle{ \zeta_n }[/math] by an expansion in the modes for the case of uniform depth. We use the Rayleigh-Ritz method. The eigenfunctions are local minimums of

[math]\displaystyle{ J[\zeta] = \int_0^1 \frac{1}{2}\left\{ \left(h(x) \partial_x \zeta\right)^2 - \lambda \zeta^2 \right\} }[/math]

subject to the boundary conditions that the normal derivative vanishes (where [math]\displaystyle{ \lambda }[/math] is the eigenvalue).

We expand the displacement in the eigenfunctions for constant depth [math]\displaystyle{ h=1 }[/math]

[math]\displaystyle{ \zeta = \sum_{n=1}^{N} a_n \psi_n(x) }[/math]

where

[math]\displaystyle{ \psi_n = \sqrt{2} \cos( (n-1) \pi x),\,\,n\ne 1 }[/math]

[math]\displaystyle{ \psi_0 = 1,\, }[/math]

and substitute this expansion into the variational equation we obtain

[math]\displaystyle{ \mathbf{M} \vec{a} = \lambda \vec{a} }[/math]

where the elements of the matrix M are

[math]\displaystyle{ M_{mn} = \int_0^1 \left\{ \left(\partial_x \psi_m h(x) \partial_x \psi_n\right) \right\} }[/math]

Waves in an infinite basin

We assume that the depth is constant and equal to one outside the region [math]\displaystyle{ 0\lt x\lt 1 }[/math]. We can therefore write the wave as

Solution using Separation of Variables

Taking a separable solution gives the eigenvalue problem

[math]\displaystyle{ \partial_x \left( h(x) \partial_x\zeta \right) = -\kappa^{2}\zeta \quad (1) }[/math]

Given boundary conditions [math]\displaystyle{ \zeta \mid_0 = a }[/math] and [math]\displaystyle{ \zeta \mid_1 = b }[/math] we can take [math]\displaystyle{ \zeta = (b-a)x + a + u }[/math] With [math]\displaystyle{ u }[/math] satisfying [math]\displaystyle{ u |_0 = u |_1 = 0 }[/math]

Substituting this form into (1) gives

[math]\displaystyle{ (b-a)\partial_xh(x)+\partial_x(h(x)\partial_xu) = -\kappa^{2}\left((b-a)x+a+u\right) }[/math]

Or, on rearranging

[math]\displaystyle{ \partial_x(h(x)\partial_xu)+\kappa^{2}u = -(b-a)\partial_xh(x)-\kappa^{2}\left((b-a)x+a\right) \quad (2) }[/math]

Now consider the homogenous Sturm-Liouville problem for u

[math]\displaystyle{ \partial_x(h(x)\partial_xu)+\lambda u = 0\quad u|_0=u|_1=0 \quad (3) }[/math]

By Sturm-Liouville theory this has an infinite set of eigenvalues [math]\displaystyle{ \lambda_k }[/math] with corresponding eigenfunctions [math]\displaystyle{ u_k }[/math]. Also since [math]\displaystyle{ u_k|_0=u_k|_1=0\quad \forall k }[/math] Each [math]\displaystyle{ u_k }[/math] can be expanded as a fourier series in terms of sine functions.

[math]\displaystyle{ u_k = \sum_{n=1}^{\infty} a_{n,k}\sin(n\pi x) }[/math]

Transforming (3) into the equivalent variational problem gives

[math]\displaystyle{ J[u] = \int_{0}^{1}\,hu'^{2}-\lambda u^{2} \, dx \quad (4) }[/math]

Substituting the fourier expansion into (4) implies J must be stationary at [math]\displaystyle{ \frac{\partial J}{\partial a_{n}}=0 \quad \forall n }[/math]

[math]\displaystyle{ \frac{\partial J}{\partial a_{n}}=\int_{0}^{1}\,hn\pi \cos(n\pi x)\sum_{m=1}^{\infty} a_{m}\cos(m\pi x)\,dx-\frac{\lambda} {2}a_{n}=0 }[/math]

By defining a vector [math]\displaystyle{ \textbf{a} = \left(a_{n}\right) }[/math] and a matrix [math]\displaystyle{ M_{(n,m)} = 2\int_{0}^{1}\,hnm\pi^{2} \cos(n\pi x)\cos(m\pi x)\,dx }[/math] we have the linear system [math]\displaystyle{ M\textbf{a} = \lambda\textbf{a} }[/math] which returns the eigenvalues and eigenvectors of equation (3), with eigenvectors [math]\displaystyle{ \textbf{a} }[/math] representing coefficient vectors of the fourier expansions of eigenfunctions.

If we now construct [math]\displaystyle{ u = \sum_{k=1}^{\infty} b_k u_k }[/math] and substitute this into equation (2) we get

[math]\displaystyle{ \sum_{k=1}^{\infty} (\kappa^{2}-\lambda_k) b_k u_k = -(b-a)\partial_xh(x)-\kappa^{2}\left((b-a)x+a\right) \quad (5) }[/math]

And defining the RHS of equation (5) as [math]\displaystyle{ f(x) }[/math], a known function, we can retrieve the coefficients [math]\displaystyle{ b_k }[/math] by integrating against [math]\displaystyle{ u_k }[/math]

[math]\displaystyle{ b_k = \frac{\int_{0}^{1}\,f u_k\,dx}{(\kappa^{2}-\lambda_k) \int_{0}^{1}\, u_{k}^{2}\,dx} }[/math]

Also to find the coefficients [math]\displaystyle{ c_n }[/math] of the fourier expansion of u are just [math]\displaystyle{ \sum_{k=1}^{\infty}a_{n,k}b_{k} }[/math] with [math]\displaystyle{ a_{n.k} }[/math] being the [math]\displaystyle{ n }[/math]th coefficient of the [math]\displaystyle{ k }[/math]th eigenfunction of the Sturm-Liouville problem.

So [math]\displaystyle{ \zeta=(b-a)x+a+\sum_{n=1}^{\infty}c_{n} \sin(n\pi x) }[/math] with [math]\displaystyle{ \zeta |_0=a \quad \zeta |_1=b }[/math] and, given [math]\displaystyle{ a }[/math] and [math]\displaystyle{ b }[/math] explicitly differentiating [math]\displaystyle{ \zeta }[/math] gives [math]\displaystyle{ \partial_x \zeta |_0 }[/math] and [math]\displaystyle{ \partial_x |zeta |_1 }[/math].

The aim here is to construct a matrix [math]\displaystyle{ S }[/math] such that, given [math]\displaystyle{ a }[/math] and [math]\displaystyle{ b }[/math]

[math]\displaystyle{ S \begin{pmatrix} \zeta |_0 \\ \zeta |_1 \end{pmatrix}=\begin{pmatrix} \partial_x \zeta |_0 \\ \partial_x \zeta |_1 \end{pmatrix} }[/math]

Taking [math]\displaystyle{ a=1,\,b=0 }[/math] to give [math]\displaystyle{ \zeta_1 }[/math] shows that the first column of [math]\displaystyle{ S }[/math] must be [math]\displaystyle{ \begin{pmatrix} \partial_x \zeta_1 |_0 \\ \partial_x \zeta_1 |_1 \end{pmatrix} }[/math] and likewise taking [math]\displaystyle{ a=0,\,b=1 }[/math] to give [math]\displaystyle{ \zeta_2 }[/math] shows the second column must be [math]\displaystyle{ \begin{pmatrix} \partial_x \zeta_2 |_0 \\ \partial_x \zeta_2 |_1 \end{pmatrix} }[/math]. So [math]\displaystyle{ S }[/math] is given by

[math]\displaystyle{ \begin{pmatrix} \partial_x \zeta_1 |_0 \, \partial_x \zeta_2 |_0 \\ \partial_x \zeta_1 |_1 \, \partial_x \zeta_2 |_1 \end{pmatrix} }[/math]

Now for the areas of constant depth there is a potential of the form [math]\displaystyle{ e^{ikx} }[/math] which, creates reflected and transmitted potentials from the variable depth area of the form [math]\displaystyle{ Re^{ikx} }[/math] and [math]\displaystyle{ Te^{ikx} }[/math] respectively where the magnitudes of [math]\displaystyle{ R }[/math] and [math]\displaystyle{ T }[/math] are unknown. We can calculate that the boundary conditions for [math]\displaystyle{ \zeta }[/math] must be

[math]\displaystyle{ \zeta |_0 = 1+R, \quad \zeta |_1 = Te^{ik}, \quad \partial_x \zeta |_0 = ik(1-R), \quad \partial_x \zeta |_1 = ikTe^{ik} }[/math]

Knowing [math]\displaystyle{ S }[/math] these boundary conditions can be solved for [math]\displaystyle{ R }[/math] and [math]\displaystyle{ T }[/math], which in turn gives actual numerical boundary conditions to the original problem. Taking a linear combination of the solutions already calculated ([math]\displaystyle{ \zeta_1 }[/math] and [math]\displaystyle{ \zeta_2 }[/math]) will provide the solution for these new boundary conditions. This solution, along with the potentials outside this region gives a potential for the whole real axis.

If a waveform [math]\displaystyle{ f(x) }[/math] is travelling in from [math]\displaystyle{ -\infty }[/math] Taking the fourier transform gives

[math]\displaystyle{ \hat{f}(k)=\int_{-\infty}^{\infty}\,f(x)e^{2\pi i k} \,dx }[/math]

and then inverting [math]\displaystyle{ \hat{f}(k) \zeta(x) }[/math] with respect to [math]\displaystyle{ t }[/math] gives

[math]\displaystyle{ f(x,t) = \int_{-\infty}^{\infty}\,\hat{f}(k) \zeta(x) e^{-2\pi i k t} \,dk }[/math]

which is the time dependent solution for the wave form.