I am trying to construct a set of decoupled system of equations from the following linear shallow water wave model which aims to capture the activity of a tsunami:
\begin{align*} h_t +(Hu)_x &= 0\\ u_t + (gh)_x &=0 \end{align*} Where $H$ is the height of the ocean; assumed to be constant, and $H+h$ is the total height after the tsunami. We also take $g = 10m/s^2$
This is my working so far:
- I wrote the system as a matrix equation:
\begin{align*} \begin{bmatrix} h\\u \end{bmatrix}_t + \begin{bmatrix} 0 & H\\ g& 0 \end{bmatrix}\begin{bmatrix} h\\u \end{bmatrix}_x = 0 \end{align*}
- I diagonalized $$A = \begin{bmatrix} 0 & H\\ g& 0 \end{bmatrix}$$ by $$ P = \begin{bmatrix} \sqrt{gH}/g & -\sqrt{gH}/g\\ 1& 1 \end{bmatrix}, \hspace{0.1cm} P^{-1} =\begin{bmatrix} \frac{g}{2\sqrt{gH}} & \frac{1}{2}\\ -\frac{g}{2\sqrt{gH}}& \frac{1}{2} \end{bmatrix}, \hspace{0.1cm} D =\begin{bmatrix} \sqrt{gH} & 0\\ 0& -\sqrt{gH} \end{bmatrix} $$
Now I am not sure how to proceed, I have tried utilising this diagonalization to get some kind of decoupled system by substituting this diagonalization into the matrix equation, but cant get anywhere. Thanks
You have $A=PDP^{-1}$. Define $s:=P^{-1}\begin{bmatrix}h\\u\end{bmatrix}$. Therefore, we get $$\frac{\partial s}{\partial t}+D\,\frac{\partial s}{\partial x}=0\,.$$ Let $s=:\begin{bmatrix}s_+\\s_-\end{bmatrix}$. Then, we have $$\frac{\partial s_+}{\partial t}+\sqrt{gH}\,\frac{\partial s_+}{\partial x}=0$$ and $$\frac{\partial s_-}{\partial t}-\sqrt{gH}\,\frac{\partial s_-}{\partial x}=0\,.$$ I hope that you know how to solve the two partial differential equations above.