standard_modes_wkb.tex

\documentclass[11pt]{article}

%% WRY has commented out some unused packages %%
%% If needed, activate these by uncommenting
\usepackage{geometry}                % See geometry.pdf to learn the layout options. There are lots.
%\geometry{letterpaper}                   % ... or a4paper or a5paper or ... 
\geometry{a4paper,left=2.5cm,right=2.5cm,top=2.5cm,bottom=2.5cm}
%\geometry{landscape}                % Activate for rotated page geometry
%\usepackage[parfill]{parskip}    % Activate to begin paragraphs with an empty line rather than an indent

%for figures
%\usepackage{graphicx}

\usepackage{color}
\definecolor{mygreen}{RGB}{28,172,0} % color values Red, Green, Blue
\definecolor{mylilas}{RGB}{170,55,241}
%% for graphics this one is also OK:
\usepackage{epsfig}

%% AMS mathsymbols are enabled with
\usepackage{amssymb,amsmath}

%% more options in enumerate
\usepackage{enumerate}
\usepackage{enumitem}

%% insert code
\usepackage{listings}

\usepackage[utf8]{inputenc}

\usepackage{hyperref}

%% colors
\usepackage{graphicx,xcolor,lipsum}


\usepackage{mathtools}

\usepackage{graphicx}
\newcommand*{\matminus}{%
  \leavevmode
  \hphantom{0}%
  \llap{%
    \settowidth{\dimen0 }{$0$}%
    \resizebox{1.1\dimen0 }{\height}{$-$}%
  }%
}

\title{WKB approximate solutions for standard baroclinic modes}
\author{Cesar B Rocha\thanks{Scripps Institution of Oceanography, University of California, San Diego; \texttt{crocha@ucsd.edu}}}
\date{\today}

\begin{document}

\include{mysymbols}

\maketitle

In this notes I derive approximate WKB solutions to the standard baroclinic modes of physical oceanography. The elementary textbook example with constant buoyancy frequency is recovered as a special case. 

\section{Pressure modes}

The standard baroclinic modes for pressure, here denoted $\sp_n(z)$,  is defined by the regular Sturm-Liouville eigenproblem

\beq
\label{eigpb}
\sL \sp_n = -\kappa_n^2 \sp_n\com
\eeq
with homogeneous Neumann boundary conditions
\beq
\label{bc}
@z = -h,\,0:\qquad \sp_n' = 0\com
\eeq
and the self-adjoint Linear operator
\beq
\label{strech}
\sL \defn \frac{\dd}{\dd z}\frac{f_0^2}{N^2}\frac{\dd}{\dd z} \per
\eeq
Hence the eigenmodes, $\sp_n$, are orthogonal. The real egeinvalues, $\kappa_n$, are the deformation wavenumber of the $n$'th mode. It is convenient to normalize the eigenmodes to have the unit $L^2$-norm 
\beq
\label{normalization0}
\frac{1}{H}\int_{-h}^{0}\!\! \sp_n \sp_m \dd z = \delta_{mn}\com
\eeq
where $\delta_{mn}$ is the Dirac delta. Equation \eqref{eigpb} can be rewritten as
\beq
\label{eigpb_wkb}
\bur \sp_n'' + \left[\bur\right]' \sp_n' + \kappa_n^2 \,\sp_n = 0\per
\eeq
Introducing the following definitions
\beq
\label{notation}
\ep \defn \frac{1}{\kappa_n} \qquad \text{and} \qquad S^2(z) \defn \ibur \per 
\eeq
we have the renotated equation
\beq
\label{dirich_eigpb_wkb_ep}
\ep^2\, \sp_n'' -\ep^2 \left[\log S^2(z)\right]' \sp_n' + S^2(z) \sp_n = 0\per
\eeq
In the WKB spirit we assume that $S^2(z)$ is slowly varying i.e., the buoyancy frequency $N^2(z)$ does not vary very fast. (This assumption may be problematic near the base of the mixed-layer.) We also assume that $\ep$ is small; the accuracy of the WKB solution improves with mode number. We now make the exponential approximation (e.g., Bender and Orszag)
\beq
\sp_n^e \defn \ee^{Q(z)/\ep}\per
\eeq
Hence
\beq
{\sp_n^e}' = \frac{Q'(z)}{\ep}\sp_n^e\com
\eeq
and 
\beq
{\sp_n^e}'' = \left[\left(\frac{Q'(z)}{\ep}\right)^2 + \frac{Q''(z)}{\ep} \right]\sp_n^e\com
\eeq
Next we expand $Q(z)$ in powers of $\ep$
\beq
\label{aseries}
Q(z) = Q_0(z)  + \ep\,Q_1(z) + \ep^2\,Q_2(z) + \mathcal{O}(\ep^3)\per
\eeq
Substituting \eqref{aseries} in \eqref{dirich_eigpb_wkb_ep} we obtain, to lowest order, $\mathcal{O}(\ep^0)$,
\beq
\label{lowest_order_eqn}
Q_0'^2 + S^2(z) = 0\per
\eeq
Thus
\beq
\label{Q0}
Q_0 = \pm \ii \int^z \!\!\!S(\xi) \,\dd \xi  = \pm \ii \tfrac{1}{f_0} \int^z \!\!\!N(\xi) \,\dd \xi \per
\eeq
At next order, $\mathcal{O}(\ep)$, we have
\beq
\label{first_order_eqn}
2\,Q_0'Q_1' + Q_0'' - Q_0'  \left[\log S^2(z)\right]' = 0\per
\eeq
Hence
\beq
\label{Q_1}
Q_1  =   \frac{1}{2} \log S^2(z) - \frac{1}{2}\log \pm \ii S(z) + \text{const}\,\, \per
\eeq
Notice that the imaginary part in the $\log$ in \eqref{Q_1} just contributes an irrelevant constant. Thus
\beq
Q_1 = \log \sqrt{S(z)} + \text{const} \,\, \per
\eeq
In the most common WKB approximation (a.k.a ``physical optics'') we truncate \eqref{aseries} at $\mathcal{O}(\ep)$. The solution to \eqref{dirich_eigpb_wkb_ep}, consistent with the bottom boundary condition \eqref{bc}, is
\beq
\sp_n^{po} = A_n\, \sqrt{N(z)}\, \cos \left(\frac{\kappa_n}{f_0} \int_{-h}^{z} \!\!\!N(\xi) \dd \xi\right)\com
\eeq
where $A_n$ is a constant. By imposing the boundary condition at $z=0$ \eqref{bc}, we obtain the eigenvalues $\kappa_n$:
\beq
\label{kappan}
\kappa_n = \frac{n \pi \, f_0}{\overline{N}\,h} \com\qquad n=0,1,2,\ldots \com
\eeq
where the mean buoyancy frequency is
\beq
\label{N_avg}
\overline{N} \defn\frac{1}{h} \int_{-h}^0N(\xi)\dd \xi\per
\eeq
The constant $A_n$ is determined by the normalization condition \eqref{normalization0}. We have
\beq
\label{an_eqn}
A_n^2 \, \int_{-h}^{0}\!\! N(z) \cos \left(\frac{\kappa_n}{f_0}\int_{-h}^{z}\!\!\!N(\xi) \dd \xi\right) \dd z = H\com\qquad n\ge 1\per
\eeq
The integral in \eqref{an_eqn} can be evaluated exactly by making the change of variables 
\beq
\eta \defn \frac{\kappa_n}{f_0}\int_{-h}^{z}\!\!\! N(\xi) \dd \xi  \qquad \Rightarrow \qquad \dd\eta = \frac{\kappa_n}{f_0}N(z) \dd z\com
\eeq
and using the expression for the eigenvalues \eqref{kappan}. We obtain 
\beq
A_n = \Big(2/\overline{N} \Big)^{1/2} \com\qquad n\ge 1\per
\eeq
Thus the WKB approximate solution to the standard pressure modes is
\beq
\sp_n^{po} = \left[\frac{2\,N(z)}{\Nb} \right]^{1/2}\!\!\cos\left( \frac{n \pi}{\Nb\,h} \,\,\,\int_{-h}^{z} \!N(\xi) \dd \xi\right)\com\qquad n\ge1\per
\eeq
The amplitude of the baroclinic modes  at the boundaries is independent of the eigenvalue:
\beq
\sp_n^{po}(z=0) = (-1)^{n} \left[\frac{2 N(0)}{\Nb}\right]^{1/2}\com
\eeq
and
\beq
\sp_n^{po}(z=-h) = \left[\frac{2 N(-h)}{\Nb}\right]^{1/2}\per
\eeq

The barotropic mode is not recovered from the WKB solution because $\kappa_0 = 0$. From \eqref{eigpb} we have that with $\kappa_0 = 0$, the barotropic mode is constant, independent of the stratification. With the normalization \eqref{normalization0} we obtain $\sp_0 = 1$.

\subsection*{Constant buoyancy frequency}
With $N = \text{const.}$  the modes are simple sinusoids. That exact result is recovered as a special case of the WKB solution
\beq
\sp_n^{po} = \sqrt{2} \cos\left[n \pi (1+z/h)\right]\per
\eeq

\section{Density modes}
Similarly the baroclinic modes for density, here denoted by $\sr_n$, are defined via the eigenproblem 
\beq
\label{eig_prob_rho}
\sr_n'' = -\kappa_n^2 \ibur \sr_n\com
\eeq
with homogeneous Dirichlet boundary conditions
\beq
\label{rho_bc}
@z = -h,0: \qquad \sr_n = 0\com
\eeq
and normalization
\beq
\label{normalization2}
\frac{1}{h}\int_{-h}^0 \!\!\sr_n \sr_m \dd z = \delta_{mn}\per 
\eeq
Alternatively, we can work on  the approximation from the beginning. The WKB approximate solution to \eqref{eig_prob_rho}-\eqref{rho_bc}, consistent with the bottom boundary conditions \eqref{rho_bc}, is
\beq
\sr_n^{po} = \frac{B_n}{\sqrt{N(z)}} \sin \left(\frac{\kappa_n}{f_0} \int_{-h}^{z} N(\xi)\dd \xi \right) \com
\eeq
The eigenvalues $\kappa_n$ are the same as before \eqref{kappan}. (This should be no surprise because it follow  from the definition of $\sp_n$ and $\sr_n$. Nonetheless,  the verification is a good sanity check.) To find $B_n$ we use the normalization \eqref{normalization2}
\beq
\label{bn_eqn}
B_n^2 \, \int_{-h}^{0}\!\!\frac{1}{N(z)} \sin \left(\frac{\kappa_n}{f_0}\int_{-h}^{z}\!\!\!N(\xi) \dd \xi\right) \dd z = h\com\qquad n\ge 1\per
\eeq
We use a similar trick as above i.e., we change variables with
\beq
\eta \defn \frac{\kappa_n}{N^2(z) f_0}\int_{-h}^{z}\!\!\! N(\xi) \dd \xi  \qquad \Rightarrow \qquad \dd\eta = \frac{\kappa_n}{N(z) f_0} \dd z\com
\eeq
where, in the WKB spirit, we used the fact that $N(z)$ is slowly varying when differentiating the relation above. We obtain
\beq
B_n = \Big(2/\Nb\Big)^{1/2}\per
\eeq
Thus the WKB approximate solution to the density modes is
\beq
\label{rpo_final}
\sr_n^{po} = \left(\frac{2}{\Nb N(z)}\right) \sin \left(\frac{n \pi}{\Nb\,h} \int_{-h}^{z} N(\xi)\dd \xi \right)\com\qquad n\ge 1 \per
\eeq
Finally, note that the modes are simply related
\beq
\frac{\dd \sr_n^{po}}{\dd z} = \underbrace{\frac{n\pi}{\Nb\,h}}_{=\kappa_n/f_0}\,\sp_n^{po}\per
\eeq

\subsection*{Constant buoyancy frequency}
Again we recover the $N = \text{const.}$ special case from \eqref{rpo_final}:
\beq
\sr_n^{po} = \frac{\sqrt{2}}{\Nb} \sin \left[n\pi(1 + z/h)\right]\per
\eeq

\end{document}