--- manual/s_overview/appendix_atmos.tex	2001/09/11 14:34:38	1.2
+++ manual/s_overview/appendix_atmos.tex	2001/09/26 14:53:10	1.3
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/Attic/appendix_atmos.tex,v 1.2 2001/09/11 14:34:38 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/Attic/appendix_atmos.tex,v 1.3 2001/09/26 14:53:10 cnh Exp $
 % $Name:  $
 
 \section{Appendix ATMOSPHERE}
@@ -78,11 +78,11 @@
 \subsubsection{Boundary conditions}
 
 The upper and lower boundary conditions are : 
-\begin{eqnarray*}
+\begin{eqnarray}
 \mbox{at the top:}\;\;p=0 &&\text{, }\omega =\frac{Dp}{Dt}=0 \\
 \mbox{at the surface:}\;\;p=p_{s} &&\text{, }\phi =\phi _{topo}=g~Z_{topo}
 \label{eq:boundary-condition-atmosphere}
-\end{eqnarray*}
+\end{eqnarray}
 In $p$-coordinates, the upper boundary acts like a solid boundary ($\omega
 =0 $); in $z$-coordinates and the lower boundary is analogous to a free
 surface ($\phi $ is imposed and $\omega \neq 0$).
@@ -95,11 +95,11 @@
 is not dynamically relevant and can therefore be subtracted from the
 equations. The equations written in terms of perturbations are obtained by
 substituting the following definitions into the previous model equations: 
-\begin{eqnarray*}
+\begin{eqnarray}
 \theta &=&\theta _{o}+\theta ^{\prime } \label{eq:atmos-ref-prof-theta} \\
 \alpha &=&\alpha _{o}+\alpha ^{\prime }  \label{eq:atmos-ref-prof-alpha}\\
 \phi &=&\phi _{o}+\phi ^{\prime } \label{eq:atmos-ref-prof-phi}
-\end{eqnarray*}
+\end{eqnarray}
 The reference state (indicated by subscript ``0'') corresponds to
 horizontally homogeneous atmosphere at rest ($\theta _{o},\alpha _{o},\phi
 _{o}$) with surface pressure $p_{o}(x,y)$ that satisfies $\phi