Diff of /manual/s_overview/continuous_eqns.tex

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--- manual/s_overview/continuous_eqns.tex	2001/09/11 14:03:33	1.2
+++ manual/s_overview/continuous_eqns.tex	2001/09/26 14:53:10	1.3
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/Attic/continuous_eqns.tex,v 1.2 2001/09/11 14:03:33 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_overview/Attic/continuous_eqns.tex,v 1.3 2001/09/26 14:53:10 cnh Exp $
 % $Name:  $
 
 \section{Continuous equations in `r' coordinates}
@@ -201,13 +201,13 @@
 
 The boundary conditions at top and bottom are given by:
 
-\begin{eqnarray*}
+\begin{eqnarray}
 &&\omega =0~\text{at }r=R_{fixed} \label{eq:fixed-bc-atmos}
 \text{ (top of the atmosphere)} \\
 \omega &=&\frac{Dp_{s}}{Dt}\text{; at }r=R_{moving}\text{ (bottom of the
 atmosphere)}
 \label{eq:moving-bc-atmos}
-\end{eqnarray*}
+\end{eqnarray}
 
 Then the (hydrostatic form of) eq(\ref{incompressible}) yields a consistent
 set of atmospheric equations which, for convenience, are written out in $p$
@@ -242,12 +242,12 @@
 
 Boundary conditions are:
 
-\begin{eqnarray*}
+\begin{eqnarray}
 w &=&0~\text{at }r=R_{fixed}\text{ (ocean bottom)} 
 \label{eq:fixed-bc-ocean}\\
 w &=&\frac{D\eta }{Dt}\text{ at }r=R_{moving}=\eta \text{ (ocean surface)
 \label{eq:moving-bc-ocean}}
-\end{eqnarray*}
+\end{eqnarray}
 where $\eta $ is the elevation of the free surface.
 
 Then eq(\ref{incompressible}) yields a consistent set of oceanic equations