Diff of /manual/s_examples/baroclinic_gyre/fourlayer.tex

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--- manual/s_examples/baroclinic_gyre/fourlayer.tex	2001/10/25 18:36:55	1.9
+++ manual/s_examples/baroclinic_gyre/fourlayer.tex	2001/11/13 19:01:42	1.10
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_examples/baroclinic_gyre/fourlayer.tex,v 1.9 2001/10/25 18:36:55 cnh Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_examples/baroclinic_gyre/fourlayer.tex,v 1.10 2001/11/13 19:01:42 adcroft Exp $
 % $Name:  $
 
 \section{Example: Four layer Baroclinic Ocean Gyre In Spherical Coordinates}
@@ -120,7 +120,7 @@
 \subsection{Equations solved}
 For this problem
 the implicit free surface, {\bf HPE} (see section \ref{sec:hydrostatic_and_quasi-hydrostatic_forms}) form of the 
-equations described in Marshall et. al \cite{Marshall97a} are
+equations described in Marshall et. al \cite{marshall:97a} are
 employed. The flow is three-dimensional with just temperature, $\theta$, as 
 an active tracer.  The equation of state is linear.
 A horizontal Laplacian operator $\nabla_{h}^2$ provides viscous