Diff of /manual/s_examples/barotropic_gyre/baro.tex

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--- manual/s_examples/barotropic_gyre/baro.tex	2001/11/13 18:19:18	1.5
+++ manual/s_examples/barotropic_gyre/baro.tex	2001/11/13 19:01:42	1.6
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_examples/barotropic_gyre/baro.tex,v 1.5 2001/11/13 18:19:18 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_examples/barotropic_gyre/baro.tex,v 1.6 2001/11/13 19:01:42 adcroft Exp $
 % $Name:  $
 
 \section{Example: Barotropic Ocean Gyre In Cartesian Coordinates}
@@ -82,7 +82,7 @@
 
 \subsection{Equations Solved}
 The model is configured in hydrostatic form. The implicit free surface form of the
-pressure equation described in Marshall et. al \cite{Marshall97a} is
+pressure equation described in Marshall et. al \cite{marshall:97a} is
 employed.
 A horizontal Laplacian operator $\nabla_{h}^2$ provides viscous
 dissipation. The wind-stress momentum input is added to the momentum equation