--- 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