--- manual/s_algorithm/text/tracer.tex	2001/11/13 15:32:28	1.9
+++ manual/s_algorithm/text/tracer.tex	2001/11/13 18:15:26	1.10
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/manual/s_algorithm/text/tracer.tex,v 1.9 2001/11/13 15:32:28 adcroft Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/manual/s_algorithm/text/tracer.tex,v 1.10 2001/11/13 18:15:26 adcroft Exp $
 % $Name:  $
 
 \section{Tracer equations}
@@ -43,7 +43,7 @@
 everywhere else. This term is therefore referred to as the surface
 correction term. Global conservation is not possible using the
 flux-form (as here) and a linearized free-surface
-(\cite{Griffies00,Campin02}).
+(\cite{griffies:00,campin:02}).
 
 The continuity equation can be recovered by setting
 $G_{diff}=G_{forc}=0$ and $\tau=1$.
@@ -200,7 +200,7 @@
 
 For non-divergent flow, this discretization can be shown to conserve
 the tracer both locally and globally and to globally conserve tracer
-variance, $\tau^2$. The proof is given in \cite{Adcroft95,Adcroft97}.
+variance, $\tau^2$. The proof is given in \cite{adcroft:95,adcroft:97}.
 
 \fbox{ \begin{minipage}{4.75in}
 {\em S/R GAD\_C2\_ADV\_X} ({\em gad\_c2\_adv\_x.F})