--- MITgcm/model/src/calc_phi_hyd.F	2001/09/26 18:09:14	1.16
+++ MITgcm/model/src/calc_phi_hyd.F	2001/09/27 18:14:20	1.17
@@ -1,4 +1,4 @@
-C $Header: /home/ubuntu/mnt/e9_copy/MITgcm/model/src/calc_phi_hyd.F,v 1.16 2001/09/26 18:09:14 cnh Exp $
+C $Header: /home/ubuntu/mnt/e9_copy/MITgcm/model/src/calc_phi_hyd.F,v 1.17 2001/09/27 18:14:20 adcroft Exp $
 C $Name:  $
 
 #include "CPP_OPTIONS.h"
@@ -180,8 +180,8 @@
 C  --  Energy Conserving Form, No hFac  --
 C------------ The integration for the first level phi(k=1) is the same
 C             for both the "finite volume" and energy conserving methods.
-C    *NOTE* o Working with geopotential Anomaly, the geopotential boundary 
-C             condition is simply Phi'(Ro_surf)=0.
+Ci    *NOTE* o Working with geopotential Anomaly, the geopotential boundary 
+C             condition is simply Phi-prime(Ro_surf)=0.
 C           o convention ddPI > 0 (same as drF & drC)
 C-----------------------------------------------------------------------
         IF (K.EQ.1) THEN