--- MITgcm_contrib/articles/ceaice/ceaice_adjoint.tex	2008/07/28 12:34:27	1.7
+++ MITgcm_contrib/articles/ceaice/ceaice_adjoint.tex	2008/07/29 08:34:22	1.8
@@ -212,7 +212,7 @@
 \ml{[which equation do you mean?]}) along a zonal axis through
 Lancaster Sound, Barrow Strait, and Melville Sound (115\degW\ to
 80\degW, averaged across the passages) are depicted as Hovmueller
-diagrams in \reffig{lancaster}. These are, from top to bottom, the
+diagrams in \reffig{lancasteradj}. These are, from top to bottom, the
 sensitivities with respect to effective ice thickness ($hc$), ocean
 surface temperature ($SST$) and precipitation ($p$) for free slip
 (left column) and no slip (right column) ice drift boundary
@@ -220,16 +220,29 @@
 %
 \begin{figure*}
   \includegraphics*[height=.8\textheight]{\fpath/lancaster_adj}
-  \caption{Hovermoeller diagrams of sensitivities (derivatives) of the
-    ``solid'' fresh water (i.e., ice and snow) export $J$ through Lancaster sound
+  \caption{Hovermoeller diagrams along the axis Viscount Melville
+    Sound/Barrow Strait/Lancaster Sound. The diagrams show the
+    sensitivities (derivatives) of the ``solid'' fresh water (i.e.,
+    ice and snow) export $J$ through Lancaster sound
     (\reffig{arctic_topog}, cross-section G) with respect to effective
     ice thickness ($hc$), ocean surface temperature (SST) and
-    precipitation ($p$) for two runs with free slip and no slip boundary
-    conditions for the sea ice drift. Also shown it the normalized ice
-    strengh $P/P^*=(hc)\,\exp[-C\,(1-c)]$ (bottom panel); each plot is
-    overlaid with the contours 1 and 3 of the normalized ice strength
-    for orientation.
-    \label{fig:lancaster}}
+    precipitation ($p$) for two runs with free slip and no slip
+    boundary conditions for the sea ice drift. Each plot is overlaid
+    with the contours 1 and 3 of the normalized ice strengh
+    $P/P^*=(hc)\,\exp[-C\,(1-c)]$ for orientation.
+    \label{fig:lancasteradj}}
+\end{figure*}
+%
+\begin{figure*}
+  \includegraphics*[height=.8\textheight]{\fpath/lancaster_fwd}
+  \caption{Hovermoeller diagrams along the axis Viscount Melville
+    Sound/Barrow Strait/Lancaster Sound of effective ice thickness
+    ($hc$), effective snow thickness ($h_{s}c$) and normalized ice
+    strengh $P/P^*=(hc)\,\exp[-C\,(1-c)]$ for two runs with free slip
+    and no slip boundary conditions for the sea ice drift. Each plot
+    is overlaid with the contours 1 and 3 of the normalized ice
+    strength for orientation.
+    \label{fig:lancasterfwd}}
 \end{figure*}
 %
 
@@ -307,7 +320,7 @@
 \ml{[Here we need for integrations to show that the adjoint
   sensitivites are not just academic. I suggest to perturb HEFF
   and THETA initial conditions, and PRECIP somewhere in the Melville
-  Sound and then produce plots similar to reffig{lancaster}. For
+  Sound and then produce plots similar to reffig{lancasteradj}. For
   PRECIP it would be great to have two perturbation experiments, one
   where ADJprecip is posivite and one where ADJprecip is negative]}
   
