--- MITgcm_contrib/articles/ceaice/ceaice_intro.tex	2008/03/01 01:01:52	1.2
+++ MITgcm_contrib/articles/ceaice/ceaice_intro.tex	2008/04/29 14:02:29	1.4
@@ -44,9 +44,11 @@
 Traditionally, probably for historical reasons and the ease of
 treating the Coriolis term, most standard sea-ice models are
 discretized on Arakawa-B-grids \citep[e.g.,][]{hibler79, harder99,
-  kreyscher00, zhang98, hunke97}. From the perspective of coupling a
-sea ice-model to a C-grid ocean model, the exchange of fluxes of heat
-and fresh-water pose no difficulty for a B-grid sea-ice model
+  kreyscher00, zhang98, hunke97}\ml{, although there are sea ice only
+  models diretized on a C-grid \citep[e.g.,][]{ip91, tremblay97,
+    lemieux09}}. From the perspective of coupling a sea ice-model to a
+C-grid ocean model, the exchange of fluxes of heat and fresh-water
+pose no difficulty for a B-grid sea-ice model
 \citep[e.g.,][]{timmermann02a}. However, surface stress is defined at
 velocities points and thus needs to be interpolated between a B-grid
 sea-ice model and a C-grid ocean model. Smoothing implicitly
@@ -74,3 +76,8 @@
 eddy-permitting, global ocean and sea-ice configuration; it compares B-grid
 and C-grid dynamic solvers in a regional Arctic configuration; and it presents
 example results from coupled ocean and sea-ice adjoint-model integrations.
+
+%%% Local Variables: 
+%%% mode: latex
+%%% TeX-master: "ceaice"
+%%% End: 
