--- MITgcm_contrib/articles/ceaice/ceaice.tex	2008/02/25 19:30:56	1.11
+++ MITgcm_contrib/articles/ceaice/ceaice.tex	2008/02/25 22:06:17	1.12
@@ -1,4 +1,4 @@
-% $Header: /home/ubuntu/mnt/e9_copy/MITgcm_contrib/articles/ceaice/ceaice.tex,v 1.11 2008/02/25 19:30:56 mlosch Exp $
+% $Header: /home/ubuntu/mnt/e9_copy/MITgcm_contrib/articles/ceaice/ceaice.tex,v 1.12 2008/02/25 22:06:17 dimitri Exp $
 % $Name:  $
 \documentclass[12pt]{article}
 
@@ -54,22 +54,28 @@
 \begin{abstract}
 
 As part of ongoing efforts to obtain a best possible synthesis of most
-available, global-scale, ocean and sea ice data, dynamic and thermodynamic
-sea-ice model components have been incorporated in the Massachusetts Institute
-of Technology general circulation model (MITgcm).  Sea-ice dynamics use either
-a visco-plastic rheology solved with a line successive relaxation (LSR)
-technique, reformulated on an Arakawa C-grid in order to match the oceanic and
-atmospheric grids of the MITgcm, and modified to permit efficient and accurate
-automatic differentiation of the coupled ocean and sea-ice model
-configurations.
+available, global-scale, ocean and sea ice data, a dynamic and thermodynamic
+sea-ice model has been coupled to the Massachusetts Institute of Technology
+general circulation model (MITgcm).  Ice mechanics follow a viscous plastic
+rheology and the ice momentum equations are solved numerically using either
+line successive relaxation (LSR) or elastic-viscous-plastic (EVP) dynamic
+models.  Ice thermodynamics are represented using either a zero-heat-capacity
+formulation or a two-layer formulation that conserves enthalpy.  The model
+includes prognostic variables for snow and for sea-ice salinity.  The above
+sea ice model components were borrowed from current-generation climate models
+but they were reformulated on an Arakawa C-grid in order to match the MITgcm
+oceanic grid and they were modified in many ways to permit efficient and
+accurate automatic differentiation.  This paper describes the MITgcm sea ice
+model; it presents example Arctic and Antarctic results from a realistic,
+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.
 
 \end{abstract}
 
 \section{Introduction}
 \label{sec:intro}
 
-more blabla
-
 \section{Model}
 \label{sec:model}
 
@@ -367,13 +373,18 @@
 \subsection{Arctic Domain with Open Boundaries}
 \label{sec:arctic}
 
-The Arctic domain of integration is illustrated in Fig.~\ref{???}.  It
+The Arctic domain of integration is illustrated in Fig.~\ref{fig:arctic1}.  It
 is carved out from, and obtains open boundary conditions from, the
 global cubed-sphere configuration of the Estimating the Circulation
 and Climate of the Ocean, Phase II (ECCO2) project
 \citet{menemenlis05}.  The domain size is 420 by 384 grid boxes
 horizontally with mean horizontal grid spacing of 18 km.
 
+\begin{figure}
+%\centerline{{\includegraphics*[width=0.44\linewidth]{\fpath/arctic1.eps}}}
+\caption{Bathymetry of Arctic Domain.\label{fig:arctic1}}
+\end{figure}
+
 There are 50 vertical levels ranging in thickness from 10 m near the surface
 to approximately 450 m at a maximum model depth of 6150 m. Bathymetry is from
 the National Geophysical Data Center (NGDC) 2-minute gridded global relief