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revision 1.11 by mlosch, Sat Mar 8 20:40:47 2008 UTC revision 1.12 by mlosch, Thu Mar 13 17:54:24 2008 UTC
# Line 106  The Arctic domain of integration is illu Line 106  The Arctic domain of integration is illu
106  \reffig{arctic_topog}.  It is carved out from, and obtains open  \reffig{arctic_topog}.  It is carved out from, and obtains open
107  boundary conditions from, the global cubed-sphere configuration  boundary conditions from, the global cubed-sphere configuration
108  described above.  The horizontal domain size is 420 by 384 grid boxes.  described above.  The horizontal domain size is 420 by 384 grid boxes.
109  \begin{figure}  \begin{figure*}
110  \centerline{{\includegraphics*[width=0.44\linewidth]{\fpath/topography}}}  \includegraphics*[width=0.44\linewidth]{\fpath/topography}
111  \caption{Bathymetry and domain boudaries of Arctic  \includegraphics*[width=0.46\linewidth]{\fpath/archipelago}
112    Domain. The letters label sections in the Canadian Archipelago,  \caption{Left: Bathymetry and domain boudaries of Arctic
113    where ice transport is evaluated.    Domain; the dashed line marks the boundaries of the inset on the
114      right hand side. The letters in the inset label sections in the
115      Canadian Archipelago, where ice transport is evaluated:
116      A: Nares Strait; %
117      B: \ml{Meighen Island}; %
118      C: Prince Gustaf Adolf Sea; %
119      D: \ml{Brock Island}; %
120      E: McClure Strait; %
121      F: Amundsen Gulf; %
122      G: Lancaster Sound; %
123      H: Barrow Strait \ml{W.}; %
124      I: Barrow Strait \ml{E.}; %
125      J: Barrow Strait \ml{N.}. %
126    \label{fig:arctic_topog}}    \label{fig:arctic_topog}}
127  \end{figure}  \end{figure*}
128    
129  The main dynamic difference from cube sphere is that it does not use  The main dynamic difference from cube sphere is that it does not use
130  rescaled vertical coordinates (z$^\ast$) and the surface boundary  rescaled vertical coordinates (z$^\ast$) and the surface boundary
131  conditions for freshwater input are different, because those features  conditions for freshwater input are different, because those features
132  are not supported by the open boundary code.  are not supported by the open boundary code.
133    
134  Open water, dry ice, wet ice, dry snow, and wet snow albedo are, respectively, 0.15, 0.85,  Open water, dry ice, wet ice, dry snow, and wet snow albedo are,
135  0.76, 0.94, and 0.8.  respectively, 0.15, 0.85, 0.76, 0.94, and 0.8.
136    
137  The model is integrated from January, 1992 to March \ml{[???]}, 2000,  The model is integrated from January, 1992 to March \ml{[???]}, 2000,
138  with three different dynamical solvers and two different boundary  with three different dynamical solvers and two different boundary
# Line 275  different experiments has consequences f Line 287  different experiments has consequences f
287  the Arctic. Although the main export of ice goes through the Fram  the Arctic. Although the main export of ice goes through the Fram
288  Strait, a considerable amoung of ice is exported through the Canadian  Strait, a considerable amoung of ice is exported through the Canadian
289  Archipelago \citep{???}. \reffig{archipelago} shows a time series of  Archipelago \citep{???}. \reffig{archipelago} shows a time series of
290  \ml{[maybe smooth to longer time scales:] daily averaged} ice  \ml{[maybe smooth to different time scales:] daily averaged, smoothed
291  transport through various straits in the Canadian Archipelago and the    with monthly running means,} ice transport through various straits
292  Fram Strait for the different model solutions.  Generally, the  in the Canadian Archipelago and the Fram Strait for the different
293  C-EVP-ns solution has highest maximum (export out of the Artic) and  model solutions.  Generally, the C-EVP-ns solution has highest maximum
294  minimum (import into the Artic) fluxes as the drift velocities are  (export out of the Artic) and minimum (import into the Artic) fluxes
295  largest in this solution \ldots  as the drift velocities are largest in this solution \ldots
296  \begin{figure}  \begin{figure}
297  \centerline{{\includegraphics*[width=0.6\linewidth]{\fpath/Jan1992xport}}}  %\centerline{{\includegraphics*[width=0.6\linewidth]{\fpath/Jan1992xport}}}
298    \centerline{{\includegraphics*[width=0.6\linewidth]{\fpath/ice_export}}}
299  \caption{Transport through Canadian Archipelago for different solver  \caption{Transport through Canadian Archipelago for different solver
300    flavors. The letters refer to the labels of the sections in    flavors. The letters refer to the labels of the sections in
301    \reffig{arctic_topog}.    \reffig{arctic_topog}.
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