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revision 1.2 by dimitri, Sat Mar 1 01:01:52 2008 UTC revision 1.3 by mlosch, Tue Mar 4 20:31:31 2008 UTC
# Line 44  studies to motivate the present work. Line 44  studies to motivate the present work.
44  Traditionally, probably for historical reasons and the ease of  Traditionally, probably for historical reasons and the ease of
45  treating the Coriolis term, most standard sea-ice models are  treating the Coriolis term, most standard sea-ice models are
46  discretized on Arakawa-B-grids \citep[e.g.,][]{hibler79, harder99,  discretized on Arakawa-B-grids \citep[e.g.,][]{hibler79, harder99,
47    kreyscher00, zhang98, hunke97}. From the perspective of coupling a    kreyscher00, zhang98, hunke97}\ml{, although there are sea ice only
48  sea ice-model to a C-grid ocean model, the exchange of fluxes of heat    models diretized on a C-grid \citep[e.g.,][]{tremblay97,
49  and fresh-water pose no difficulty for a B-grid sea-ice model      lemieux09}}. From the perspective of coupling a sea ice-model to a
50    C-grid ocean model, the exchange of fluxes of heat and fresh-water
51    pose no difficulty for a B-grid sea-ice model
52  \citep[e.g.,][]{timmermann02a}. However, surface stress is defined at  \citep[e.g.,][]{timmermann02a}. However, surface stress is defined at
53  velocities points and thus needs to be interpolated between a B-grid  velocities points and thus needs to be interpolated between a B-grid
54  sea-ice model and a C-grid ocean model. Smoothing implicitly  sea-ice model and a C-grid ocean model. Smoothing implicitly
# Line 74  model; it presents example Arctic and An Line 76  model; it presents example Arctic and An
76  eddy-permitting, global ocean and sea-ice configuration; it compares B-grid  eddy-permitting, global ocean and sea-ice configuration; it compares B-grid
77  and C-grid dynamic solvers in a regional Arctic configuration; and it presents  and C-grid dynamic solvers in a regional Arctic configuration; and it presents
78  example results from coupled ocean and sea-ice adjoint-model integrations.  example results from coupled ocean and sea-ice adjoint-model integrations.
79    
80    %%% Local Variables:
81    %%% mode: latex
82    %%% TeX-master: "ceaice"
83    %%% End:
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