| 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}\ml{, although there are sea ice only |
kreyscher00, zhang98, hunke97}\ml{, although there are sea ice only |
| 48 |
models diretized on a C-grid \citep[e.g.,][]{tremblay97, |
models diretized on a C-grid \citep[e.g.,][]{ip91, tremblay97, |
| 49 |
lemieux09}}. From the perspective of coupling a sea ice-model to a |
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 |
C-grid ocean model, the exchange of fluxes of heat and fresh-water |
| 51 |
pose no difficulty for a B-grid sea-ice model |
pose no difficulty for a B-grid sea-ice model |