
The NPS 18 km Stand-Alone Sea Ice Model
The NPS 18 km resolution Stand-Alone Sea Ice Model
includes:
-
A switch for using viscous-plastic ice rheology of
Hibler (1979) with more efficient numerics of Zhang and Hibler (1997)
or using elastic-viscous-plastic ice rheology of Hunke and Dukowicz
(1997).
-
Parkinson/Washington (1979) surface heat budgets.
-
Zero-layer thermodynamics of Semtner (1976).
-
Atmospheric forcing: 1983-1984 3-daily mean ECMWF
reanalysis data. Specifically 10 m winds, 2 m temperature and
dewpoint, surface downward longwave and shortwave radiation.
-
Oceanic forcing: 1983-1984 3-daily mean output from
the NPS 18 km coupled ice-ocean model. Specifically, 10 m
(first level) Temperature and Salinity, 32.5 m (2nd level) u and v
velocities.
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- Last modified 29 January 2003 -
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