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A sea ice model which contains Hibler’s (1979, 1980) dynamics and Parkinson & Washington’s (1979) thermodynamics is used to simulate the seasonal cycle of sea ice motion, thickness,compactness and growth rate in the Arctic Ocean under mean annual climatological forcing. Furthermore, it is used to investigate the air-sea heat flux and mean annual heat state over the entire Arctic Ocean.
A sea ice model which contains Hibler’s (1979, 1980) dynamics and Parkinson & Washington’s (1979) thermodynamics is used to simulate the seasonal cycle of sea ice motion, thickness, compactness and growth rate in the Arctic Ocean under the mean annual climatological forcing. , it is used to investigate the air-sea heat flux and mean annual heat state over the entire Arctic Ocean.