摘要
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 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.
出处
《冰川冻土》
CSCD
北大核心
1998年第4期330-342,共13页
Journal of Glaciology and Geocryology
关键词
海冰
海冰运移
海冰消退
数值模拟
北极
arctic sea ice, drifting and decaying, numerical modeling
