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- thermodynamic sea ice model 海冰热力模式
- Inter-comparison of parameterizations of radiative fluxes used in thermodynamic sea ice modeling for the Bohai Sea and the Baltic Sea 海冰热力模式的辐射参数化方案在渤海和波罗的海应用的比较
- Inter?comparison of parameterizations of radiative fluxes used in thermodynamic sea ice modeling for the Bohai Sea and the Baltic Sea 海冰热力模式的辐射参数化方案在渤海和波罗的海应用的比较
- Test forecasts and simulations on the sea ice thickness, concentration, drift velocity and ice edge have been carried out by using the dynamic sea ice model for the Bohai Sea. 该项工作使用海冰动力模式对黄、渤海海冰厚度、密集度、漂流速度和流冰外缘线进行了模拟和试报。
- An ocean model developed by the Bergen University in Norway (BOM, Bergen Ocean Model) was coupled with a state of art sea ice model CSIM4 (Community Sea Ice Model Version 4). 对挪威卑尔根大学发展的海洋模式BOM(Bergen Ocean Model)与集成最新海冰模式发展成果的海冰模式CSIM4(Community Sea Ice Model Version 4)进行了耦合，对北极海冰的气候变率进行了模拟。
- thermodynamic-dynamic sea ice model 热动力海冰模式
- Improvement of a Thermodynamic-dynamic Sea Ice Model 一个热动力海冰模式的改进与实验
- An area of open water surrounded by sea ice. 冰间湖由海水冰围成的一块开阔的水域
- A Review on Development of Sea Ice Model in Foreign Countries during Recent Years 近年来国外海冰模式发展的回顾
- Influence of tides on sea ice in the Weddell Sea: Investigations with a high-resolution dynamic-thermodynamic sea ice model 威德尔海潮汐对海冰的影响:用高分辨动力学-热力学海冰模式的研究
- The meltwater puddled the flat sea ice. 融化的冰水在平坦冰冻的海面上形成水坑。
- particle-in-cell sea ice model 质点-网格海冰模式
- Arctic Ocean sea ice volume: What explains its recent depletion? 北冰洋的海冰量:怎样解释近期的减少?
- Arctic summertime sea ice is decreasing by just over 7% a decade. 北极夏季海冰正在以每十年刚刚超过7%25的速度减少。
- By 2080, there may be no Arctic summer sea ice at all. 到2080年，北极夏季海冰可能将不复存在。
- The Coupled model was used to simulate the Arctic Ocean sea ice climate variability. 在资料分析和数值模拟的基础上，对北极海冰的气候变率进行了深入的研究，结果如下：
- Some problems about the ice model test are also discussed by comparison with the observed data from the prototype. 同时对照了原型观测成果,讨论了冰凌运动模型试验中的一些问题。
- Using the CSIM4, the Arctic sea ice equilibrium state was simulated reasonably. 采用CSIM4海冰模式对北极海冰的气候态进行了模拟。
- At transition region,the sea ice bending strength reached the maximum value. 海冰的弯曲强度随着应力速率的增加，经过延性、过渡和脆性三个阶段，在过渡区，海冰的弯曲强度达到最大值。
- This study is leaded by POM model, based on“3D ocean non-stationary baroclinic model”, which is proposed by Russian scientist and developed by considering sea ice in the model. 该问题的解决以POM模型为先导,以俄罗斯海洋学家的“海洋三维非定常斜压模型”为基础,同时加入作者对该模型海冰部分的补充。
