建立了一个适用于复杂地形的冰雹云模式。模式是二维、弹性、非静力、采用地形跟随坐标、包含双变参数冰相微物理过程参数化。
A hail cloud model that is two dimensional elastic non hydrostatic, USES a terrain following coordinate system and includes double parameters for ice phase microphysics, has been developed.
为了研究层状冷云自然降水和人工降水的机制建立了一维非定常的数值模式。
An one-dimensional time dependent numerical model has been developed to study the mechanism of natural and artificial precipitation from the cold layer clouds.
层状云由于在水平上较为均匀， 可以用一维模式来模拟其云微物理过程。
The stratiform cloud can be simulated with a one-dimensional model, duo to its uniform horizontal distribution of physical characters.
应用推荐