冰云

冰云光学特性与等效球Mie理论的误差分析

Optical properties of ice clouds and error analysis under Mie theory of equivalent spheres

用等效球Mie理论计算冰云光学特性的一种新方法

A new method calculating optical properties of ice clouds using Mie theory for equivalent Ice Sphere

文章提出了一种简单且适用于大气环流模式（GCM）的冰云辐射参数化。

A Scheme of simple radiative parameterization of ice clouds suitable for use in GCM model is presented .

奥尔顿怀疑是木星全球风的模式改变将富含氨的物质带到了SEB之上的清澈而寒冷的区域，为在高空形成冰云打下了基础。

Orton suspects that changes in global wind patterns have brought ammonia-rich material into the clear , cold zone above the SEB , setting the stage for formation of the high-altitude , icy clouds .

这种结合激光雷达和红外观测（CLIM）的方法主要是用IIR三波段红外亮温来区分冰云和厚沙尘层并用激光雷达识别薄沙尘和水云层。

This combined lidar and IR measurement ( hereafter , CLIM ) method uses the IIR tri-spectral IR brightness temperatures to discriminate between ice cloud and dense dust layers , and lidar measurements to detect thin dust and water cloud layers .

不同环境温度下冰云粒子的单次散射参量

Single Scattering of Ice Crystals in Ice Clouds with Various Ambient Temperature

冰云短波辐射特性参数化

Parameterization of shortwave radiation properties of ice cloud

水平取向对冰云辐射传输的影响

The Transmission Loop the level of carbohydrates ; EFFECTS OF HORIZONTAL ORIENTATION ON THE RADIATIVE PROPERTIES OF ICE CLOUDS

冰云和水云对短波辐射性质（消光系数、单次散射反照率及不对称因子）的影响很不相同，应分别计算。

It is well known that due to their different influences on solar radiation transfer , different parameterizations should be used for ice clouds and water clouds , respectively .

粒子在冰云和成长相结合，变得如此之大，向上流动）在云中的空气（上升气流可以不再支持他们，他们倒在地上。

The ice particles in the clouds grow and combine to become so large that upward flowing air ( updrafts ) in the clouds can no longer support them , and they fall to the ground .

最后，考虑到冰云在辐射传播中的重要作用，利用温度方法对云中冰水和液水进行了区分，同时还研究了模式对云粒子有效半径的敏感性。

Finally , considering the important role of ice cloud in radiative transfer , we discriminate ice water and liquid water in terms of temperature , and also discuss the model 's sensitivity to cloud droplet effective radius .