| 1. | Investigation on catalyst dosage in aircraft cloud seeding in stratiform clouds
层状云飞机增雨催化剂用量研究 |
| 2. | As the warm , moist air goes up , the moisture therein will condense into extensive stratiform clouds
当暖湿空气抬升时，水汽冷却凝结成大范围的层状云。 |
| 3. | Numerical simulation on the mesoscale structure and organization of a stratiform cloud system in henan province
河南省层状降水云系中尺度结构的数值模拟 |
| 4. | The rain from thick stratiform clouds usually lasts longer than showers although the intensity is lighter
由深厚层状云产生的降水，通常比骤雨持续的时间长，但雨势较小。 |
| 5. | It was sunny most of the time that day , but by dusk stratiform clouds could be faintly seen approaching from the west ( left hand side )
当天日间普遍天晴，黄昏时隐约可见层状云正从西方（左面）移近。 |
| 6. | It was sunny most of the time that day , but by dusk stratiform clouds could be faintly seen approaching from the west left hand side
象站向北面拍摄的天气照片。当天日间普遍天晴，黄昏时隐约可见层状云正从西方左面移近。 |
| 7. | There is an active growth layer and super cooled water exists with ice crystals that may be an important feature layer to occur rain in stratiform cloud
过冷水滴和冰晶共存层存在，且冰晶活跃增长，此层的存在可能是发生降水的关键。 |
| 8. | Stratiform clouds are layered clouds formed mainly by uplifting of air on a large scale , commonly seen near a front , which signifies the interface of warm , moist air climbing up cold air on encountering the latter
乌云接日头，半夜雨稠稠的层状云天气：层状云主要由大范围的气流上升运动形成，常见于锋面附近，即暖湿空气碰到冷气团，向上爬升的交界面上。 |
| 9. | In this paper aircraft has made vertical and synthetic detecting flying purposefully on 9 . 17 , 2003 according to cloud ' s macro and microstructure . vertical layers and representative places of stratiform cloud on 9 . 17 , 2003 are analyzed using the observational data of particle measurement system ( pms ) , combined with satellite data , radar data , and precipitation data on ground . by this we have got cloud ' s microphysical structure and physical process of the natural precipitation , and the physical effect evidence has been testified according to observational data after lco2 seeding
本文用综合观测的方法，利用机载pms云粒子探测系统，根据云系的宏微观结构特征进行有针对性的垂直探测飞行，配合卫星、雷达、地面雨量、雨强计网观测资料对2003年9月17日延安降水性层状云系中那些有代表性的部位或垂直分层做细致的观测分析，获得云系的微物理结构和自然降水形成的物理过程，并用观测事实来验证人工增雨引晶催化后的物理响应判据。 |
| 10. | There is a vaporizing layer below 0 layer and it is far thick , which may be one of the important reasons of small precipitation on ground ; in the paper the cloud and the rain drop size distribution in warm layer of stratiform cloud are calculated and analyzed . it is found that n ( d ) = n0dnexp ( - a d ) can express the size distributions of little cloud drops , big cloud drops and rain drops . the observational and calculated results are well matched
在零度层以下蒸发层的存在，且比较深厚，应是导致地面雨强较小的重要因素之一；本文对暖层的云滴谱和雨滴谱进行了计算，对小云滴、大云滴和雨滴分布可以用同一种形式的分布密度函数多阶函数n ( d ) = n _ 0d ~ nexp ( - d )来表示。 |
