地面雨量 meaning in English
ground rainfall
Examples
- In addition , by analyzing radar data and precipitation data on ground , we draw conclusion that the choice of seeding region condition is reasonable and the seeding has worked
并结合雷达、地面雨量进行了分析，观测事实说明作业区作业条件选择是合理的，并有一定的作业效果。 - 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。 - Rainfall and vertical profile of hydrometers are retrieved for land and ocean using tmi 1b11 data . the comparison of retrievals of gprof v6 . 1 and v6 . 2 with ground - based radar and gauge data on land and pr data on ocean show that the gprof - v6 algorithm can retrieve rain intensity much well and indicate vertical distribution of hydrometers mainly . as far as retrieved precipitation area , it is better for convective precipitation type than stratified precipitation type
将陆地的反演结果与地基雷达资料和地面雨量计资料进行比较，海洋的反演结果结合trmmpr的降水产品进行比较，结果表明： gprof - v6算法反演的降水产品可以较好地反映降水强度并反映降水的主要垂直结构；在落区方面，对流降水反映较好，层云降水则较差；云-辐射数据集的扩充与改进可提高反演精度。 - Distinct changing features of clouds after seeding were analyzed , then some significant conclusions are got . with the suitable seeding methods in proper time and region in clouds , precipitation is enhanced . and spacial distribution is changed , for example , position of rainfall center and intensities were significantly changed
研究发现不同催化剂对云体的影响各有其自身特色，但也有共同之处：在云体发展的合适时机和部位进行适量的催化，地面累积总降水量提高；同时有可能改变降水的空间分布，使地面雨量中心位置和强度发生改变。