ascending motion meaning in Chinese
上升运动
Examples
- The compensating descending motions normally occur over a much larger area than the ascending motion .
补偿下沉运动通常出现在比上升运动大得多的区域上。 - Ascend motion analysis of reusable launch vehicle
可重复使用运载器上升段运动分析 - The results show that the " 8 . 11 " rainstorm had significant mesoscale character . ascending motion , divergence and vorticity field intensified rapidly in the narrow area of rainstorm
11 ”暴雨过程的常用物理量场的分析表明：这次暴雨过程的中尺度特征非常明显，在分辨率较低的大尺度场上很难分析出其物理量场的迅速变化。 - Analyzing the physics structure of vorticity , divergence , vertical velocity , frontogenesis " function , apparent heat source and apparent moist sink etc . indicated the physics fields are favorable for the occurance of the heavy rain over changjiang - huaihe river basin where the physics values are well according to the heavy rainstorm positions ; the low level jet is closely subject to the moisture and the coupled system of the low and the upper level jetstreams induced the strongly " ascending motion ; the intensity of the frontogenesis varies with the development of the rainfall system and reacts the rainfall intensity
主要分析了这次过程中的多种物理量，包括涡度、散度、垂直速度、锋生函数、视热源、视水汽汇等，对这一暴雨过程有了比较系统的认识。结果表明：在江淮流域存在着有利于发生暴雨的物理量场配置，涡度、散度、垂直速度等物理量，与暴雨的落区都很吻合的；低空急流的产生不仅有利于水汽的输送，而且高低空急流的耦合造成了有利于强上升运动的配置；锋生强度随着降水系统的发展变化，并影响降水强度。 - The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows , so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening , one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea . furthermore , with the effect of terrain , the southern shaanxi province became the center of this extremely heavy rain process
中尺度结构分析表明，本次暴雨具有明显的中尺度特征，是由三支气流共同作用的结果，分析发现( 1 )地面东南风和地形在这次大暴雨过程起主要作用； ( 2 )东路冷空气主要是通过中低层侵入陕南地区的，并与地面冷式锢囚锋的形成密不可分； ( 3 )夜博士论文:中尺度地形对陕南暴雨的影响研究间垂直次级环流发展加强可能有两个原因，一个是由于地形山谷风的作用，另一个是降水的潜热释放激发了上升运动: ( 4 )位势不稳定层结的形成与低层暖湿平流的发展有很好的对应关系; ( 5 )本次暴雨的水汽主要靠偏南风急流将孟加拉湾和中国南海的水汽输送至西北地区东部，为暴雨的发生提供了必要热力条件。