对流降水 meaning in Chinese
convective precipitation
Examples
- At the same time , the disturbance of the low - level jet might be the triggering condition for heavy rain . but the surface occluded front crossing qinling mountains and strengthening , maybe the direct reason
同时，由于冷空气是从中层侵入西北地区东部，这样就形成了较强的对流不稳定层结，有利于对流降水的发生。 - In this paper , firstly large - scale air circulation and weather system evolution are analyzed , and get the scale feature and spread process of the meso - scale convective system by analyzing time - space layout of precipitation and satellite cloud maps . the lower resolution of t213 model and less time - space resolution of data were responsible for the above mentioned misforecast . in this study , the event is simulated by mm5v3 . 6 with two - way - interaction and triple nested grid
分析并指出了此次过程中对流降水的演变规律：对流活动引起的高层重力波和边界层冷涌是对流传播和触发大暴雨中心对流活动的主要机制，地面冷空气的侵入，引起边界层暖湿空气的交汇和强烈辐合是对流活动显著加强的原因。 - 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。 - While the precipitation of southeast of inner - mogolio is attributed as the strong convective precipitation , the rainfall of liaoning and northeast of heilongjiang is induced by subtropical high and westerly trough , and that of west of heilongjiang is influenced directly by vortex in upper air
各区域产生极端降水的天气背景也不相同：内蒙古东南部的降水是前倾槽引起的强对流降水天气，辽宁和黑龙江东北部的降水是由于副热带高压和西风槽的共同作用引起的。黑龙江西部的降水是由于高空涡的直接作用引起的。